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Changes in Soil Organic Carbon Stocks and Chemical Properties in Organogenic Soils Under Long‐Term Agricultural Use in Central Europe, Poland

Bibliographic Data

ID21647958
AuthorsEwelina Zając (0000-0002-5076-8347, Faculty of Environmental Engineering and Geodesy, Department of Land Reclamation and Environmental Development University of Agriculture in Krakow Krakow Poland, corresponding author), Bożena Smreczak (0000-0001-8972-8636, Institute of Soil Science and Plant Cultivation – State Research Institute Pulawy Poland, corresponding author), Tomasz Skalski (0000-0001-6059-8663, Biotechnology Center Silesian University of Technology Gliwice Poland), Ryszard Oleszczuk (0000-0002-0334-2132, Institute of Environmental Engineering Warsaw University of Life Sciences – SGGW Warsaw Poland), Aleksandra Ukalska‐Jaruga (Institute of Soil Science and Plant Cultivation – State Research Institute Pulawy Poland), Aleksandra Ukalska-Jaruga (0000-0002-9253-2383, Institute of Soil Science and Plant Cultivation), Bryant C Scharenbroch (College of Natural Resources University of Wisconsin – Stevens Point Stevens Point Wisconsin USA)
Year2025
Volume36
Issue11
Pages3756-3768
Publication date2025-07-15
Open AccessYes
TypeARTICLE
VenueLand Degradation and Development (JOURNAL)
Journal identifiersISSN: 1085-3278 • E-ISSN: 1099-145X
PublisherWiley (PUBLISHER • GB)
DOI10.1002/ldr.5597
OpenAlexW4409180853
LanguageEN
References cited63

Organic soils, particularly peatlands, are important carbon sinks. In Europe, almost half of the area has been drained mainly for agriculture, which causes problems with high carbon dioxide emissