{"id":5911,"date":"2025-08-19T10:11:03","date_gmt":"2025-08-19T08:11:03","guid":{"rendered":"https:\/\/www.nobveenweiden.nl\/?page_id=5911"},"modified":"2025-08-19T10:13:48","modified_gmt":"2025-08-19T08:13:48","slug":"findings-scientific-papers","status":"publish","type":"page","link":"https:\/\/www.nobveenweiden.nl\/en\/findings-scientific-papers\/","title":{"rendered":"Findings"},"content":{"rendered":"<div id='av-layout-grid-1'  class='av-layout-grid-container av-4zctes-8efd1fd331f7621838e216dacf842050 entry-content-wrapper main_color av-flex-cells  avia-builder-el-0  el_before_av_section  avia-builder-el-first   container_wrap fullsize'  >\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-4w9du4-a33f9cbee56572d9b4c5ef98b67689da\">\n.flex_cell.av-4w9du4-a33f9cbee56572d9b4c5ef98b67689da{\nvertical-align:middle;\nheight:400px;\nmin-height:400px;\npadding:70px 70px 70px 0px;\nbackground-color:#008fa8;\n}\n<\/style>\n<div class='flex_cell av-4w9du4-a33f9cbee56572d9b4c5ef98b67689da av-gridrow-cell av_one_half no_margin  avia-builder-el-1  el_before_av_cell_one_half  avia-builder-el-first ' ><div class='flex_cell_inner'><\/div><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-4r8bbg-1fe2c9a9a912c01d832d585f4602c0ac\">\n.flex_cell.av-4r8bbg-1fe2c9a9a912c01d832d585f4602c0ac{\nvertical-align:top;\nheight:400px;\nmin-height:400px;\npadding:30px 30px 30px 30px;\nbackground:url(https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/rapportages_kleur.jpg) 50% 50% no-repeat scroll ;\n}\n<\/style>\n<div class='flex_cell av-4r8bbg-1fe2c9a9a912c01d832d585f4602c0ac av-gridrow-cell av_one_half no_margin av-hide-on-mobile  avia-builder-el-2  el_after_av_cell_one_half  avia-builder-el-last  avia-full-stretch' ><div class='flex_cell_inner'><\/div><\/div>\n<\/div>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-4ki79o-300dd3ed0ebe96678bf2c260f4e6840d\">\n.avia-section.av-4ki79o-300dd3ed0ebe96678bf2c260f4e6840d{\nbackground-color:rgba(0,0,0,0.01);\nbackground-image:unset;\nmargin-top:-380px;\nmargin-bottom:0px;\n}\n<\/style>\n<div id='av_section_1'  class='avia-section av-4ki79o-300dd3ed0ebe96678bf2c260f4e6840d main_color avia-section-default avia-no-border-styling  avia-builder-el-3  el_after_av_layout_row  el_before_av_one_full  avia-bg-style-scroll container_wrap fullsize'  ><div class='container av-section-cont-open' ><div class='template-page content  av-content-full alpha units'><div class='post-entry post-entry-type-page post-entry-5911'><div class='entry-content-wrapper clearfix'>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-4ckeos-5a46923e93ee6c6bdd5626475685f32e\">\n.flex_column.av-4ckeos-5a46923e93ee6c6bdd5626475685f32e{\n-webkit-border-radius:0px 0px 0px 0px;\n-moz-border-radius:0px 0px 0px 0px;\nborder-radius:0px 0px 0px 0px;\n}\n<\/style>\n<div class='flex_column av-4ckeos-5a46923e93ee6c6bdd5626475685f32e av_one_half  avia-builder-el-4  el_before_av_one_half  avia-builder-el-first  first flex_column_div av-zero-column-padding '     ><p>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-4ai2rg-7967f4b30e94f6a5e0158a9bf7605822\">\n#top .av-special-heading.av-4ai2rg-7967f4b30e94f6a5e0158a9bf7605822{\npadding-bottom:10px;\ncolor:#ffffff;\n}\nbody .av-special-heading.av-4ai2rg-7967f4b30e94f6a5e0158a9bf7605822 .av-special-heading-tag .heading-char{\nfont-size:25px;\n}\n.av-special-heading.av-4ai2rg-7967f4b30e94f6a5e0158a9bf7605822 .special-heading-inner-border{\nborder-color:#ffffff;\n}\n.av-special-heading.av-4ai2rg-7967f4b30e94f6a5e0158a9bf7605822 .av-subheading{\nfont-size:15px;\n}\n<\/style>\n<div  class='av-special-heading av-4ai2rg-7967f4b30e94f6a5e0158a9bf7605822 av-special-heading-h1 custom-color-heading blockquote modern-quote  avia-builder-el-5  el_before_av_hr  avia-builder-el-first '><h1 class='av-special-heading-tag'  itemprop=\"headline\"  >Scientific Papers<\/h1><div class=\"special-heading-border\"><div class=\"special-heading-inner-border\"><\/div><\/div><\/div><br \/>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-eef04-1718f5b92132040184e49172f76abe8a\">\n#top .hr.av-eef04-1718f5b92132040184e49172f76abe8a{\nmargin-top:0px;\nmargin-bottom:0px;\n}\n.hr.av-eef04-1718f5b92132040184e49172f76abe8a .hr-inner{\nwidth:150px;\nborder-color:#ffffff;\n}\n<\/style>\n<div  class='hr av-eef04-1718f5b92132040184e49172f76abe8a hr-custom  avia-builder-el-6  el_after_av_heading  el_before_av_textblock  hr-left hr-icon-no'><span class='hr-inner inner-border-av-border-fat'><span class=\"hr-inner-style\"><\/span><\/span><\/div><br \/>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-3vyy78-adde676bd65c5023da1547b5b2d127c7\">\n#top .av_textblock_section.av-3vyy78-adde676bd65c5023da1547b5b2d127c7 .avia_textblock{\ncolor:#ffffff;\n}\n<\/style>\n<section  class='av_textblock_section av-3vyy78-adde676bd65c5023da1547b5b2d127c7'  itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div class='avia_textblock av_inherit_color'  itemprop=\"text\" ><p>The Scientific Papers that the NOBV has published can be found on this page.<\/p>\n<\/div><\/section><\/p><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-3nt7cs-83fdebcbdde8974839ad3a6bb1751f4d\">\n.flex_column.av-3nt7cs-83fdebcbdde8974839ad3a6bb1751f4d{\n-webkit-border-radius:0px 0px 0px 0px;\n-moz-border-radius:0px 0px 0px 0px;\nborder-radius:0px 0px 0px 0px;\n}\n<\/style>\n<div class='flex_column av-3nt7cs-83fdebcbdde8974839ad3a6bb1751f4d av_one_half  avia-builder-el-8  el_after_av_one_half  avia-builder-el-last  flex_column_div av-zero-column-padding '     ><\/div><\/div><\/div><\/div><!-- close content main div --><\/div><\/div><div id='after_section_1'  class='main_color av_default_container_wrap container_wrap fullsize'  ><div class='container av-section-cont-open' ><div class='template-page content  av-content-full alpha units'><div class='post-entry post-entry-type-page post-entry-5911'><div class='entry-content-wrapper clearfix'>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-3ht418-f6df6fa537a935eff546e25f80949ed2\">\n#top .flex_column.av-3ht418-f6df6fa537a935eff546e25f80949ed2{\nmargin-top:-100px;\nmargin-bottom:0px;\n}\n.flex_column.av-3ht418-f6df6fa537a935eff546e25f80949ed2{\n-webkit-border-radius:0px 0px 0px 0px;\n-moz-border-radius:0px 0px 0px 0px;\nborder-radius:0px 0px 0px 0px;\n}\n.responsive #top #wrap_all .flex_column.av-3ht418-f6df6fa537a935eff546e25f80949ed2{\nmargin-top:-100px;\nmargin-bottom:0px;\n}\n<\/style>\n<div class='flex_column av-3ht418-f6df6fa537a935eff546e25f80949ed2 av_one_full  avia-builder-el-9  el_after_av_section  el_before_av_section  avia-builder-el-no-sibling  first flex_column_div av-zero-column-padding '     ><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-3cbhu4-1445f7790a3b8e5c9a79cab9fa93ba4f\">\n.avia-image-container.av-3cbhu4-1445f7790a3b8e5c9a79cab9fa93ba4f img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-3cbhu4-1445f7790a3b8e5c9a79cab9fa93ba4f .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div  class='avia-image-container av-3cbhu4-1445f7790a3b8e5c9a79cab9fa93ba4f av-styling-circle avia-align-center  avia-builder-el-10  avia-builder-el-no-sibling  icoonimage'   itemprop=\"image\" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/ImageObject\" ><div class=\"avia-image-container-inner\"><div class=\"avia-image-overlay-wrap\"><img decoding=\"async\" class='wp-image-4699 avia-img-lazy-loading-not-4699 avia_image ' src=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/09\/resultaten.png\" alt='' title='resultaten'  height=\"180\" width=\"180\"  itemprop=\"thumbnailUrl\" srcset=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/09\/resultaten.png 180w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/09\/resultaten-80x80.png 80w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/09\/resultaten-36x36.png 36w\" sizes=\"(max-width: 180px) 100vw, 180px\" \/><\/div><\/div><\/div><\/div><\/p>\n<\/div><\/div><\/div><!-- close content main div --><\/div><\/div><div id='av_section_2'  class='avia-section av-39dhh8-b96df6f05d0cdb6f278e01e0f75f9ac8 main_color avia-section-default avia-no-border-styling  avia-builder-el-11  el_after_av_one_full  el_before_av_hr  avia-bg-style-scroll container_wrap fullsize'  ><div class='container av-section-cont-open' ><div class='template-page content  av-content-full alpha units'><div class='post-entry post-entry-type-page post-entry-5911'><div class='entry-content-wrapper clearfix'>\n\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-c9wuda-628877362915379f66dd431193383508\">\n#top .hr.hr-invisible.av-c9wuda-628877362915379f66dd431193383508{\nheight:30px;\n}\n<\/style>\n<div  class='hr av-c9wuda-628877362915379f66dd431193383508 hr-invisible  avia-builder-el-13  el_after_av_heading  el_before_av_hr '><span class='hr-inner '><span class=\"hr-inner-style\"><\/span><\/span><\/div>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-3zi69a-0fa341f61807b62c260d55d033e92040\">\n#top .hr.hr-invisible.av-3zi69a-0fa341f61807b62c260d55d033e92040{\nheight:30px;\n}\n<\/style>\n<div  class='hr av-3zi69a-0fa341f61807b62c260d55d033e92040 hr-invisible  avia-builder-el-14  el_after_av_hr  el_before_av_heading '><span class='hr-inner '><span class=\"hr-inner-style\"><\/span><\/span><\/div>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-3prqim-94da644c11ac45a52c05a53830b4f09b\">\n#top .av-special-heading.av-3prqim-94da644c11ac45a52c05a53830b4f09b{\npadding-bottom:10px;\n}\nbody .av-special-heading.av-3prqim-94da644c11ac45a52c05a53830b4f09b .av-special-heading-tag .heading-char{\nfont-size:25px;\n}\n.av-special-heading.av-3prqim-94da644c11ac45a52c05a53830b4f09b .av-subheading{\nfont-size:15px;\n}\n<\/style>\n<div  class='av-special-heading av-3prqim-94da644c11ac45a52c05a53830b4f09b av-special-heading-h3 blockquote modern-quote  avia-builder-el-15  el_after_av_hr  el_before_av_one_half '><h3 class='av-special-heading-tag'  itemprop=\"headline\"  >Drivers and annual totals of methane emissions from Dutch Peatlands<\/h3><div class=\"special-heading-border\"><div class=\"special-heading-inner-border\"><\/div><\/div><\/div>\n<div class='flex_column av-c0d9ji-b6961adf09ce65799e255d09447d6a5e av_one_half  avia-builder-el-16  el_after_av_heading  el_before_av_one_half  first flex_column_div '     ><section  class='av_textblock_section av-m3efl148-8743047699e9fa5aad5529177502b6c2'  itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div class='avia_textblock'  itemprop=\"text\" ><button class=\"responsivevoice-button\" type=\"button\" title=\"ResponsiveVoice Tap to Start\/Stop Speech\" data-rvtts-action=\"speak\" data-rvtts-text=\"In the NOBV, not only CO2 emissions from peatlands are meseared, but also emissions of the greenhouse gases methane and nitrous oxide. The measurements of methane emissions under different land uses have been published in a scientific article entitled \u201cDrivers and annual totals of methane emissions from Dutch Peatlands.\u201d Measurements were taken at various locations and over several years using Eddy Covariance (EC) towers to visualize the variation between years and between land uses. The measurements show that average methane emissions were highest at wet natural sites with groundwater levels above or just below ground level and lowest at agricultural grasslands. Authors: Alexander J.V. Buzacott (VU), Bart Kruijt (WUR), Laurent Bataille (WUR), Quint van Giersbergen (RUN), Tom S. Heuts (RUN), Christian Fritz (RUN), Reinder Nouta (Wetterskip Frysl\u00e2n), Gilles Erkens (Deltares\/UU), Jim Boonman (VU), Merit van den Berg (VU), Jacobus van Huissteden, Ype van der Velde (VU) greater than Read the paper here.\" data-rvtts-voice=\"Dutch Female\" data-rvtts-brand-url=\"https:\/\/responsivevoice.org\/?utm_source=wordpress-plugin&amp;utm_medium=referral&amp;utm_campaign=powered-by\" data-rvtts-brand-label=\"Powered by ResponsiveVoice\"><svg class=\"rvtts-icon\" width=\"22\" height=\"22\" viewBox=\"0 0 22 22\" fill=\"currentColor\" aria-hidden=\"true\" focusable=\"false\"><path fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M11 0C4.92345 0 0 4.92345 0 11C0 13.2683 0.690345 15.3772 1.86621 17.1221L0.811724 21.0517L4.70345 20.0124C6.48621 21.2641 8.65586 22 11 22C17.0766 22 22 17.0766 22 11C22 4.92345 17.0766 0 11 0ZM3.99793 9.99862C3.99793 9.44483 4.44552 8.99724 4.99931 8.99724C5.5531 8.99724 6.00069 9.44483 6.00069 9.99862V12.0014C6.00069 12.5552 5.5531 13.0028 4.99931 13.0028C4.44552 13.0028 3.99793 12.5552 3.99793 12.0014V9.99862ZM8.99724 13.9966C8.99724 14.5503 8.54966 14.9979 7.99586 14.9979C7.44207 14.9979 6.99448 14.5503 6.99448 13.9966V7.99586C6.99448 7.44207 7.44207 6.99448 7.99586 6.99448C8.54966 6.99448 8.99724 7.44207 8.99724 7.99586V13.9966ZM12.0014 17.0007C12.0014 17.5545 11.5538 18.0021 11 18.0021C10.4462 18.0021 9.99862 17.5545 9.99862 17.0007V4.99931C9.99862 4.44552 10.4462 3.99793 11 3.99793C11.5538 3.99793 12.0014 4.44552 12.0014 4.99931V17.0007ZM14.9979 13.9966C14.9979 14.5503 14.5503 14.9979 13.9966 14.9979C13.4428 14.9979 12.9952 14.5503 12.9952 13.9966V7.99586C12.9952 7.44207 13.4428 6.99448 13.9966 6.99448C14.5503 6.99448 14.9979 7.44207 14.9979 7.99586V13.9966ZM18.0021 12.0014C18.0021 12.5552 17.5545 13.0028 17.0007 13.0028C16.4469 13.0028 15.9993 12.5552 15.9993 12.0014V9.99862C15.9993 9.44483 16.4469 8.99724 17.0007 8.99724C17.5545 8.99724 18.0021 9.44483 18.0021 9.99862V12.0014Z\"\/><\/svg><span class=\"responsivevoice-button__label\">Tekst oplezen<\/span><\/button> <\/p>\n<div>\n<p>In the NOBV, not only CO2 emissions from peatlands are meseared, but also emissions of the greenhouse gases methane and nitrous oxide. The measurements of methane emissions under different land uses have been published in a scientific article entitled &#8220;Drivers and annual totals of methane emissions from Dutch Peatlands.&#8221; Measurements were taken at various locations and over several years using Eddy Covariance (EC) towers to visualize the variation between years and between land uses. The measurements show that average methane emissions were highest at wet natural sites with groundwater levels above or just below ground level and lowest at agricultural grasslands.<\/p>\n<\/div>\n<p><b>Authors: <\/b>Alexander J.V. Buzacott (VU), Bart Kruijt (WUR), Laurent Bataille (WUR), Quint van Giersbergen (RUN), Tom S. Heuts (RUN), Christian Fritz (RUN), Reinder Nouta (Wetterskip Frysl\u00e2n), Gilles Erkens (Deltares\/UU), Jim Boonman (VU), Merit van den Berg (VU), Jacobus van Huissteden, Ype van der Velde (VU)<\/p>\n<p><a href=\"https:\/\/onlinelibrary.wiley.com\/doi\/10.1111\/gcb.17590\">&gt; Read the paper here<\/a>.<\/p>\n<p>\n<\/div><\/section><\/div><div class='flex_column av-5njqm6-1e39ca8b43355d926a025c2583ee426a av_one_half  avia-builder-el-18  el_after_av_one_half  el_before_av_heading  flex_column_div '     ><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-m4iiunpo-2b51459ef6f57c5409de9e4b610949d2\">\n.avia-image-container.av-m4iiunpo-2b51459ef6f57c5409de9e4b610949d2 img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-m4iiunpo-2b51459ef6f57c5409de9e4b610949d2 .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div  class='avia-image-container av-m4iiunpo-2b51459ef6f57c5409de9e4b610949d2 av-styling- avia-align-center  avia-builder-el-19  avia-builder-el-no-sibling '   itemprop=\"image\" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/ImageObject\" ><div class=\"avia-image-container-inner\"><div class=\"avia-image-overlay-wrap\"><a href=\"https:\/\/onlinelibrary.wiley.com\/doi\/10.1111\/gcb.17590\" class=\"avia_image\" target=\"_blank\" rel=\"noopener noreferrer\"><img decoding=\"async\" class='wp-image-5349 avia-img-lazy-loading-not-5349 avia_image ' src=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Drivers_and_annual_totals-192x300.jpg\" alt='' title='Drivers_and_annual_totals'  height=\"300\" width=\"192\"  itemprop=\"thumbnailUrl\" srcset=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Drivers_and_annual_totals-192x300.jpg 192w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Drivers_and_annual_totals-452x705.jpg 452w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Drivers_and_annual_totals.jpg 564w\" sizes=\"(max-width: 192px) 100vw, 192px\" \/><\/a><\/div><\/div><\/div><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-39nqvy-b256e90e453ffb1c2c6a7b4002b2814d\">\n#top .av-special-heading.av-39nqvy-b256e90e453ffb1c2c6a7b4002b2814d{\npadding-bottom:10px;\n}\nbody .av-special-heading.av-39nqvy-b256e90e453ffb1c2c6a7b4002b2814d .av-special-heading-tag .heading-char{\nfont-size:25px;\n}\n.av-special-heading.av-39nqvy-b256e90e453ffb1c2c6a7b4002b2814d .av-subheading{\nfont-size:15px;\n}\n<\/style>\n<div  class='av-special-heading av-39nqvy-b256e90e453ffb1c2c6a7b4002b2814d av-special-heading-h3 blockquote modern-quote  avia-builder-el-20  el_after_av_one_half  el_before_av_one_half '><h3 class='av-special-heading-tag'  itemprop=\"headline\"  >Monitoring long-term peat subsidence with subsidence platens in Zegveld, The Netherlands<\/h3><div class=\"special-heading-border\"><div class=\"special-heading-inner-border\"><\/div><\/div><\/div>\n<div class='flex_column av-czj0u-8f264e0f3cf0c3387348427b31a51145 av_one_half  avia-builder-el-21  el_after_av_heading  el_before_av_one_half  first flex_column_div '     ><section  class='av_textblock_section av-2yaky6-efb124c2f8a68202b03ac643b9f165a8'  itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div class='avia_textblock'  itemprop=\"text\" ><button class=\"responsivevoice-button\" type=\"button\" title=\"ResponsiveVoice Tap to Start\/Stop Speech\" data-rvtts-action=\"speak\" data-rvtts-text=\"This paper, written by a team of researchers from Wageningen Environmental Research and Deltares, is based on data from the NOBV (Dutch Institute for Peat Soil Research) and 50 years of field measurements. In Zegveld, subsidence plates were installed in a plot with a low ditch water level in 1970 and in a plot with a high ditch water level in 1973. The plates were placed at seven different depths, allowing researchers to investigate where subsidence occurs within the peat profile. The height of both the plates and the soil surface was measured annually at the end of winter by surveyors. This provided a time series (up to 2023) of soil height data, which have now been analyzed. Authors: Harry T. Massop (WENR), Rudi Hessel (WENR), Jan J.H. van den Akker (WENR), Sanneke van Asselen (Deltares), Gilles Erkens (Deltares), Paul A. Gerritsen (WENR), Frank H.G.A. Gerritsen (WENR) greater than Read the paper here.\" data-rvtts-voice=\"Dutch Female\" data-rvtts-brand-url=\"https:\/\/responsivevoice.org\/?utm_source=wordpress-plugin&amp;utm_medium=referral&amp;utm_campaign=powered-by\" data-rvtts-brand-label=\"Powered by ResponsiveVoice\"><svg class=\"rvtts-icon\" width=\"22\" height=\"22\" viewBox=\"0 0 22 22\" fill=\"currentColor\" aria-hidden=\"true\" focusable=\"false\"><path fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M11 0C4.92345 0 0 4.92345 0 11C0 13.2683 0.690345 15.3772 1.86621 17.1221L0.811724 21.0517L4.70345 20.0124C6.48621 21.2641 8.65586 22 11 22C17.0766 22 22 17.0766 22 11C22 4.92345 17.0766 0 11 0ZM3.99793 9.99862C3.99793 9.44483 4.44552 8.99724 4.99931 8.99724C5.5531 8.99724 6.00069 9.44483 6.00069 9.99862V12.0014C6.00069 12.5552 5.5531 13.0028 4.99931 13.0028C4.44552 13.0028 3.99793 12.5552 3.99793 12.0014V9.99862ZM8.99724 13.9966C8.99724 14.5503 8.54966 14.9979 7.99586 14.9979C7.44207 14.9979 6.99448 14.5503 6.99448 13.9966V7.99586C6.99448 7.44207 7.44207 6.99448 7.99586 6.99448C8.54966 6.99448 8.99724 7.44207 8.99724 7.99586V13.9966ZM12.0014 17.0007C12.0014 17.5545 11.5538 18.0021 11 18.0021C10.4462 18.0021 9.99862 17.5545 9.99862 17.0007V4.99931C9.99862 4.44552 10.4462 3.99793 11 3.99793C11.5538 3.99793 12.0014 4.44552 12.0014 4.99931V17.0007ZM14.9979 13.9966C14.9979 14.5503 14.5503 14.9979 13.9966 14.9979C13.4428 14.9979 12.9952 14.5503 12.9952 13.9966V7.99586C12.9952 7.44207 13.4428 6.99448 13.9966 6.99448C14.5503 6.99448 14.9979 7.44207 14.9979 7.99586V13.9966ZM18.0021 12.0014C18.0021 12.5552 17.5545 13.0028 17.0007 13.0028C16.4469 13.0028 15.9993 12.5552 15.9993 12.0014V9.99862C15.9993 9.44483 16.4469 8.99724 17.0007 8.99724C17.5545 8.99724 18.0021 9.44483 18.0021 9.99862V12.0014Z\"\/><\/svg><span class=\"responsivevoice-button__label\">Tekst oplezen<\/span><\/button> <\/p>\n<div>\n<p>This paper, written by a team of researchers from Wageningen Environmental Research and Deltares, is based on data from the NOBV (Dutch Institute for Peat Soil Research) and 50 years of field measurements. In Zegveld, subsidence plates were installed in a plot with a low ditch water level in 1970 and in a plot with a high ditch water level in 1973. The plates were placed at seven different depths, allowing researchers to investigate where subsidence occurs within the peat profile. The height of both the plates and the soil surface was measured annually at the end of winter by surveyors. This provided a time series (up to 2023) of soil height data, which have now been analyzed.<\/p>\n<\/div>\n<p><strong>Authors<\/strong>: Harry T. Massop (WENR), Rudi Hessel (WENR), Jan J.H. van den Akker (WENR), Sanneke van Asselen (Deltares), Gilles Erkens (Deltares), Paul A. Gerritsen (WENR), Frank H.G.A. Gerritsen (WENR)<\/p>\n<p><a href=\"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0016706124002684\">&gt; Read the paper here.<\/a><\/p>\n<p>\n<\/div><\/section><\/div><div class='flex_column av-bacu4e-88bb9d78b3c205fbd9350d19a1044201 av_one_half  avia-builder-el-23  el_after_av_one_half  el_before_av_heading  flex_column_div '     ><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-m3eff3zi-d32a0422369f44e661dcf7136d48d0b1\">\n.avia-image-container.av-m3eff3zi-d32a0422369f44e661dcf7136d48d0b1 img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-m3eff3zi-d32a0422369f44e661dcf7136d48d0b1 .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div  class='avia-image-container av-m3eff3zi-d32a0422369f44e661dcf7136d48d0b1 av-styling- avia-align-center  avia-builder-el-24  avia-builder-el-no-sibling '   itemprop=\"image\" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/ImageObject\" ><div class=\"avia-image-container-inner\"><div class=\"avia-image-overlay-wrap\"><a href=\"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0016706124002684\" class=\"avia_image\" target=\"_blank\" rel=\"noopener noreferrer\"><img decoding=\"async\" class='wp-image-5096 avia-img-lazy-loading-not-5096 avia_image ' src=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/10\/peat_subsidence-192x300.jpg\" alt='' title='peat_subsidence'  height=\"300\" width=\"192\"  itemprop=\"thumbnailUrl\" srcset=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/10\/peat_subsidence-192x300.jpg 192w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/10\/peat_subsidence-452x705.jpg 452w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/10\/peat_subsidence.jpg 564w\" sizes=\"(max-width: 192px) 100vw, 192px\" \/><\/a><\/div><\/div><\/div><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-8l8tn2-c6796b2c01ac9975091d8a01c87a8a6b\">\n#top .av-special-heading.av-8l8tn2-c6796b2c01ac9975091d8a01c87a8a6b{\npadding-bottom:10px;\n}\nbody .av-special-heading.av-8l8tn2-c6796b2c01ac9975091d8a01c87a8a6b .av-special-heading-tag .heading-char{\nfont-size:25px;\n}\n.av-special-heading.av-8l8tn2-c6796b2c01ac9975091d8a01c87a8a6b .av-subheading{\nfont-size:15px;\n}\n<\/style>\n<div  class='av-special-heading av-8l8tn2-c6796b2c01ac9975091d8a01c87a8a6b av-special-heading-h3 blockquote modern-quote  avia-builder-el-25  el_after_av_one_half  el_before_av_one_half '><h3 class='av-special-heading-tag'  itemprop=\"headline\"  >A Bayesian inference approach to determine experimental Typha latifolia paludiculture greenhouse gas exchange measured with eddy covariance<\/h3><div class=\"special-heading-border\"><div class=\"special-heading-inner-border\"><\/div><\/div><\/div>\n<div class='flex_column av-7u1j0e-d8259edccb3ac1c3f589abc06f2145f3 av_one_half  avia-builder-el-26  el_after_av_heading  el_before_av_one_half  first flex_column_div '     ><section  class='av_textblock_section av-5bqxem-185df529adfce7d38b2e44a65aede357'  itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div class='avia_textblock'  itemprop=\"text\" ><button class=\"responsivevoice-button\" type=\"button\" title=\"ResponsiveVoice Tap to Start\/Stop Speech\" data-rvtts-action=\"speak\" data-rvtts-text=\"One of the methods used at the NOBV to measure greenhouse gas emissions from peat soils is the Eddy Covariance (EC) tower. An EC tower measures emissions over an area of approximately one hectare. This study focuses on EC measurements of cattails at the NOBV site in Zegveld. Authors: Alexander J.V. Buzacott (VU), Merit van den Berg (VU), Bart Kruijt (WUR), Jeroen Pijlman (Louis Bolk Instituut), Chrisitan Fritz (RUN), Pascal Wintjen (TNO), Ype van der Velde (VU) greater than Read the paper here.\" data-rvtts-voice=\"Dutch Female\" data-rvtts-brand-url=\"https:\/\/responsivevoice.org\/?utm_source=wordpress-plugin&amp;utm_medium=referral&amp;utm_campaign=powered-by\" data-rvtts-brand-label=\"Powered by ResponsiveVoice\"><svg class=\"rvtts-icon\" width=\"22\" height=\"22\" viewBox=\"0 0 22 22\" fill=\"currentColor\" aria-hidden=\"true\" focusable=\"false\"><path fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M11 0C4.92345 0 0 4.92345 0 11C0 13.2683 0.690345 15.3772 1.86621 17.1221L0.811724 21.0517L4.70345 20.0124C6.48621 21.2641 8.65586 22 11 22C17.0766 22 22 17.0766 22 11C22 4.92345 17.0766 0 11 0ZM3.99793 9.99862C3.99793 9.44483 4.44552 8.99724 4.99931 8.99724C5.5531 8.99724 6.00069 9.44483 6.00069 9.99862V12.0014C6.00069 12.5552 5.5531 13.0028 4.99931 13.0028C4.44552 13.0028 3.99793 12.5552 3.99793 12.0014V9.99862ZM8.99724 13.9966C8.99724 14.5503 8.54966 14.9979 7.99586 14.9979C7.44207 14.9979 6.99448 14.5503 6.99448 13.9966V7.99586C6.99448 7.44207 7.44207 6.99448 7.99586 6.99448C8.54966 6.99448 8.99724 7.44207 8.99724 7.99586V13.9966ZM12.0014 17.0007C12.0014 17.5545 11.5538 18.0021 11 18.0021C10.4462 18.0021 9.99862 17.5545 9.99862 17.0007V4.99931C9.99862 4.44552 10.4462 3.99793 11 3.99793C11.5538 3.99793 12.0014 4.44552 12.0014 4.99931V17.0007ZM14.9979 13.9966C14.9979 14.5503 14.5503 14.9979 13.9966 14.9979C13.4428 14.9979 12.9952 14.5503 12.9952 13.9966V7.99586C12.9952 7.44207 13.4428 6.99448 13.9966 6.99448C14.5503 6.99448 14.9979 7.44207 14.9979 7.99586V13.9966ZM18.0021 12.0014C18.0021 12.5552 17.5545 13.0028 17.0007 13.0028C16.4469 13.0028 15.9993 12.5552 15.9993 12.0014V9.99862C15.9993 9.44483 16.4469 8.99724 17.0007 8.99724C17.5545 8.99724 18.0021 9.44483 18.0021 9.99862V12.0014Z\"\/><\/svg><span class=\"responsivevoice-button__label\">Tekst oplezen<\/span><\/button> <\/p>\n<div>\n<p>One of the methods used at the NOBV to measure greenhouse gas emissions from peat soils is the Eddy Covariance (EC) tower. An EC tower measures emissions over an area of approximately one hectare. This study focuses on EC measurements of cattails at the NOBV site in Zegveld.<\/p>\n<\/div>\n<p><strong>Authors<\/strong>: Alexander J.V. Buzacott (VU), Merit van den Berg (VU), Bart Kruijt (WUR), Jeroen Pijlman (Louis Bolk Instituut), Chrisitan Fritz (RUN), Pascal Wintjen (TNO), Ype van der Velde (VU)<\/p>\n<p><a href=\"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0168192324002922?via%3Dihub\">&gt; Read the paper here.<\/a><\/p>\n<p>\n<\/div><\/section><\/div><div class='flex_column av-48cgla-93ae0112029c6953fc7d6fa2480c22c8 av_one_half  avia-builder-el-28  el_after_av_one_half  el_before_av_heading  flex_column_div '     ><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-m0v1xdq7-1708354e0a98e6aaac747802f8a396a2\">\n.avia-image-container.av-m0v1xdq7-1708354e0a98e6aaac747802f8a396a2 img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-m0v1xdq7-1708354e0a98e6aaac747802f8a396a2 .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div  class='avia-image-container av-m0v1xdq7-1708354e0a98e6aaac747802f8a396a2 av-styling- avia-align-center  avia-builder-el-29  avia-builder-el-no-sibling '   itemprop=\"image\" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/ImageObject\" ><div class=\"avia-image-container-inner\"><div class=\"avia-image-overlay-wrap\"><a href=\"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0168192324002922?via%3Dihub\" class=\"avia_image\" target=\"_blank\" rel=\"noopener noreferrer\"><img decoding=\"async\" class='wp-image-5318 avia-img-lazy-loading-not-5318 avia_image ' src=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Bayesian-inference-approach-192x300.jpg\" alt='' title='Bayesian-inference-approach'  height=\"300\" width=\"192\"  itemprop=\"thumbnailUrl\" srcset=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Bayesian-inference-approach-192x300.jpg 192w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Bayesian-inference-approach-452x705.jpg 452w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Bayesian-inference-approach.jpg 564w\" sizes=\"(max-width: 192px) 100vw, 192px\" \/><\/a><\/div><\/div><\/div><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-1zpif2-b61684f37d1d60bee4eff73f32e3e9f9\">\n#top .av-special-heading.av-1zpif2-b61684f37d1d60bee4eff73f32e3e9f9{\npadding-bottom:10px;\n}\nbody .av-special-heading.av-1zpif2-b61684f37d1d60bee4eff73f32e3e9f9 .av-special-heading-tag .heading-char{\nfont-size:25px;\n}\n.av-special-heading.av-1zpif2-b61684f37d1d60bee4eff73f32e3e9f9 .av-subheading{\nfont-size:15px;\n}\n<\/style>\n<div  class='av-special-heading av-1zpif2-b61684f37d1d60bee4eff73f32e3e9f9 av-special-heading-h3 blockquote modern-quote  avia-builder-el-30  el_after_av_one_half  el_before_av_one_half '><h3 class='av-special-heading-tag'  itemprop=\"headline\"  >CO2 emissions of drained coastal peatlands in the Netherlands and potential emission reduction by water infiltration systems <\/h3><div class=\"special-heading-border\"><div class=\"special-heading-inner-border\"><\/div><\/div><\/div>\n<div class='flex_column av-569ixa-0617bb921e057119a0cd13ac907deca8 av_one_half  avia-builder-el-31  el_after_av_heading  el_before_av_one_half  first flex_column_div '     ><section  class='av_textblock_section av-m0v20vis-dbcc26ce19a8c385bf7193c580810309'  itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div class='avia_textblock'  itemprop=\"text\" ><button class=\"responsivevoice-button\" type=\"button\" title=\"ResponsiveVoice Tap to Start\/Stop Speech\" data-rvtts-action=\"speak\" data-rvtts-text=\"What is the relationship between groundwater levels and CO2 emissions in Dutch peat meadow areas, and to what extent are water infiltrations systems effective in reducing emissions? This paper was published in Biogeosciences. Authors: Ralf Aben (RUN), Daniel van de Craats (WENR), Jim Boonman (VU), Stijn Peeters (RUN), Bart Vriend (VU), Coline Boonman (RUN), Ype van der Velde (VU), Gilles Erkens (Deltares\/UU), Merit van den berg (VU) greater than Read the paper here.\" data-rvtts-voice=\"Dutch Female\" data-rvtts-brand-url=\"https:\/\/responsivevoice.org\/?utm_source=wordpress-plugin&amp;utm_medium=referral&amp;utm_campaign=powered-by\" data-rvtts-brand-label=\"Powered by ResponsiveVoice\"><svg class=\"rvtts-icon\" width=\"22\" height=\"22\" viewBox=\"0 0 22 22\" fill=\"currentColor\" aria-hidden=\"true\" focusable=\"false\"><path fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M11 0C4.92345 0 0 4.92345 0 11C0 13.2683 0.690345 15.3772 1.86621 17.1221L0.811724 21.0517L4.70345 20.0124C6.48621 21.2641 8.65586 22 11 22C17.0766 22 22 17.0766 22 11C22 4.92345 17.0766 0 11 0ZM3.99793 9.99862C3.99793 9.44483 4.44552 8.99724 4.99931 8.99724C5.5531 8.99724 6.00069 9.44483 6.00069 9.99862V12.0014C6.00069 12.5552 5.5531 13.0028 4.99931 13.0028C4.44552 13.0028 3.99793 12.5552 3.99793 12.0014V9.99862ZM8.99724 13.9966C8.99724 14.5503 8.54966 14.9979 7.99586 14.9979C7.44207 14.9979 6.99448 14.5503 6.99448 13.9966V7.99586C6.99448 7.44207 7.44207 6.99448 7.99586 6.99448C8.54966 6.99448 8.99724 7.44207 8.99724 7.99586V13.9966ZM12.0014 17.0007C12.0014 17.5545 11.5538 18.0021 11 18.0021C10.4462 18.0021 9.99862 17.5545 9.99862 17.0007V4.99931C9.99862 4.44552 10.4462 3.99793 11 3.99793C11.5538 3.99793 12.0014 4.44552 12.0014 4.99931V17.0007ZM14.9979 13.9966C14.9979 14.5503 14.5503 14.9979 13.9966 14.9979C13.4428 14.9979 12.9952 14.5503 12.9952 13.9966V7.99586C12.9952 7.44207 13.4428 6.99448 13.9966 6.99448C14.5503 6.99448 14.9979 7.44207 14.9979 7.99586V13.9966ZM18.0021 12.0014C18.0021 12.5552 17.5545 13.0028 17.0007 13.0028C16.4469 13.0028 15.9993 12.5552 15.9993 12.0014V9.99862C15.9993 9.44483 16.4469 8.99724 17.0007 8.99724C17.5545 8.99724 18.0021 9.44483 18.0021 9.99862V12.0014Z\"\/><\/svg><span class=\"responsivevoice-button__label\">Tekst oplezen<\/span><\/button> <\/p>\n<div>\n<p>What is the relationship between groundwater levels and CO2 emissions in Dutch peat meadow areas, and to what extent are water infiltrations systems effective in reducing emissions? This paper was published in Biogeosciences.<\/p>\n<\/div>\n<p><strong>Authors<\/strong>: Ralf Aben (RUN), Daniel van de Craats (WENR), Jim Boonman (VU), Stijn Peeters (RUN), Bart Vriend (VU), Coline Boonman (RUN), Ype van der Velde (VU), Gilles Erkens (Deltares\/UU), Merit van den berg (VU)<\/p>\n<p>&gt; <a href=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/07\/Aben-et-al.-CO2-emissions-and-potential-emission-reduction_final.pdf\">Read the paper here<\/a>.<\/p>\n<p>\n<\/div><\/section><\/div><div class='flex_column av-4e27zy-872a884fc2a04c0b96d1670c0af59586 av_one_half  avia-builder-el-33  el_after_av_one_half  el_before_av_heading  flex_column_div '     ><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-m3efb3lp-662513e370a697059c20baf1c76e56a1\">\n.avia-image-container.av-m3efb3lp-662513e370a697059c20baf1c76e56a1 img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-m3efb3lp-662513e370a697059c20baf1c76e56a1 .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div  class='avia-image-container av-m3efb3lp-662513e370a697059c20baf1c76e56a1 av-styling- avia-align-center  avia-builder-el-34  avia-builder-el-no-sibling '   itemprop=\"image\" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/ImageObject\" ><div class=\"avia-image-container-inner\"><div class=\"avia-image-overlay-wrap\"><a href=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/07\/Aben-et-al.-CO2-emissions-and-potential-emission-reduction_final.pdf\" class=\"avia_image\" target=\"_blank\" rel=\"noopener noreferrer\"><img decoding=\"async\" class='wp-image-4649 avia-img-lazy-loading-not-4649 avia_image ' src=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/09\/CO2_emissions--192x300.jpg\" alt='' title='CO2_emissions-'  height=\"300\" width=\"192\"  itemprop=\"thumbnailUrl\" srcset=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/09\/CO2_emissions--192x300.jpg 192w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/09\/CO2_emissions--452x705.jpg 452w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/09\/CO2_emissions-.jpg 564w\" sizes=\"(max-width: 192px) 100vw, 192px\" \/><\/a><\/div><\/div><\/div><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-1v0m66-29e9a7badc939f449e8c797ea3007561\">\n#top .av-special-heading.av-1v0m66-29e9a7badc939f449e8c797ea3007561{\npadding-bottom:10px;\n}\nbody .av-special-heading.av-1v0m66-29e9a7badc939f449e8c797ea3007561 .av-special-heading-tag .heading-char{\nfont-size:25px;\n}\n.av-special-heading.av-1v0m66-29e9a7badc939f449e8c797ea3007561 .av-subheading{\nfont-size:15px;\n}\n<\/style>\n<div  class='av-special-heading av-1v0m66-29e9a7badc939f449e8c797ea3007561 av-special-heading-h3 blockquote modern-quote  avia-builder-el-35  el_after_av_one_half  el_before_av_one_half '><h3 class='av-special-heading-tag'  itemprop=\"headline\"  >Effects of subsurface water infiltration systems on land movement dynamics in Dutch peat meadows<\/h3><div class=\"special-heading-border\"><div class=\"special-heading-inner-border\"><\/div><\/div><\/div>\n<div class='flex_column av-6fpyym-e38e890dad056f7ddc2bcfd94064f843 av_one_half  avia-builder-el-36  el_after_av_heading  el_before_av_one_half  first flex_column_div '     ><section  class='av_textblock_section av-m71wuvbh-516ec6283735e06a7335cb3e9735f879'  itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div class='avia_textblock'  itemprop=\"text\" ><button class=\"responsivevoice-button\" type=\"button\" title=\"ResponsiveVoice Tap to Start\/Stop Speech\" data-rvtts-action=\"speak\" data-rvtts-text=\"Large-scale drainage and exploitation of peatlands over the past centuries has resulted in significant land subsidence and CO2 emissions due to peat degradation caused by microbial activity, shrinkage, and soil compaction. To reduce CO2 emissions and land subsidence in drained peatlands, subsurface water infiltration systems (WIS) are expected to be a suitable measure. This study evaluated the effects of WIS on seasonal vertical ground movements, based on field measurements from five locations in Dutch peat meadows, for the years 2021 and 2022. Authors: Sanneke van Asselen (Deltares), Gilles Erkens (Deltares\/UU), Christian Fritz (RUN), Rudi Hessel (WENR), Jan J.H. van den Akker (WENR) greater than Read the paper here.\" data-rvtts-voice=\"Dutch Female\" data-rvtts-brand-url=\"https:\/\/responsivevoice.org\/?utm_source=wordpress-plugin&amp;utm_medium=referral&amp;utm_campaign=powered-by\" data-rvtts-brand-label=\"Powered by ResponsiveVoice\"><svg class=\"rvtts-icon\" width=\"22\" height=\"22\" viewBox=\"0 0 22 22\" fill=\"currentColor\" aria-hidden=\"true\" focusable=\"false\"><path fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M11 0C4.92345 0 0 4.92345 0 11C0 13.2683 0.690345 15.3772 1.86621 17.1221L0.811724 21.0517L4.70345 20.0124C6.48621 21.2641 8.65586 22 11 22C17.0766 22 22 17.0766 22 11C22 4.92345 17.0766 0 11 0ZM3.99793 9.99862C3.99793 9.44483 4.44552 8.99724 4.99931 8.99724C5.5531 8.99724 6.00069 9.44483 6.00069 9.99862V12.0014C6.00069 12.5552 5.5531 13.0028 4.99931 13.0028C4.44552 13.0028 3.99793 12.5552 3.99793 12.0014V9.99862ZM8.99724 13.9966C8.99724 14.5503 8.54966 14.9979 7.99586 14.9979C7.44207 14.9979 6.99448 14.5503 6.99448 13.9966V7.99586C6.99448 7.44207 7.44207 6.99448 7.99586 6.99448C8.54966 6.99448 8.99724 7.44207 8.99724 7.99586V13.9966ZM12.0014 17.0007C12.0014 17.5545 11.5538 18.0021 11 18.0021C10.4462 18.0021 9.99862 17.5545 9.99862 17.0007V4.99931C9.99862 4.44552 10.4462 3.99793 11 3.99793C11.5538 3.99793 12.0014 4.44552 12.0014 4.99931V17.0007ZM14.9979 13.9966C14.9979 14.5503 14.5503 14.9979 13.9966 14.9979C13.4428 14.9979 12.9952 14.5503 12.9952 13.9966V7.99586C12.9952 7.44207 13.4428 6.99448 13.9966 6.99448C14.5503 6.99448 14.9979 7.44207 14.9979 7.99586V13.9966ZM18.0021 12.0014C18.0021 12.5552 17.5545 13.0028 17.0007 13.0028C16.4469 13.0028 15.9993 12.5552 15.9993 12.0014V9.99862C15.9993 9.44483 16.4469 8.99724 17.0007 8.99724C17.5545 8.99724 18.0021 9.44483 18.0021 9.99862V12.0014Z\"\/><\/svg><span class=\"responsivevoice-button__label\">Tekst oplezen<\/span><\/button> <\/p>\n<div>\n<p>Large-scale drainage and exploitation of peatlands over the past centuries has resulted in significant land subsidence and CO2 emissions due to peat degradation caused by microbial activity, shrinkage, and soil compaction. To reduce CO2 emissions and land subsidence in drained peatlands, subsurface water infiltration systems (WIS) are expected to be a suitable measure. This study evaluated the effects of WIS on seasonal vertical ground movements, based on field measurements from five locations in Dutch peat meadows, for the years 2021 and 2022.<\/p>\n<\/div>\n<p><strong>Authors<\/strong>: Sanneke van Asselen (Deltares), Gilles Erkens (Deltares\/UU), Christian Fritz (RUN), Rudi Hessel (WENR), Jan J.H. van den Akker (WENR)<\/p>\n<p><a href=\"https:\/\/hess.copernicus.org\/preprints\/hess-2024-152\/\">&gt; Read the paper here.<\/a><\/p>\n<p>\n<\/div><\/section><\/div><div class='flex_column av-4kb9um-903ec2f2827ca82d00de5f1c048478a3 av_one_half  avia-builder-el-38  el_after_av_one_half  el_before_av_heading  flex_column_div '     ><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-m71wvl2t-bb266e1db4ac6192ab69bd2df8813618\">\n.avia-image-container.av-m71wvl2t-bb266e1db4ac6192ab69bd2df8813618 img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-m71wvl2t-bb266e1db4ac6192ab69bd2df8813618 .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div  class='avia-image-container av-m71wvl2t-bb266e1db4ac6192ab69bd2df8813618 av-styling- avia-align-center  avia-builder-el-39  avia-builder-el-no-sibling '   itemprop=\"image\" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/ImageObject\" ><div class=\"avia-image-container-inner\"><div class=\"avia-image-overlay-wrap\"><a href=\"https:\/\/hess.copernicus.org\/preprints\/hess-2024-152\/\" class=\"avia_image\" target=\"_blank\" rel=\"noopener noreferrer\"><img decoding=\"async\" class='wp-image-5581 avia-img-lazy-loading-not-5581 avia_image ' src=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/02\/Effects-of-subsurface-water-infiltration-192x300.jpg\" alt='' title='Effects-of-subsurface-water-infiltration'  height=\"300\" width=\"192\"  itemprop=\"thumbnailUrl\" srcset=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/02\/Effects-of-subsurface-water-infiltration-192x300.jpg 192w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/02\/Effects-of-subsurface-water-infiltration-452x705.jpg 452w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/02\/Effects-of-subsurface-water-infiltration.jpg 564w\" sizes=\"(max-width: 192px) 100vw, 192px\" \/><\/a><\/div><\/div><\/div><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-237jge-78141cf64e7c73f97731156c1d796618\">\n#top .av-special-heading.av-237jge-78141cf64e7c73f97731156c1d796618{\npadding-bottom:10px;\n}\nbody .av-special-heading.av-237jge-78141cf64e7c73f97731156c1d796618 .av-special-heading-tag .heading-char{\nfont-size:25px;\n}\n.av-special-heading.av-237jge-78141cf64e7c73f97731156c1d796618 .av-subheading{\nfont-size:15px;\n}\n<\/style>\n<div  class='av-special-heading av-237jge-78141cf64e7c73f97731156c1d796618 av-special-heading-h3 blockquote modern-quote  avia-builder-el-40  el_after_av_one_half  el_before_av_one_half '><h3 class='av-special-heading-tag'  itemprop=\"headline\"  >Drainage effects on carbon budgets of degraded peatlands in the north of the Netherlands<\/h3><div class=\"special-heading-border\"><div class=\"special-heading-inner-border\"><\/div><\/div><\/div>\n<div class='flex_column av-m2wyni-3edd08ad747f247a03ce04ac43f2a79b av_one_half  avia-builder-el-41  el_after_av_heading  el_before_av_one_half  first flex_column_div '     ><section  class='av_textblock_section av-m7vtwvim-05b70405114e17229282eae81e1e28f6'  itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div class='avia_textblock'  itemprop=\"text\" ><button class=\"responsivevoice-button\" type=\"button\" title=\"ResponsiveVoice Tap to Start\/Stop Speech\" data-rvtts-action=\"speak\" data-rvtts-text=\"Peatlands can store large amounts of carbon. However, drainage for land use leads to peat oxidation, resulting in CO2 emissions. This study used mobile chamber systems in the Northern Netherlands to investigate the regional causes of CO2 emissions. Carbon budgets were estimated for a total of 13 grassland sites in Friesland. Authors: Thomas P.A.\u00a0Nijman (Radboud Universiteit Nijmegen),\u00a0Quint\u00a0van Giersbergen (Radboud Universiteit Nijmegen),\u00a0Tom S.\u00a0Heuts\u00a0(Radboud Universiteit Nijmegen),\u00a0Reinder\u00a0Nouta (Wetterskip Frysl\u00e2n),\u00a0Coline C.F.\u00a0Boonman\u00a0(Wageningen University),\u00a0Mandy\u00a0Velthuis (Radboud Universiteit Nijmegen),\u00a0Bart\u00a0Kruijt (Wageningen University),\u00a0Ralf C.H.\u00a0Aben (Radboud Universiteit Nijmegen),\u00a0Christian\u00a0Fritz (Radboud Universiteit Nijmegen) greater than Read the paper here.\" data-rvtts-voice=\"Dutch Female\" data-rvtts-brand-url=\"https:\/\/responsivevoice.org\/?utm_source=wordpress-plugin&amp;utm_medium=referral&amp;utm_campaign=powered-by\" data-rvtts-brand-label=\"Powered by ResponsiveVoice\"><svg class=\"rvtts-icon\" width=\"22\" height=\"22\" viewBox=\"0 0 22 22\" fill=\"currentColor\" aria-hidden=\"true\" focusable=\"false\"><path fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M11 0C4.92345 0 0 4.92345 0 11C0 13.2683 0.690345 15.3772 1.86621 17.1221L0.811724 21.0517L4.70345 20.0124C6.48621 21.2641 8.65586 22 11 22C17.0766 22 22 17.0766 22 11C22 4.92345 17.0766 0 11 0ZM3.99793 9.99862C3.99793 9.44483 4.44552 8.99724 4.99931 8.99724C5.5531 8.99724 6.00069 9.44483 6.00069 9.99862V12.0014C6.00069 12.5552 5.5531 13.0028 4.99931 13.0028C4.44552 13.0028 3.99793 12.5552 3.99793 12.0014V9.99862ZM8.99724 13.9966C8.99724 14.5503 8.54966 14.9979 7.99586 14.9979C7.44207 14.9979 6.99448 14.5503 6.99448 13.9966V7.99586C6.99448 7.44207 7.44207 6.99448 7.99586 6.99448C8.54966 6.99448 8.99724 7.44207 8.99724 7.99586V13.9966ZM12.0014 17.0007C12.0014 17.5545 11.5538 18.0021 11 18.0021C10.4462 18.0021 9.99862 17.5545 9.99862 17.0007V4.99931C9.99862 4.44552 10.4462 3.99793 11 3.99793C11.5538 3.99793 12.0014 4.44552 12.0014 4.99931V17.0007ZM14.9979 13.9966C14.9979 14.5503 14.5503 14.9979 13.9966 14.9979C13.4428 14.9979 12.9952 14.5503 12.9952 13.9966V7.99586C12.9952 7.44207 13.4428 6.99448 13.9966 6.99448C14.5503 6.99448 14.9979 7.44207 14.9979 7.99586V13.9966ZM18.0021 12.0014C18.0021 12.5552 17.5545 13.0028 17.0007 13.0028C16.4469 13.0028 15.9993 12.5552 15.9993 12.0014V9.99862C15.9993 9.44483 16.4469 8.99724 17.0007 8.99724C17.5545 8.99724 18.0021 9.44483 18.0021 9.99862V12.0014Z\"\/><\/svg><span class=\"responsivevoice-button__label\">Tekst oplezen<\/span><\/button> <\/p>\n<p>Peatlands can store large amounts of carbon. However, drainage for land use leads to peat oxidation, resulting in CO2 emissions. This study used mobile chamber systems in the Northern Netherlands to investigate the regional causes of CO2 emissions. Carbon budgets were estimated for a total of 13 grassland sites in Friesland.<\/p>\n<p><strong>Authors<\/strong>: Thomas P.A.\u00a0Nijman (Radboud Universiteit Nijmegen),\u00a0Quint\u00a0van Giersbergen (Radboud Universiteit Nijmegen),\u00a0Tom S.\u00a0Heuts\u00a0(Radboud Universiteit Nijmegen),\u00a0Reinder\u00a0Nouta (Wetterskip Frysl\u00e2n),\u00a0Coline C.F.\u00a0Boonman\u00a0(Wageningen University),\u00a0Mandy\u00a0Velthuis (Radboud Universiteit Nijmegen),\u00a0Bart\u00a0Kruijt (Wageningen University),\u00a0Ralf C.H.\u00a0Aben (Radboud Universiteit Nijmegen),\u00a0Christian\u00a0Fritz (Radboud Universiteit Nijmegen)<\/p>\n<p><a href=\"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0048969724030298?via%3Dihub\">&gt; Read the paper here.<\/a><\/p>\n<p>\n<\/div><\/section><\/div><div class='flex_column av-4pr6bi-1fd0e57681a68f7d819d1678015cdcf2 av_one_half  avia-builder-el-43  el_after_av_one_half  el_before_av_heading  flex_column_div '     ><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-2wgzu6-1efa107b1dc4f964b10997ef2ff18eb0\">\n.avia-image-container.av-2wgzu6-1efa107b1dc4f964b10997ef2ff18eb0 img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-2wgzu6-1efa107b1dc4f964b10997ef2ff18eb0 .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div  class='avia-image-container av-2wgzu6-1efa107b1dc4f964b10997ef2ff18eb0 av-styling- avia-align-center  avia-builder-el-44  avia-builder-el-no-sibling '   itemprop=\"image\" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/ImageObject\" ><div class=\"avia-image-container-inner\"><div class=\"avia-image-overlay-wrap\"><a href=\"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0048969724030298?via%3Dihub \" class=\"avia_image\" target=\"_blank\" rel=\"noopener noreferrer\"><img decoding=\"async\" class='wp-image-5666 avia-img-lazy-loading-not-5666 avia_image ' src=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/03\/drainage_effects_on_carbon--192x300.jpg\" alt='' title='drainage_effects_on_carbon-'  height=\"300\" width=\"192\"  itemprop=\"thumbnailUrl\" srcset=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/03\/drainage_effects_on_carbon--192x300.jpg 192w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/03\/drainage_effects_on_carbon--452x705.jpg 452w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/03\/drainage_effects_on_carbon-.jpg 564w\" sizes=\"(max-width: 192px) 100vw, 192px\" \/><\/a><\/div><\/div><\/div><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-k4wtce-562f624d11a89cb1b2294947024ac25b\">\n#top .av-special-heading.av-k4wtce-562f624d11a89cb1b2294947024ac25b{\npadding-bottom:10px;\n}\nbody .av-special-heading.av-k4wtce-562f624d11a89cb1b2294947024ac25b .av-special-heading-tag .heading-char{\nfont-size:25px;\n}\n.av-special-heading.av-k4wtce-562f624d11a89cb1b2294947024ac25b .av-subheading{\nfont-size:15px;\n}\n<\/style>\n<div  class='av-special-heading av-k4wtce-562f624d11a89cb1b2294947024ac25b av-special-heading-h3 blockquote modern-quote  avia-builder-el-45  el_after_av_one_half  el_before_av_one_half '><h3 class='av-special-heading-tag'  itemprop=\"headline\"  >Transparent automated CO2 flux chambers reveal spatial and temporal patterns of net carbon fluxes from managed peatlands<\/h3><div class=\"special-heading-border\"><div class=\"special-heading-inner-border\"><\/div><\/div><\/div>\n<div class='flex_column av-31cbke-9628bae1136bb0fff0312e4b6ec65968 av_one_half  avia-builder-el-46  el_after_av_heading  el_before_av_one_half  first flex_column_div '     ><section  class='av_textblock_section av-lxn4wnbe-fca2ae5393d85042a6b2d151daa309a3'  itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div class='avia_textblock'  itemprop=\"text\" ><button class=\"responsivevoice-button\" type=\"button\" title=\"ResponsiveVoice Tap to Start\/Stop Speech\" data-rvtts-action=\"speak\" data-rvtts-text=\"How do we measure CO2 emissions from peat soils? At the NOBV, we use three different methods: automatic chamber measurements that cover an area of approximately one square meter, Eddy Covariance (EC) towers that measure emissions over a larger area (approximately one hectare), and aircraft measurements taken over a large area (hundreds of hectares). All three systems are used in the research program, but the results have not yet been compared in detail. This study compares the insights provided by the automatic chamber measurements with those obtained using an EC tower. Authors: Jim Boonman (VU), Alexander J.V. Buzacott (VU), Merit van den Berg (VU), Corine van Huissteden (VU), Ype van der Velde (VU) greater than Read the paper here.\" data-rvtts-voice=\"Dutch Female\" data-rvtts-brand-url=\"https:\/\/responsivevoice.org\/?utm_source=wordpress-plugin&amp;utm_medium=referral&amp;utm_campaign=powered-by\" data-rvtts-brand-label=\"Powered by ResponsiveVoice\"><svg class=\"rvtts-icon\" width=\"22\" height=\"22\" viewBox=\"0 0 22 22\" fill=\"currentColor\" aria-hidden=\"true\" focusable=\"false\"><path fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M11 0C4.92345 0 0 4.92345 0 11C0 13.2683 0.690345 15.3772 1.86621 17.1221L0.811724 21.0517L4.70345 20.0124C6.48621 21.2641 8.65586 22 11 22C17.0766 22 22 17.0766 22 11C22 4.92345 17.0766 0 11 0ZM3.99793 9.99862C3.99793 9.44483 4.44552 8.99724 4.99931 8.99724C5.5531 8.99724 6.00069 9.44483 6.00069 9.99862V12.0014C6.00069 12.5552 5.5531 13.0028 4.99931 13.0028C4.44552 13.0028 3.99793 12.5552 3.99793 12.0014V9.99862ZM8.99724 13.9966C8.99724 14.5503 8.54966 14.9979 7.99586 14.9979C7.44207 14.9979 6.99448 14.5503 6.99448 13.9966V7.99586C6.99448 7.44207 7.44207 6.99448 7.99586 6.99448C8.54966 6.99448 8.99724 7.44207 8.99724 7.99586V13.9966ZM12.0014 17.0007C12.0014 17.5545 11.5538 18.0021 11 18.0021C10.4462 18.0021 9.99862 17.5545 9.99862 17.0007V4.99931C9.99862 4.44552 10.4462 3.99793 11 3.99793C11.5538 3.99793 12.0014 4.44552 12.0014 4.99931V17.0007ZM14.9979 13.9966C14.9979 14.5503 14.5503 14.9979 13.9966 14.9979C13.4428 14.9979 12.9952 14.5503 12.9952 13.9966V7.99586C12.9952 7.44207 13.4428 6.99448 13.9966 6.99448C14.5503 6.99448 14.9979 7.44207 14.9979 7.99586V13.9966ZM18.0021 12.0014C18.0021 12.5552 17.5545 13.0028 17.0007 13.0028C16.4469 13.0028 15.9993 12.5552 15.9993 12.0014V9.99862C15.9993 9.44483 16.4469 8.99724 17.0007 8.99724C17.5545 8.99724 18.0021 9.44483 18.0021 9.99862V12.0014Z\"\/><\/svg><span class=\"responsivevoice-button__label\">Tekst oplezen<\/span><\/button> <\/p>\n<p>How do we measure CO2 emissions from peat soils? At the NOBV, we use three different methods: automatic chamber measurements that cover an area of approximately one square meter, Eddy Covariance (EC) towers that measure emissions over a larger area (approximately one hectare), and aircraft measurements taken over a large area (hundreds of hectares). All three systems are used in the research program, but the results have not yet been compared in detail. This study compares the insights provided by the automatic chamber measurements with those obtained using an EC tower.<\/p>\n<p><strong>Authors<\/strong>: Jim Boonman (VU), Alexander J.V. Buzacott (VU), Merit van den Berg (VU), Corine van Huissteden (VU), Ype van der Velde (VU)<\/p>\n<p><a href=\"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S1470160X24005788\">&gt; Read the paper here.<\/a><\/p>\n<p>\n<\/div><\/section><\/div><div class='flex_column av-1wpwym-c5815e95405205d765ca93e02e0efac4 av_one_half  avia-builder-el-48  el_after_av_one_half  el_before_av_heading  flex_column_div '     ><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-gvrs2m-957a736e58b3b71c03e22e502433484a\">\n.avia-image-container.av-gvrs2m-957a736e58b3b71c03e22e502433484a img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-gvrs2m-957a736e58b3b71c03e22e502433484a .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div  class='avia-image-container av-gvrs2m-957a736e58b3b71c03e22e502433484a av-styling- avia-align-center  avia-builder-el-49  avia-builder-el-no-sibling '   itemprop=\"image\" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/ImageObject\" ><div class=\"avia-image-container-inner\"><div class=\"avia-image-overlay-wrap\"><a href=\"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S1470160X24005788\" class=\"avia_image\" target=\"_blank\" rel=\"noopener noreferrer\"><img decoding=\"async\" class='wp-image-5322 avia-img-lazy-loading-not-5322 avia_image ' src=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Transparentautomated-192x300.jpg\" alt='' title='Transparentautomated'  height=\"300\" width=\"192\"  itemprop=\"thumbnailUrl\" srcset=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Transparentautomated-192x300.jpg 192w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Transparentautomated-452x705.jpg 452w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Transparentautomated.jpg 564w\" sizes=\"(max-width: 192px) 100vw, 192px\" \/><\/a><\/div><\/div><\/div><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-fu2tri-f744d84fa72c23b7bb8157fc2f5c1d03\">\n#top .av-special-heading.av-fu2tri-f744d84fa72c23b7bb8157fc2f5c1d03{\npadding-bottom:10px;\n}\nbody .av-special-heading.av-fu2tri-f744d84fa72c23b7bb8157fc2f5c1d03 .av-special-heading-tag .heading-char{\nfont-size:25px;\n}\n.av-special-heading.av-fu2tri-f744d84fa72c23b7bb8157fc2f5c1d03 .av-subheading{\nfont-size:15px;\n}\n<\/style>\n<div  class='av-special-heading av-fu2tri-f744d84fa72c23b7bb8157fc2f5c1d03 av-special-heading-h3 blockquote modern-quote  avia-builder-el-50  el_after_av_one_half  el_before_av_one_half '><h3 class='av-special-heading-tag'  itemprop=\"headline\"  >Rewetting drained peatlands through subsoil infiltration stabilises redox-dependent soil carbon and nutrient dynamics<\/h3><div class=\"special-heading-border\"><div class=\"special-heading-inner-border\"><\/div><\/div><\/div>\n<div class='flex_column av-2ospum-600e1dbc24204732f729866688c6224a av_one_half  avia-builder-el-51  el_after_av_heading  el_before_av_one_half  first flex_column_div '     ><section  class='av_textblock_section av-lsbjekrr-7886edb72b6dbd86fda607e9ee09b654'  itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div class='avia_textblock'  itemprop=\"text\" ><button class=\"responsivevoice-button\" type=\"button\" title=\"ResponsiveVoice Tap to Start\/Stop Speech\" data-rvtts-action=\"speak\" data-rvtts-text=\"Centuries of drainage have stimulated peat degradation in Dutch peat meadow areas. To counteract the resulting increase in greenhouse gas emissions and land subsidence, passive and active water infiltration systems (WIS) have been developed to rewet peat meadow areas. In this study, we investigated the effects of WIS systems on groundwater levels, pore water composition, and redox potential in four drained peatlands in the Netherlands to determine how they influence soil processes, particularly carbon and nutrient dynamics. Authors: Sarah Faye Harpenslager (B-Ware), Gijs van Dijk (B-Ware), Jim Boonman (VU), Stefan T.J. Weideveld (B-Ware),\u00a0 Bas van der Riet (B-Ware), Mariet M. Hefting (VU), Alfons J.P. Smolders (B-Ware) greater than Read the paper here.\" data-rvtts-voice=\"Dutch Female\" data-rvtts-brand-url=\"https:\/\/responsivevoice.org\/?utm_source=wordpress-plugin&amp;utm_medium=referral&amp;utm_campaign=powered-by\" data-rvtts-brand-label=\"Powered by ResponsiveVoice\"><svg class=\"rvtts-icon\" width=\"22\" height=\"22\" viewBox=\"0 0 22 22\" fill=\"currentColor\" aria-hidden=\"true\" focusable=\"false\"><path fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M11 0C4.92345 0 0 4.92345 0 11C0 13.2683 0.690345 15.3772 1.86621 17.1221L0.811724 21.0517L4.70345 20.0124C6.48621 21.2641 8.65586 22 11 22C17.0766 22 22 17.0766 22 11C22 4.92345 17.0766 0 11 0ZM3.99793 9.99862C3.99793 9.44483 4.44552 8.99724 4.99931 8.99724C5.5531 8.99724 6.00069 9.44483 6.00069 9.99862V12.0014C6.00069 12.5552 5.5531 13.0028 4.99931 13.0028C4.44552 13.0028 3.99793 12.5552 3.99793 12.0014V9.99862ZM8.99724 13.9966C8.99724 14.5503 8.54966 14.9979 7.99586 14.9979C7.44207 14.9979 6.99448 14.5503 6.99448 13.9966V7.99586C6.99448 7.44207 7.44207 6.99448 7.99586 6.99448C8.54966 6.99448 8.99724 7.44207 8.99724 7.99586V13.9966ZM12.0014 17.0007C12.0014 17.5545 11.5538 18.0021 11 18.0021C10.4462 18.0021 9.99862 17.5545 9.99862 17.0007V4.99931C9.99862 4.44552 10.4462 3.99793 11 3.99793C11.5538 3.99793 12.0014 4.44552 12.0014 4.99931V17.0007ZM14.9979 13.9966C14.9979 14.5503 14.5503 14.9979 13.9966 14.9979C13.4428 14.9979 12.9952 14.5503 12.9952 13.9966V7.99586C12.9952 7.44207 13.4428 6.99448 13.9966 6.99448C14.5503 6.99448 14.9979 7.44207 14.9979 7.99586V13.9966ZM18.0021 12.0014C18.0021 12.5552 17.5545 13.0028 17.0007 13.0028C16.4469 13.0028 15.9993 12.5552 15.9993 12.0014V9.99862C15.9993 9.44483 16.4469 8.99724 17.0007 8.99724C17.5545 8.99724 18.0021 9.44483 18.0021 9.99862V12.0014Z\"\/><\/svg><span class=\"responsivevoice-button__label\">Tekst oplezen<\/span><\/button> <\/p>\n<p>Centuries of drainage have stimulated peat degradation in Dutch peat meadow areas. To counteract the resulting increase in greenhouse gas emissions and land subsidence, passive and active water infiltration systems (WIS) have been developed to rewet peat meadow areas. In this study, we investigated the effects of WIS systems on groundwater levels, pore water composition, and redox potential in four drained peatlands in the Netherlands to determine how they influence soil processes, particularly carbon and nutrient dynamics.<\/p>\n<p><strong>Authors<\/strong>: Sarah Faye Harpenslager (B-Ware), Gijs van Dijk (B-Ware), Jim Boonman (VU), Stefan T.J. Weideveld (B-Ware),\u00a0 Bas van der Riet (B-Ware), Mariet M. Hefting (VU), Alfons J.P. Smolders (B-Ware)<\/p>\n<p><a href=\"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0016706124000168\">&gt; Read the paper here.<\/a><\/p>\n<p>\n<\/div><\/section><\/div><div class='flex_column av-2v7k1a-fbd2aa6ab616760f9e8277347a504a85 av_one_half  avia-builder-el-53  el_after_av_one_half  el_before_av_heading  flex_column_div '     ><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-lsbiqn7d-26ad005132954109f7665387fcf21ab3\">\n.avia-image-container.av-lsbiqn7d-26ad005132954109f7665387fcf21ab3 img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-lsbiqn7d-26ad005132954109f7665387fcf21ab3 .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div  class='avia-image-container av-lsbiqn7d-26ad005132954109f7665387fcf21ab3 av-styling- avia-align-center  avia-builder-el-54  avia-builder-el-no-sibling '   itemprop=\"image\" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/ImageObject\" ><div class=\"avia-image-container-inner\"><div class=\"avia-image-overlay-wrap\"><a href=\"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0016706124000168\" class=\"avia_image\" target=\"_blank\" rel=\"noopener noreferrer\"><img decoding=\"async\" class='wp-image-4647 avia-img-lazy-loading-not-4647 avia_image ' src=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/09\/Rewetting_drained_peatlands--192x300.jpg\" alt='' title='Rewetting_drained_peatlands-'  height=\"300\" width=\"192\"  itemprop=\"thumbnailUrl\" srcset=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/09\/Rewetting_drained_peatlands--192x300.jpg 192w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/09\/Rewetting_drained_peatlands--452x705.jpg 452w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/09\/Rewetting_drained_peatlands-.jpg 564w\" sizes=\"(max-width: 192px) 100vw, 192px\" \/><\/a><\/div><\/div><\/div><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-lqgsg8uf-6feef0b2eb5066dd0642e923ac4d5924\">\n#top .av-special-heading.av-lqgsg8uf-6feef0b2eb5066dd0642e923ac4d5924{\npadding-bottom:10px;\n}\nbody .av-special-heading.av-lqgsg8uf-6feef0b2eb5066dd0642e923ac4d5924 .av-special-heading-tag .heading-char{\nfont-size:25px;\n}\n.av-special-heading.av-lqgsg8uf-6feef0b2eb5066dd0642e923ac4d5924 .av-subheading{\nfont-size:15px;\n}\n<\/style>\n<div  class='av-special-heading av-lqgsg8uf-6feef0b2eb5066dd0642e923ac4d5924 av-special-heading-h3 blockquote modern-quote  avia-builder-el-55  el_after_av_one_half  el_before_av_one_half '><h3 class='av-special-heading-tag'  itemprop=\"headline\"  >Physiological processes affecting methane transport by wetland vegetation \u2013 A review<\/h3><div class=\"special-heading-border\"><div class=\"special-heading-inner-border\"><\/div><\/div><\/div>\n<div class='flex_column av-e6erim-911a85a3d0edd911c565ec5b95afc2e0 av_one_half  avia-builder-el-56  el_after_av_heading  el_before_av_one_half  first flex_column_div '     ><section  class='av_textblock_section av-m7vttl5r-29275047b3aac4616ba65e9c703cf0c4'  itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div class='avia_textblock'  itemprop=\"text\" ><button class=\"responsivevoice-button\" type=\"button\" title=\"ResponsiveVoice Tap to Start\/Stop Speech\" data-rvtts-action=\"speak\" data-rvtts-text=\"Plants in wetlands possess traits that allow them to transport oxygen to their roots while simultaneously transporting methane (CH4) from the sediment to the atmosphere. The contribution of these vegetation-driven emissions to total wetland methane emissions is uncertain. To accurately quantify these emissions, it is important to understand the physiological processes that drive plant-mediated methane transport. This review describes the current state of knowledge regarding methane transport by trees and plants in wetlands. Authors: R.J.E.\u00a0Vroom\u00a0((Radboud Universiteit Nijmegen),\u00a0M.\u00a0van den Berg (Vrije Universiteit),\u00a0S.R.\u00a0Pangala (Lancaster University) O.E.\u00a0van der Scheer (Radboud Universiteit Nijmegen), B.K.\u00a0Sorrell (Aarhus University) greater than Read the paper here.\" data-rvtts-voice=\"Dutch Female\" data-rvtts-brand-url=\"https:\/\/responsivevoice.org\/?utm_source=wordpress-plugin&amp;utm_medium=referral&amp;utm_campaign=powered-by\" data-rvtts-brand-label=\"Powered by ResponsiveVoice\"><svg class=\"rvtts-icon\" width=\"22\" height=\"22\" viewBox=\"0 0 22 22\" fill=\"currentColor\" aria-hidden=\"true\" focusable=\"false\"><path fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M11 0C4.92345 0 0 4.92345 0 11C0 13.2683 0.690345 15.3772 1.86621 17.1221L0.811724 21.0517L4.70345 20.0124C6.48621 21.2641 8.65586 22 11 22C17.0766 22 22 17.0766 22 11C22 4.92345 17.0766 0 11 0ZM3.99793 9.99862C3.99793 9.44483 4.44552 8.99724 4.99931 8.99724C5.5531 8.99724 6.00069 9.44483 6.00069 9.99862V12.0014C6.00069 12.5552 5.5531 13.0028 4.99931 13.0028C4.44552 13.0028 3.99793 12.5552 3.99793 12.0014V9.99862ZM8.99724 13.9966C8.99724 14.5503 8.54966 14.9979 7.99586 14.9979C7.44207 14.9979 6.99448 14.5503 6.99448 13.9966V7.99586C6.99448 7.44207 7.44207 6.99448 7.99586 6.99448C8.54966 6.99448 8.99724 7.44207 8.99724 7.99586V13.9966ZM12.0014 17.0007C12.0014 17.5545 11.5538 18.0021 11 18.0021C10.4462 18.0021 9.99862 17.5545 9.99862 17.0007V4.99931C9.99862 4.44552 10.4462 3.99793 11 3.99793C11.5538 3.99793 12.0014 4.44552 12.0014 4.99931V17.0007ZM14.9979 13.9966C14.9979 14.5503 14.5503 14.9979 13.9966 14.9979C13.4428 14.9979 12.9952 14.5503 12.9952 13.9966V7.99586C12.9952 7.44207 13.4428 6.99448 13.9966 6.99448C14.5503 6.99448 14.9979 7.44207 14.9979 7.99586V13.9966ZM18.0021 12.0014C18.0021 12.5552 17.5545 13.0028 17.0007 13.0028C16.4469 13.0028 15.9993 12.5552 15.9993 12.0014V9.99862C15.9993 9.44483 16.4469 8.99724 17.0007 8.99724C17.5545 8.99724 18.0021 9.44483 18.0021 9.99862V12.0014Z\"\/><\/svg><span class=\"responsivevoice-button__label\">Tekst oplezen<\/span><\/button> <\/p>\n<p>Plants in wetlands possess traits that allow them to transport oxygen to their roots while simultaneously transporting methane (CH4) from the sediment to the atmosphere. The contribution of these vegetation-driven emissions to total wetland methane emissions is uncertain. To accurately quantify these emissions, it is important to understand the physiological processes that drive plant-mediated methane transport. This review describes the current state of knowledge regarding methane transport by trees and plants in wetlands.<\/p>\n<p><strong>Authors<\/strong>: R.J.E.\u00a0Vroom\u00a0((Radboud Universiteit Nijmegen),\u00a0M.\u00a0van den Berg (Vrije Universiteit),\u00a0S.R.\u00a0Pangala (Lancaster University) O.E.\u00a0van der Scheer (Radboud Universiteit Nijmegen), B.K.\u00a0Sorrell (Aarhus University)<\/p>\n<p><a href=\"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0304377022000596?via%3Dihub\">&gt; Read the paper here.<\/a><\/p>\n<p>\n<\/div><\/section><\/div><div class='flex_column av-6lyt3i-5db80846d6e55f446495a5059d856436 av_one_half  avia-builder-el-58  el_after_av_one_half  el_before_av_heading  flex_column_div '     ><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-3yile6-8d680a6c744ad0355a1d5adce555ccfd\">\n.avia-image-container.av-3yile6-8d680a6c744ad0355a1d5adce555ccfd img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-3yile6-8d680a6c744ad0355a1d5adce555ccfd .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div  class='avia-image-container av-3yile6-8d680a6c744ad0355a1d5adce555ccfd av-styling- avia-align-center  avia-builder-el-59  avia-builder-el-no-sibling '   itemprop=\"image\" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/ImageObject\" ><div class=\"avia-image-container-inner\"><div class=\"avia-image-overlay-wrap\"><a href=\"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0304377022000596?via%3Dihub \" class=\"avia_image\" target=\"_blank\" rel=\"noopener noreferrer\"><img decoding=\"async\" class='wp-image-5664 avia-img-lazy-loading-not-5664 avia_image ' src=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/03\/Physiological_processes_affecting_methane-192x300.jpg\" alt='' title='Physiological_processes_affecting_methane'  height=\"300\" width=\"192\"  itemprop=\"thumbnailUrl\" srcset=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/03\/Physiological_processes_affecting_methane-192x300.jpg 192w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/03\/Physiological_processes_affecting_methane-452x705.jpg 452w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/03\/Physiological_processes_affecting_methane.jpg 564w\" sizes=\"(max-width: 192px) 100vw, 192px\" \/><\/a><\/div><\/div><\/div><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-cz4ju6-2c72bf62b9c776cfe4499c1c979dace9\">\n#top .av-special-heading.av-cz4ju6-2c72bf62b9c776cfe4499c1c979dace9{\npadding-bottom:10px;\n}\nbody .av-special-heading.av-cz4ju6-2c72bf62b9c776cfe4499c1c979dace9 .av-special-heading-tag .heading-char{\nfont-size:25px;\n}\n.av-special-heading.av-cz4ju6-2c72bf62b9c776cfe4499c1c979dace9 .av-subheading{\nfont-size:15px;\n}\n<\/style>\n<div  class='av-special-heading av-cz4ju6-2c72bf62b9c776cfe4499c1c979dace9 av-special-heading-h3 blockquote modern-quote  avia-builder-el-60  el_after_av_one_half  el_before_av_one_half '><h3 class='av-special-heading-tag'  itemprop=\"headline\"  >Redox potential is a robust indicator for decomposition processes in drained agricultural peat soils: A valuable tool in monitoring peatland wetting efforts<\/h3><div class=\"special-heading-border\"><div class=\"special-heading-inner-border\"><\/div><\/div><\/div>\n<div class='flex_column av-2inb66-bf8548dbbe66c79a93f9b9eac1654491 av_one_half  avia-builder-el-61  el_after_av_heading  el_before_av_one_half  first flex_column_div '     ><section  class='av_textblock_section av-lqgsftdm-e2ce4d38787329e235adc95e9c139598'  itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div class='avia_textblock'  itemprop=\"text\" ><button class=\"responsivevoice-button\" type=\"button\" title=\"ResponsiveVoice Tap to Start\/Stop Speech\" data-rvtts-action=\"speak\" data-rvtts-text=\"Because aerobic oxidation (oxidation with oxygen, above the groundwater level) accounts for the largest share of net peat decomposition, anaerobic oxidation (without oxygen) often remains understudied. In this NOBV study, all forms of oxidation in peat soils were successfully mapped using redox sensors. Using these sensors, we learned how soil processes vary from location to location and how these processes change after submerged drainage systems are installed: for example, the depletion of iron and sulfate reserves in the soil increases the risk of methane formation, especially near submerged drains. This study also revealed that oxygen penetration into the soil is often limited at low groundwater levels. Authors: Jim Boonman (VU), Sarah Faye Harpenslager (B-Ware), Gijs van Dijk (B-Ware), Alfons J.P. Smolders (B-Ware), Mariet M. Hefting (VU), Bas van der Riet (B-Ware), Ype van der Velde (VU) greater than Read the paper here.\" data-rvtts-voice=\"Dutch Female\" data-rvtts-brand-url=\"https:\/\/responsivevoice.org\/?utm_source=wordpress-plugin&amp;utm_medium=referral&amp;utm_campaign=powered-by\" data-rvtts-brand-label=\"Powered by ResponsiveVoice\"><svg class=\"rvtts-icon\" width=\"22\" height=\"22\" viewBox=\"0 0 22 22\" fill=\"currentColor\" aria-hidden=\"true\" focusable=\"false\"><path fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M11 0C4.92345 0 0 4.92345 0 11C0 13.2683 0.690345 15.3772 1.86621 17.1221L0.811724 21.0517L4.70345 20.0124C6.48621 21.2641 8.65586 22 11 22C17.0766 22 22 17.0766 22 11C22 4.92345 17.0766 0 11 0ZM3.99793 9.99862C3.99793 9.44483 4.44552 8.99724 4.99931 8.99724C5.5531 8.99724 6.00069 9.44483 6.00069 9.99862V12.0014C6.00069 12.5552 5.5531 13.0028 4.99931 13.0028C4.44552 13.0028 3.99793 12.5552 3.99793 12.0014V9.99862ZM8.99724 13.9966C8.99724 14.5503 8.54966 14.9979 7.99586 14.9979C7.44207 14.9979 6.99448 14.5503 6.99448 13.9966V7.99586C6.99448 7.44207 7.44207 6.99448 7.99586 6.99448C8.54966 6.99448 8.99724 7.44207 8.99724 7.99586V13.9966ZM12.0014 17.0007C12.0014 17.5545 11.5538 18.0021 11 18.0021C10.4462 18.0021 9.99862 17.5545 9.99862 17.0007V4.99931C9.99862 4.44552 10.4462 3.99793 11 3.99793C11.5538 3.99793 12.0014 4.44552 12.0014 4.99931V17.0007ZM14.9979 13.9966C14.9979 14.5503 14.5503 14.9979 13.9966 14.9979C13.4428 14.9979 12.9952 14.5503 12.9952 13.9966V7.99586C12.9952 7.44207 13.4428 6.99448 13.9966 6.99448C14.5503 6.99448 14.9979 7.44207 14.9979 7.99586V13.9966ZM18.0021 12.0014C18.0021 12.5552 17.5545 13.0028 17.0007 13.0028C16.4469 13.0028 15.9993 12.5552 15.9993 12.0014V9.99862C15.9993 9.44483 16.4469 8.99724 17.0007 8.99724C17.5545 8.99724 18.0021 9.44483 18.0021 9.99862V12.0014Z\"\/><\/svg><span class=\"responsivevoice-button__label\">Tekst oplezen<\/span><\/button> <\/p>\n<p>Because aerobic oxidation (oxidation with oxygen, above the groundwater level) accounts for the largest share of net peat decomposition, anaerobic oxidation (without oxygen) often remains understudied. In this NOBV study, all forms of oxidation in peat soils were successfully mapped using redox sensors. Using these sensors, we learned how soil processes vary from location to location and how these processes change after submerged drainage systems are installed: for example, the depletion of iron and sulfate reserves in the soil increases the risk of methane formation, especially near submerged drains. This study also revealed that oxygen penetration into the soil is often limited at low groundwater levels.<\/p>\n<p><strong>Authors<\/strong>: Jim Boonman (VU), Sarah Faye Harpenslager (B-Ware), Gijs van Dijk (B-Ware), Alfons J.P. Smolders (B-Ware), Mariet M. Hefting (VU), Bas van der Riet (B-Ware), Ype van der Velde (VU)<\/p>\n<p><a href=\"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0016706123004056\">&gt; Read the paper here.<\/a><\/p>\n<p>\n<\/div><\/section><\/div><div class='flex_column av-a5ds9q-8a6530fb3e54e1a292d24e66f01f5c06 av_one_half  avia-builder-el-63  el_after_av_one_half  el_before_av_heading  flex_column_div '     ><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-9ud9ku-ca1c07c38db81f1369716640d9085b93\">\n.avia-image-container.av-9ud9ku-ca1c07c38db81f1369716640d9085b93 img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-9ud9ku-ca1c07c38db81f1369716640d9085b93 .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div  class='avia-image-container av-9ud9ku-ca1c07c38db81f1369716640d9085b93 av-styling- avia-align-center  avia-builder-el-64  avia-builder-el-no-sibling '   itemprop=\"image\" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/ImageObject\" ><div class=\"avia-image-container-inner\"><div class=\"avia-image-overlay-wrap\"><a href=\"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0016706123004056\" class=\"avia_image\" target=\"_blank\" rel=\"noopener noreferrer\"><img decoding=\"async\" class='wp-image-5324 avia-img-lazy-loading-not-5324 avia_image ' src=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Redoxpotential-192x300.jpg\" alt='' title='Redoxpotential'  height=\"300\" width=\"192\"  itemprop=\"thumbnailUrl\" srcset=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Redoxpotential-192x300.jpg 192w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Redoxpotential-452x705.jpg 452w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Redoxpotential.jpg 564w\" sizes=\"(max-width: 192px) 100vw, 192px\" \/><\/a><\/div><\/div><\/div><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-2m4sc4-e8dfdd00180c5368f0743689c8654894\">\n#top .av-special-heading.av-2m4sc4-e8dfdd00180c5368f0743689c8654894{\npadding-bottom:10px;\n}\nbody .av-special-heading.av-2m4sc4-e8dfdd00180c5368f0743689c8654894 .av-special-heading-tag .heading-char{\nfont-size:25px;\n}\n.av-special-heading.av-2m4sc4-e8dfdd00180c5368f0743689c8654894 .av-subheading{\nfont-size:15px;\n}\n<\/style>\n<div  class='av-special-heading av-2m4sc4-e8dfdd00180c5368f0743689c8654894 av-special-heading-h3 blockquote modern-quote  avia-builder-el-65  el_after_av_one_half  el_before_av_one_half '><h3 class='av-special-heading-tag'  itemprop=\"headline\"  >Cutting peatland CO2 emissions with water management practices<\/h3><div class=\"special-heading-border\"><div class=\"special-heading-inner-border\"><\/div><\/div><\/div>\n<div class='flex_column av-a3grpa-5d2e2b4c4b2dbf02c36b4e6b6d18e890 av_one_half  avia-builder-el-66  el_after_av_heading  el_before_av_one_half  first flex_column_div '     ><section  class='av_textblock_section av-2evem4-46eda3e0a3d0580188269e8cfe025782'  itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div class='avia_textblock'  itemprop=\"text\" ><button class=\"responsivevoice-button\" type=\"button\" title=\"ResponsiveVoice Tap to Start\/Stop Speech\" data-rvtts-action=\"speak\" data-rvtts-text=\"In October 2022, the first NOBV scientific article, titled \u201cCutting peatland CO2 emissions with water management practices,\u201d was accepted for publication in the Journal of Biogeosciences. The article discusses a new method for simulating peat degradation based on soil moisture and temperature. Authors: Jim Boonman (Vrije Universiteit), Mariet M. Hefting(Universiteit Utrecht), Corine J. A. van Huissteden(Vrije Universiteit), Merit van den Berg (Vrije Universiteit), Jacobus (Ko) van Huissteden(Vrije Universiteit), Gilles Erkens (Deltares), Roel Melman (Deltares), and Ype van der Velde (Vrije Universiteit) greater than Read the paper here.\" data-rvtts-voice=\"Dutch Female\" data-rvtts-brand-url=\"https:\/\/responsivevoice.org\/?utm_source=wordpress-plugin&amp;utm_medium=referral&amp;utm_campaign=powered-by\" data-rvtts-brand-label=\"Powered by ResponsiveVoice\"><svg class=\"rvtts-icon\" width=\"22\" height=\"22\" viewBox=\"0 0 22 22\" fill=\"currentColor\" aria-hidden=\"true\" focusable=\"false\"><path fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M11 0C4.92345 0 0 4.92345 0 11C0 13.2683 0.690345 15.3772 1.86621 17.1221L0.811724 21.0517L4.70345 20.0124C6.48621 21.2641 8.65586 22 11 22C17.0766 22 22 17.0766 22 11C22 4.92345 17.0766 0 11 0ZM3.99793 9.99862C3.99793 9.44483 4.44552 8.99724 4.99931 8.99724C5.5531 8.99724 6.00069 9.44483 6.00069 9.99862V12.0014C6.00069 12.5552 5.5531 13.0028 4.99931 13.0028C4.44552 13.0028 3.99793 12.5552 3.99793 12.0014V9.99862ZM8.99724 13.9966C8.99724 14.5503 8.54966 14.9979 7.99586 14.9979C7.44207 14.9979 6.99448 14.5503 6.99448 13.9966V7.99586C6.99448 7.44207 7.44207 6.99448 7.99586 6.99448C8.54966 6.99448 8.99724 7.44207 8.99724 7.99586V13.9966ZM12.0014 17.0007C12.0014 17.5545 11.5538 18.0021 11 18.0021C10.4462 18.0021 9.99862 17.5545 9.99862 17.0007V4.99931C9.99862 4.44552 10.4462 3.99793 11 3.99793C11.5538 3.99793 12.0014 4.44552 12.0014 4.99931V17.0007ZM14.9979 13.9966C14.9979 14.5503 14.5503 14.9979 13.9966 14.9979C13.4428 14.9979 12.9952 14.5503 12.9952 13.9966V7.99586C12.9952 7.44207 13.4428 6.99448 13.9966 6.99448C14.5503 6.99448 14.9979 7.44207 14.9979 7.99586V13.9966ZM18.0021 12.0014C18.0021 12.5552 17.5545 13.0028 17.0007 13.0028C16.4469 13.0028 15.9993 12.5552 15.9993 12.0014V9.99862C15.9993 9.44483 16.4469 8.99724 17.0007 8.99724C17.5545 8.99724 18.0021 9.44483 18.0021 9.99862V12.0014Z\"\/><\/svg><span class=\"responsivevoice-button__label\">Tekst oplezen<\/span><\/button> <\/p>\n<p>In October 2022, the first NOBV scientific article, titled \u201cCutting peatland CO2 emissions with water management practices,\u201d was accepted for publication in the Journal of Biogeosciences. The article discusses a new method for simulating peat degradation based on soil moisture and temperature.<\/p>\n<p><strong>Authors<\/strong>: Jim Boonman (Vrije Universiteit), Mariet M. Hefting(Universiteit Utrecht), Corine J. A. van Huissteden(Vrije Universiteit), Merit van den Berg (Vrije Universiteit), Jacobus (Ko) van Huissteden(Vrije Universiteit), Gilles Erkens (Deltares), Roel Melman (Deltares), and Ype van der Velde (Vrije Universiteit)<\/p>\n<p><a href=\"https:\/\/bg.copernicus.org\/articles\/19\/5707\/2022\/\">&gt; Read the paper here.<\/a><\/p>\n<p>\n<\/div><\/section><\/div><div class='flex_column av-8gezxa-22711f5c2d830138a5cd687c731184df av_one_half  avia-builder-el-68  el_after_av_one_half  el_before_av_hr  flex_column_div '     ><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-79y5ce-b76044c9fa95ea1c13112a46674c6dbc\">\n.avia-image-container.av-79y5ce-b76044c9fa95ea1c13112a46674c6dbc img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-79y5ce-b76044c9fa95ea1c13112a46674c6dbc .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div  class='avia-image-container av-79y5ce-b76044c9fa95ea1c13112a46674c6dbc av-styling- avia-align-center  avia-builder-el-69  avia-builder-el-no-sibling '   itemprop=\"image\" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/ImageObject\" ><div class=\"avia-image-container-inner\"><div class=\"avia-image-overlay-wrap\"><a href=\"https:\/\/bg.copernicus.org\/articles\/19\/5707\/2022\/\" class=\"avia_image\" target=\"_blank\" rel=\"noopener noreferrer\"><img decoding=\"async\" class='wp-image-5328 avia-img-lazy-loading-not-5328 avia_image ' src=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Cuttingpeatland-192x300.jpg\" alt='' title='Cuttingpeatland'  height=\"300\" width=\"192\"  itemprop=\"thumbnailUrl\" srcset=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Cuttingpeatland-192x300.jpg 192w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Cuttingpeatland-452x705.jpg 452w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/Cuttingpeatland.jpg 564w\" sizes=\"(max-width: 192px) 100vw, 192px\" \/><\/a><\/div><\/div><\/div><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-2wzzo4-2ec420fa2e333b5c3c9a97cdffcb912a\">\n#top .hr.hr-invisible.av-2wzzo4-2ec420fa2e333b5c3c9a97cdffcb912a{\nheight:30px;\n}\n<\/style>\n<div  class='hr av-2wzzo4-2ec420fa2e333b5c3c9a97cdffcb912a hr-invisible  avia-builder-el-70  el_after_av_one_half  el_before_av_heading '><span class='hr-inner '><span class=\"hr-inner-style\"><\/span><\/span><\/div>\n\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-24bdac-eac2d23053a57c952dfc6719448ca86e\">\n#top .av-special-heading.av-24bdac-eac2d23053a57c952dfc6719448ca86e{\npadding-bottom:10px;\n}\nbody .av-special-heading.av-24bdac-eac2d23053a57c952dfc6719448ca86e .av-special-heading-tag .heading-char{\nfont-size:25px;\n}\n.av-special-heading.av-24bdac-eac2d23053a57c952dfc6719448ca86e .av-subheading{\nfont-size:15px;\n}\n<\/style>\n<div  class='av-special-heading av-24bdac-eac2d23053a57c952dfc6719448ca86e av-special-heading-h3 blockquote modern-quote  avia-builder-el-71  el_after_av_hr  el_before_av_one_half '><h3 class='av-special-heading-tag'  itemprop=\"headline\"  >Probabilistic Estimation of InSAR Displacement Phase Guided by Contextual Information and Artificial Intelligence<\/h3><div class=\"special-heading-border\"><div class=\"special-heading-inner-border\"><\/div><\/div><\/div>\n<div class='flex_column av-6hlhim-dbf3f0b29eefab7245e050792ddecb80 av_one_half  avia-builder-el-72  el_after_av_heading  el_before_av_one_half  first flex_column_div '     ><section  class='av_textblock_section av-1v0k1o-525b9043ee25eab4da68c3590d8a4624'  itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div class='avia_textblock'  itemprop=\"text\" ><button class=\"responsivevoice-button\" type=\"button\" title=\"ResponsiveVoice Tap to Start\/Stop Speech\" data-rvtts-action=\"speak\" data-rvtts-text=\"The NOBV is working closely with the NWA-LOSS (Living on Soft Soils) research program and the Groene Hart Regional Deal on Soil Subsidence to prepare InSAR data for determining soil subsidence in peat meadow areas. PhD Philip Conroy (Delft University of Technology\/NWA-LOSS) wrote a paper on the use of InSAR for monitoring soil movement in Dutch peatlands, titled \u201cProbabilistic Estimation of InSAR Displacement Phase Guided by Contextual Information and Artificial Intelligence.\u201d Authors: Philip Conroy (TU Delft), Simon A.N. van Diepen (TU Delft),\u00a0Sanneke van Asselen (Deltares), Gilles Erkens (Deltares), Freek J. van Leijen (TU Delft), Ramon F. Hanssen (TU Delft) greater than Read the paper here.\" data-rvtts-voice=\"Dutch Female\" data-rvtts-brand-url=\"https:\/\/responsivevoice.org\/?utm_source=wordpress-plugin&amp;utm_medium=referral&amp;utm_campaign=powered-by\" data-rvtts-brand-label=\"Powered by ResponsiveVoice\"><svg class=\"rvtts-icon\" width=\"22\" height=\"22\" viewBox=\"0 0 22 22\" fill=\"currentColor\" aria-hidden=\"true\" focusable=\"false\"><path fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M11 0C4.92345 0 0 4.92345 0 11C0 13.2683 0.690345 15.3772 1.86621 17.1221L0.811724 21.0517L4.70345 20.0124C6.48621 21.2641 8.65586 22 11 22C17.0766 22 22 17.0766 22 11C22 4.92345 17.0766 0 11 0ZM3.99793 9.99862C3.99793 9.44483 4.44552 8.99724 4.99931 8.99724C5.5531 8.99724 6.00069 9.44483 6.00069 9.99862V12.0014C6.00069 12.5552 5.5531 13.0028 4.99931 13.0028C4.44552 13.0028 3.99793 12.5552 3.99793 12.0014V9.99862ZM8.99724 13.9966C8.99724 14.5503 8.54966 14.9979 7.99586 14.9979C7.44207 14.9979 6.99448 14.5503 6.99448 13.9966V7.99586C6.99448 7.44207 7.44207 6.99448 7.99586 6.99448C8.54966 6.99448 8.99724 7.44207 8.99724 7.99586V13.9966ZM12.0014 17.0007C12.0014 17.5545 11.5538 18.0021 11 18.0021C10.4462 18.0021 9.99862 17.5545 9.99862 17.0007V4.99931C9.99862 4.44552 10.4462 3.99793 11 3.99793C11.5538 3.99793 12.0014 4.44552 12.0014 4.99931V17.0007ZM14.9979 13.9966C14.9979 14.5503 14.5503 14.9979 13.9966 14.9979C13.4428 14.9979 12.9952 14.5503 12.9952 13.9966V7.99586C12.9952 7.44207 13.4428 6.99448 13.9966 6.99448C14.5503 6.99448 14.9979 7.44207 14.9979 7.99586V13.9966ZM18.0021 12.0014C18.0021 12.5552 17.5545 13.0028 17.0007 13.0028C16.4469 13.0028 15.9993 12.5552 15.9993 12.0014V9.99862C15.9993 9.44483 16.4469 8.99724 17.0007 8.99724C17.5545 8.99724 18.0021 9.44483 18.0021 9.99862V12.0014Z\"\/><\/svg><span class=\"responsivevoice-button__label\">Tekst oplezen<\/span><\/button> <\/p>\n<p>The NOBV is working closely with the NWA-LOSS (Living on Soft Soils) research program and the Groene Hart Regional Deal on Soil Subsidence to prepare InSAR data for determining soil subsidence in peat meadow areas. PhD Philip Conroy (Delft University of Technology\/NWA-LOSS) wrote a paper on the use of InSAR for monitoring soil movement in Dutch peatlands, titled &#8220;Probabilistic Estimation of InSAR Displacement Phase Guided by Contextual Information and Artificial Intelligence.&#8221;<\/p>\n<p><strong>Authors<\/strong>: Philip Conroy (TU Delft), Simon A.N. van Diepen (TU Delft),\u00a0Sanneke van Asselen (Deltares), Gilles Erkens (Deltares), Freek J. van Leijen (TU Delft), Ramon F. Hanssen (TU Delft)<\/p>\n<p><a href=\"https:\/\/ieeexplore.ieee.org\/document\/9874898\/authors#authors\">&gt; Read the paper here.<\/a><\/p>\n<p>\n<\/div><\/section><\/div><div class='flex_column av-4hcyou-57a866dfd8b9d7f5f1856f3cfae5e513 av_one_half  avia-builder-el-74  el_after_av_one_half  el_before_av_heading  flex_column_div '     ><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-2rdb6m-fbbc97cda2b81262fef1a10f3a6fd11e\">\n.avia-image-container.av-2rdb6m-fbbc97cda2b81262fef1a10f3a6fd11e img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-2rdb6m-fbbc97cda2b81262fef1a10f3a6fd11e .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div  class='avia-image-container av-2rdb6m-fbbc97cda2b81262fef1a10f3a6fd11e av-styling- avia-align-center  avia-builder-el-75  avia-builder-el-no-sibling '   itemprop=\"image\" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/ImageObject\" ><div class=\"avia-image-container-inner\"><div class=\"avia-image-overlay-wrap\"><a href=\"https:\/\/ieeexplore.ieee.org\/document\/9874898\/authors#authors\" class=\"avia_image\" target=\"_blank\" rel=\"noopener noreferrer\"><img decoding=\"async\" class='wp-image-5326 avia-img-lazy-loading-not-5326 avia_image ' src=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/ProbabilisticEstimation-192x300.jpg\" alt='' title='ProbabilisticEstimation'  height=\"300\" width=\"192\"  itemprop=\"thumbnailUrl\" srcset=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/ProbabilisticEstimation-192x300.jpg 192w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/ProbabilisticEstimation-452x705.jpg 452w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2024\/11\/ProbabilisticEstimation.jpg 564w\" sizes=\"(max-width: 192px) 100vw, 192px\" \/><\/a><\/div><\/div><\/div><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-m7ddffmk-84738568ac2756358dc048257c0c7c69\">\n#top .av-special-heading.av-m7ddffmk-84738568ac2756358dc048257c0c7c69{\npadding-bottom:10px;\n}\nbody .av-special-heading.av-m7ddffmk-84738568ac2756358dc048257c0c7c69 .av-special-heading-tag .heading-char{\nfont-size:25px;\n}\n.av-special-heading.av-m7ddffmk-84738568ac2756358dc048257c0c7c69 .av-subheading{\nfont-size:15px;\n}\n<\/style>\n<div  class='av-special-heading av-m7ddffmk-84738568ac2756358dc048257c0c7c69 av-special-heading-h3 blockquote modern-quote  avia-builder-el-76  el_after_av_one_half  el_before_av_one_half '><h3 class='av-special-heading-tag'  itemprop=\"headline\"  >Verticale beweging van de veenbodem: meettechnieken en ervaringen te Zegveld<\/h3><div class=\"special-heading-border\"><div class=\"special-heading-inner-border\"><\/div><\/div><\/div>\n<div class='flex_column av-78ds0u-345035a7f2708c219d094236aca190a8 av_one_half  avia-builder-el-77  el_after_av_heading  el_before_av_one_half  first flex_column_div '     ><section  class='av_textblock_section av-m7vtzdqm-b2748ddacc5f242dda13180c4ca31a8a'  itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div class='avia_textblock'  itemprop=\"text\" ><button class=\"responsivevoice-button\" type=\"button\" title=\"ResponsiveVoice Tap to Start\/Stop Speech\" data-rvtts-action=\"speak\" data-rvtts-text=\"This article presents the initial results of the measured vertical ground movement from two different measuring systems at Zegveld (Utrecht). The measuring systems differ in the positions, types of anchors, and sensors used to record the ground movement. One measuring system (extensometer) uses anchors at various depths in the ground, while the other (VSM sensor) uses a grid placed on the surface. The ground moves up and down in the order of centimeters. Combined with satellite data, both measuring systems can play a significant role in addressing the subsidence task in the peat meadow area. Authors: Dion van Deijl (KnowH2O), Sanneke van Asselen (Deltares), Gilles Erkens (Deltares), Bernard Voortman (Moisture Matters), G\u00e9 van den Eertwegh (KnowH2O) greater than Read the paper here.\" data-rvtts-voice=\"Dutch Female\" data-rvtts-brand-url=\"https:\/\/responsivevoice.org\/?utm_source=wordpress-plugin&amp;utm_medium=referral&amp;utm_campaign=powered-by\" data-rvtts-brand-label=\"Powered by ResponsiveVoice\"><svg class=\"rvtts-icon\" width=\"22\" height=\"22\" viewBox=\"0 0 22 22\" fill=\"currentColor\" aria-hidden=\"true\" focusable=\"false\"><path fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M11 0C4.92345 0 0 4.92345 0 11C0 13.2683 0.690345 15.3772 1.86621 17.1221L0.811724 21.0517L4.70345 20.0124C6.48621 21.2641 8.65586 22 11 22C17.0766 22 22 17.0766 22 11C22 4.92345 17.0766 0 11 0ZM3.99793 9.99862C3.99793 9.44483 4.44552 8.99724 4.99931 8.99724C5.5531 8.99724 6.00069 9.44483 6.00069 9.99862V12.0014C6.00069 12.5552 5.5531 13.0028 4.99931 13.0028C4.44552 13.0028 3.99793 12.5552 3.99793 12.0014V9.99862ZM8.99724 13.9966C8.99724 14.5503 8.54966 14.9979 7.99586 14.9979C7.44207 14.9979 6.99448 14.5503 6.99448 13.9966V7.99586C6.99448 7.44207 7.44207 6.99448 7.99586 6.99448C8.54966 6.99448 8.99724 7.44207 8.99724 7.99586V13.9966ZM12.0014 17.0007C12.0014 17.5545 11.5538 18.0021 11 18.0021C10.4462 18.0021 9.99862 17.5545 9.99862 17.0007V4.99931C9.99862 4.44552 10.4462 3.99793 11 3.99793C11.5538 3.99793 12.0014 4.44552 12.0014 4.99931V17.0007ZM14.9979 13.9966C14.9979 14.5503 14.5503 14.9979 13.9966 14.9979C13.4428 14.9979 12.9952 14.5503 12.9952 13.9966V7.99586C12.9952 7.44207 13.4428 6.99448 13.9966 6.99448C14.5503 6.99448 14.9979 7.44207 14.9979 7.99586V13.9966ZM18.0021 12.0014C18.0021 12.5552 17.5545 13.0028 17.0007 13.0028C16.4469 13.0028 15.9993 12.5552 15.9993 12.0014V9.99862C15.9993 9.44483 16.4469 8.99724 17.0007 8.99724C17.5545 8.99724 18.0021 9.44483 18.0021 9.99862V12.0014Z\"\/><\/svg><span class=\"responsivevoice-button__label\">Tekst oplezen<\/span><\/button> <\/p>\n<p>This article presents the initial results of the measured vertical ground movement from two different measuring systems at Zegveld (Utrecht). The measuring systems differ in the positions, types of anchors, and sensors used to record the ground movement. One measuring system (extensometer) uses anchors at various depths in the ground, while the other (VSM sensor) uses a grid placed on the surface. The ground moves up and down in the order of centimeters. Combined with satellite data, both measuring systems can play a significant role in addressing the subsidence task in the peat meadow area.<\/p>\n<p><strong>Authors<\/strong>: Dion van Deijl (KnowH2O), Sanneke van Asselen (Deltares), Gilles Erkens (Deltares), Bernard Voortman (Moisture Matters), G\u00e9 van den Eertwegh (KnowH2O)<\/p>\n<p><a href=\"https:\/\/www.nhv.nu\/wp-content\/uploads\/2022\/07\/330434_NHV_02_Stromingen-2-2022-ARTIKEL-DEIJL-LR.pdf\"><span style=\"font-style: inherit; font-weight: inherit;\">&gt; Read the paper here.<\/span><\/a><\/p>\n<p>\n<\/div><\/section><\/div><div class='flex_column av-2tcwce-3e60d46324cb85697cce2ef5716ca1f0 av_one_half  avia-builder-el-79  el_after_av_one_half  el_before_av_heading  flex_column_div '     ><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-m680o1ax-28bd4e9c07ca1a92280b3bff3d7545e1\">\n.avia-image-container.av-m680o1ax-28bd4e9c07ca1a92280b3bff3d7545e1 img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-m680o1ax-28bd4e9c07ca1a92280b3bff3d7545e1 .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div  class='avia-image-container av-m680o1ax-28bd4e9c07ca1a92280b3bff3d7545e1 av-styling- avia-align-center  avia-builder-el-80  avia-builder-el-no-sibling '   itemprop=\"image\" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/ImageObject\" ><div class=\"avia-image-container-inner\"><div class=\"avia-image-overlay-wrap\"><a href=\"https:\/\/www.nhv.nu\/wp-content\/uploads\/2022\/07\/330434_NHV_02_Stromingen-2-2022-ARTIKEL-DEIJL-LR.pdf\" class=\"avia_image\" target=\"_blank\" rel=\"noopener noreferrer\"><img decoding=\"async\" class='wp-image-5668 avia-img-lazy-loading-not-5668 avia_image ' src=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/03\/Verticale_beweging_van_de_veenbodem-192x300.jpg\" alt='' title='Verticale_beweging_van_de_veenbodem'  height=\"300\" width=\"192\"  itemprop=\"thumbnailUrl\" srcset=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/03\/Verticale_beweging_van_de_veenbodem-192x300.jpg 192w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/03\/Verticale_beweging_van_de_veenbodem-452x705.jpg 452w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/03\/Verticale_beweging_van_de_veenbodem.jpg 564w\" sizes=\"(max-width: 192px) 100vw, 192px\" \/><\/a><\/div><\/div><\/div><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-59p732-6052832db415813fc5f2d398f493eb61\">\n#top .av-special-heading.av-59p732-6052832db415813fc5f2d398f493eb61{\npadding-bottom:10px;\n}\nbody .av-special-heading.av-59p732-6052832db415813fc5f2d398f493eb61 .av-special-heading-tag .heading-char{\nfont-size:25px;\n}\n.av-special-heading.av-59p732-6052832db415813fc5f2d398f493eb61 .av-subheading{\nfont-size:15px;\n}\n<\/style>\n<div  class='av-special-heading av-59p732-6052832db415813fc5f2d398f493eb61 av-special-heading-h3 blockquote modern-quote  avia-builder-el-81  el_after_av_one_half  el_before_av_one_half '><h3 class='av-special-heading-tag'  itemprop=\"headline\"  >Monitoring Shallow Subsidence in Cultivated Peatlands<\/h3><div class=\"special-heading-border\"><div class=\"special-heading-inner-border\"><\/div><\/div><\/div>\n<div class='flex_column av-4w5l2m-9a91b160b5dc5de07557ec0268a8301b av_one_half  avia-builder-el-82  el_after_av_heading  el_before_av_one_half  first flex_column_div '     ><section  class='av_textblock_section av-m680qsgs-9d3aa8500d38abc6402e29a6591d4cef'  itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div class='avia_textblock'  itemprop=\"text\" ><button class=\"responsivevoice-button\" type=\"button\" title=\"ResponsiveVoice Tap to Start\/Stop Speech\" data-rvtts-action=\"speak\" data-rvtts-text=\"Accurate monitoring of shallow soil subsidence in peat meadow areas is a major challenge. To design and test a system for monitoring soil subsidence in peat meadows, four methods for measuring soil subsidence are applied and evaluated in a peat meadow area in Overijssel, namely: spirit leveling, measuring with an extensometer, LiDAR, and InSAR. This article focuses on the methods and measurements of spirit levels and extensometers. Authors: Sanneke van Asselen (Deltares), Gilles Erkens (Deltares, Universiteit Utrecht), Francis de Graaf (Waterschap Drents Overijsselse Delta) greater than Read the paper here.\" data-rvtts-voice=\"Dutch Female\" data-rvtts-brand-url=\"https:\/\/responsivevoice.org\/?utm_source=wordpress-plugin&amp;utm_medium=referral&amp;utm_campaign=powered-by\" data-rvtts-brand-label=\"Powered by ResponsiveVoice\"><svg class=\"rvtts-icon\" width=\"22\" height=\"22\" viewBox=\"0 0 22 22\" fill=\"currentColor\" aria-hidden=\"true\" focusable=\"false\"><path fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M11 0C4.92345 0 0 4.92345 0 11C0 13.2683 0.690345 15.3772 1.86621 17.1221L0.811724 21.0517L4.70345 20.0124C6.48621 21.2641 8.65586 22 11 22C17.0766 22 22 17.0766 22 11C22 4.92345 17.0766 0 11 0ZM3.99793 9.99862C3.99793 9.44483 4.44552 8.99724 4.99931 8.99724C5.5531 8.99724 6.00069 9.44483 6.00069 9.99862V12.0014C6.00069 12.5552 5.5531 13.0028 4.99931 13.0028C4.44552 13.0028 3.99793 12.5552 3.99793 12.0014V9.99862ZM8.99724 13.9966C8.99724 14.5503 8.54966 14.9979 7.99586 14.9979C7.44207 14.9979 6.99448 14.5503 6.99448 13.9966V7.99586C6.99448 7.44207 7.44207 6.99448 7.99586 6.99448C8.54966 6.99448 8.99724 7.44207 8.99724 7.99586V13.9966ZM12.0014 17.0007C12.0014 17.5545 11.5538 18.0021 11 18.0021C10.4462 18.0021 9.99862 17.5545 9.99862 17.0007V4.99931C9.99862 4.44552 10.4462 3.99793 11 3.99793C11.5538 3.99793 12.0014 4.44552 12.0014 4.99931V17.0007ZM14.9979 13.9966C14.9979 14.5503 14.5503 14.9979 13.9966 14.9979C13.4428 14.9979 12.9952 14.5503 12.9952 13.9966V7.99586C12.9952 7.44207 13.4428 6.99448 13.9966 6.99448C14.5503 6.99448 14.9979 7.44207 14.9979 7.99586V13.9966ZM18.0021 12.0014C18.0021 12.5552 17.5545 13.0028 17.0007 13.0028C16.4469 13.0028 15.9993 12.5552 15.9993 12.0014V9.99862C15.9993 9.44483 16.4469 8.99724 17.0007 8.99724C17.5545 8.99724 18.0021 9.44483 18.0021 9.99862V12.0014Z\"\/><\/svg><span class=\"responsivevoice-button__label\">Tekst oplezen<\/span><\/button> <\/p>\n<p>Accurate monitoring of shallow soil subsidence in peat meadow areas is a major challenge. To design and test a system for monitoring soil subsidence in peat meadows, four methods for measuring soil subsidence are applied and evaluated in a peat meadow area in Overijssel, namely: spirit leveling, measuring with an extensometer, LiDAR, and InSAR. This article focuses on the methods and measurements of spirit levels and extensometers.<\/p>\n<p><span style=\"font-style: inherit; font-weight: inherit;\"><strong>Authors<\/strong>: Sanneke van Asselen (Deltares), Gilles Erkens (Deltares, Universiteit Utrecht), Francis de Graaf (Waterschap Drents Overijsselse Delta)<\/span><\/p>\n<p><a href=\"https:\/\/piahs.copernicus.org\/articles\/382\/189\/2020\/\"><span style=\"font-style: inherit; font-weight: inherit;\">&gt; Read the paper here.<\/span><\/a><\/p>\n<p>\n<\/div><\/section><\/div><div class='flex_column av-4525by-ef05aef0a2cbcb5c6345699c6ad8ca3b av_one_half  avia-builder-el-84  el_after_av_one_half  el_before_av_heading  flex_column_div '     ><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-2dczbi-d9336a541e7a06cb357a18bd96c0d6ea\">\n.avia-image-container.av-2dczbi-d9336a541e7a06cb357a18bd96c0d6ea img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-2dczbi-d9336a541e7a06cb357a18bd96c0d6ea .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div  class='avia-image-container av-2dczbi-d9336a541e7a06cb357a18bd96c0d6ea av-styling- avia-align-center  avia-builder-el-85  avia-builder-el-no-sibling '   itemprop=\"image\" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/ImageObject\" ><div class=\"avia-image-container-inner\"><div class=\"avia-image-overlay-wrap\"><a href=\"https:\/\/piahs.copernicus.org\/articles\/382\/189\/2020\/\" class=\"avia_image\" target=\"_blank\" rel=\"noopener noreferrer\"><img decoding=\"async\" class='wp-image-5520 avia-img-lazy-loading-not-5520 avia_image ' src=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/01\/Monitoring-_shallow_subsidence-192x300.jpg\" alt='' title='Monitoring-_shallow_subsidence'  height=\"300\" width=\"192\"  itemprop=\"thumbnailUrl\" srcset=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/01\/Monitoring-_shallow_subsidence-192x300.jpg 192w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/01\/Monitoring-_shallow_subsidence-452x705.jpg 452w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/01\/Monitoring-_shallow_subsidence.jpg 564w\" sizes=\"(max-width: 192px) 100vw, 192px\" \/><\/a><\/div><\/div><\/div><\/div>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-ktlce-48fed492e447ef6c038bf3070321754a\">\n#top .av-special-heading.av-ktlce-48fed492e447ef6c038bf3070321754a{\npadding-bottom:10px;\n}\nbody .av-special-heading.av-ktlce-48fed492e447ef6c038bf3070321754a .av-special-heading-tag .heading-char{\nfont-size:25px;\n}\n.av-special-heading.av-ktlce-48fed492e447ef6c038bf3070321754a .av-subheading{\nfont-size:15px;\n}\n<\/style>\n<div  class='av-special-heading av-ktlce-48fed492e447ef6c038bf3070321754a av-special-heading-h3 blockquote modern-quote  avia-builder-el-86  el_after_av_one_half  el_before_av_one_half '><h3 class='av-special-heading-tag'  itemprop=\"headline\"  >The relation between land subsidence and CO2 emissions in peatlands<\/h3><div class=\"special-heading-border\"><div class=\"special-heading-inner-border\"><\/div><\/div><\/div>\n<div class='flex_column av-3t29hq-311a54a443590496e114beca70780130 av_one_half  avia-builder-el-87  el_after_av_heading  el_before_av_one_half  first flex_column_div '     ><section  class='av_textblock_section av-mbujak90-799e26afc988d27cc5ab3f9abbc8d043'  itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/CreativeWork\" ><div class='avia_textblock'  itemprop=\"text\" ><button class=\"responsivevoice-button\" type=\"button\" title=\"ResponsiveVoice Tap to Start\/Stop Speech\" data-rvtts-action=\"speak\" data-rvtts-text=\"When using land subsidence data to estimate CO\u2082 emissions from drained peatlands, two crucial factors must be considered: not all land subsidence is due to microbial decomposition of peat, and a conversion factor is needed to convert land subsidence (a change in volume) into CO\u2082 emissions (a change in mass). This article assesses how previous studies have addressed these two factors and supplements existing knowledge and experience with new data and insights gathered in recent years. Authors: Sanneke van Asselen (Deltares), Gilles Erkens (Deltares\/Universiteit Utrecht) greater than Read the article here.\" data-rvtts-voice=\"Dutch Female\" data-rvtts-brand-url=\"https:\/\/responsivevoice.org\/?utm_source=wordpress-plugin&amp;utm_medium=referral&amp;utm_campaign=powered-by\" data-rvtts-brand-label=\"Powered by ResponsiveVoice\"><svg class=\"rvtts-icon\" width=\"22\" height=\"22\" viewBox=\"0 0 22 22\" fill=\"currentColor\" aria-hidden=\"true\" focusable=\"false\"><path fill-rule=\"evenodd\" clip-rule=\"evenodd\" d=\"M11 0C4.92345 0 0 4.92345 0 11C0 13.2683 0.690345 15.3772 1.86621 17.1221L0.811724 21.0517L4.70345 20.0124C6.48621 21.2641 8.65586 22 11 22C17.0766 22 22 17.0766 22 11C22 4.92345 17.0766 0 11 0ZM3.99793 9.99862C3.99793 9.44483 4.44552 8.99724 4.99931 8.99724C5.5531 8.99724 6.00069 9.44483 6.00069 9.99862V12.0014C6.00069 12.5552 5.5531 13.0028 4.99931 13.0028C4.44552 13.0028 3.99793 12.5552 3.99793 12.0014V9.99862ZM8.99724 13.9966C8.99724 14.5503 8.54966 14.9979 7.99586 14.9979C7.44207 14.9979 6.99448 14.5503 6.99448 13.9966V7.99586C6.99448 7.44207 7.44207 6.99448 7.99586 6.99448C8.54966 6.99448 8.99724 7.44207 8.99724 7.99586V13.9966ZM12.0014 17.0007C12.0014 17.5545 11.5538 18.0021 11 18.0021C10.4462 18.0021 9.99862 17.5545 9.99862 17.0007V4.99931C9.99862 4.44552 10.4462 3.99793 11 3.99793C11.5538 3.99793 12.0014 4.44552 12.0014 4.99931V17.0007ZM14.9979 13.9966C14.9979 14.5503 14.5503 14.9979 13.9966 14.9979C13.4428 14.9979 12.9952 14.5503 12.9952 13.9966V7.99586C12.9952 7.44207 13.4428 6.99448 13.9966 6.99448C14.5503 6.99448 14.9979 7.44207 14.9979 7.99586V13.9966ZM18.0021 12.0014C18.0021 12.5552 17.5545 13.0028 17.0007 13.0028C16.4469 13.0028 15.9993 12.5552 15.9993 12.0014V9.99862C15.9993 9.44483 16.4469 8.99724 17.0007 8.99724C17.5545 8.99724 18.0021 9.44483 18.0021 9.99862V12.0014Z\"\/><\/svg><span class=\"responsivevoice-button__label\">Tekst oplezen<\/span><\/button> <\/p>\n<div class=\"wnVEW\">\n<div role=\"document\">\n<div class=\"Yy5or GNqVo allowTextSelection OuGoX\" tabindex=\"0\" aria-label=\"Berichttekst\">\n<div class=\"BIZfh\">\n<div>\n<div>\n<div lang=\"nl\">\n<div>\n<div><\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<div class=\"wnVEW\">\n<div role=\"document\">\n<div class=\"T31hC GNqVo allowTextSelection OuGoX\" tabindex=\"0\" aria-label=\"Berichttekst\" data-fui-focus-visible=\"\">\n<div class=\"BIZfh\">\n<div>\n<div>\n<div lang=\"nl\">\n<div>\n<div>\n<p>When using land subsidence data to estimate CO\u2082 emissions from drained peatlands, two crucial factors must be considered:<\/p>\n<ol>\n<li>not all land subsidence is due to microbial decomposition of peat, and<\/li>\n<li>a conversion factor is needed to convert land subsidence (a change in volume) into CO\u2082 emissions (a change in mass).<\/li>\n<\/ol>\n<p>This article assesses how previous studies have addressed these two factors and supplements existing knowledge and experience with new data and insights gathered in recent years.<\/p>\n<p><strong>Authors: <\/strong>Sanneke van Asselen (Deltares), Gilles Erkens (Deltares\/Universiteit Utrecht)<\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<p><a href=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/06\/TISOLS_ErkensVanAsselen-1.pdf\"><span style=\"font-style: inherit; font-weight: inherit;\">&gt; Read the article here.<\/span><\/a><\/p>\n<p>\n<\/div><\/section><\/div><div class='flex_column av-2x3xge-38a011359dc114e4aafe8069008d963e av_one_half  avia-builder-el-89  el_after_av_one_half  avia-builder-el-last  flex_column_div '     ><style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-mbuj99ed-a24f26465205ffe212373e3bc83b1a55\">\n.avia-image-container.av-mbuj99ed-a24f26465205ffe212373e3bc83b1a55 img.avia_image{\nbox-shadow:none;\n}\n.avia-image-container.av-mbuj99ed-a24f26465205ffe212373e3bc83b1a55 .av-image-caption-overlay-center{\ncolor:#ffffff;\n}\n<\/style>\n<div  class='avia-image-container av-mbuj99ed-a24f26465205ffe212373e3bc83b1a55 av-styling- avia-align-center  avia-builder-el-90  avia-builder-el-no-sibling '   itemprop=\"image\" itemscope=\"itemscope\" itemtype=\"https:\/\/schema.org\/ImageObject\" ><div class=\"avia-image-container-inner\"><div class=\"avia-image-overlay-wrap\"><a href=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/06\/TISOLS_ErkensVanAsselen-1.pdf\" class=\"avia_image\" target=\"_blank\" rel=\"noopener noreferrer\"><img decoding=\"async\" class='wp-image-5839 avia-img-lazy-loading-not-5839 avia_image ' src=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/06\/The_relation_between_land_subsidence-192x300.jpg\" alt='' title='_The_relation_between_land_subsidence'  height=\"300\" width=\"192\"  itemprop=\"thumbnailUrl\" srcset=\"https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/06\/The_relation_between_land_subsidence-192x300.jpg 192w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/06\/The_relation_between_land_subsidence-452x705.jpg 452w, https:\/\/www.nobveenweiden.nl\/wp-content\/uploads\/2025\/06\/The_relation_between_land_subsidence.jpg 564w\" sizes=\"(max-width: 192px) 100vw, 192px\" \/><\/a><\/div><\/div><\/div><\/div><\/div><\/div><\/div><!-- close content main div --><\/div><\/div><div id='after_section_2'  class='main_color av_default_container_wrap container_wrap fullsize'  ><div class='container av-section-cont-open' ><div class='template-page content  av-content-full alpha units'><div class='post-entry post-entry-type-page post-entry-5911'><div class='entry-content-wrapper clearfix'>\n<style type=\"text\/css\" data-created_by=\"avia_inline_auto\" id=\"style-css-av-3wafla-c01598717a242768c59bbd872433b28b\">\n#top .hr.hr-invisible.av-3wafla-c01598717a242768c59bbd872433b28b{\nheight:30px;\n}\n<\/style>\n<div  class='hr av-3wafla-c01598717a242768c59bbd872433b28b hr-invisible  avia-builder-el-91  el_after_av_section  avia-builder-el-no-sibling '><span class='hr-inner '><span class=\"hr-inner-style\"><\/span><\/span><\/div><\/p>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"tags":[87,90,91,88,92,89,86,85,93],"class_list":["post-5911","page","type-page","status-publish","hentry","tag-bodemaanpassing-en","tag-bodemopbouw-en","tag-doorlatendheid-en","tag-grondwaterpeil-en","tag-kwel-en","tag-methaan-en","tag-natte-teelt-en","tag-waterinfiltratiesystemen-en","tag-wegzijging-en"],"_links":{"self":[{"href":"https:\/\/www.nobveenweiden.nl\/en\/wp-json\/wp\/v2\/pages\/5911","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.nobveenweiden.nl\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.nobveenweiden.nl\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.nobveenweiden.nl\/en\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.nobveenweiden.nl\/en\/wp-json\/wp\/v2\/comments?post=5911"}],"version-history":[{"count":2,"href":"https:\/\/www.nobveenweiden.nl\/en\/wp-json\/wp\/v2\/pages\/5911\/revisions"}],"predecessor-version":[{"id":5937,"href":"https:\/\/www.nobveenweiden.nl\/en\/wp-json\/wp\/v2\/pages\/5911\/revisions\/5937"}],"wp:attachment":[{"href":"https:\/\/www.nobveenweiden.nl\/en\/wp-json\/wp\/v2\/media?parent=5911"}],"wp:term":[{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.nobveenweiden.nl\/en\/wp-json\/wp\/v2\/tags?post=5911"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}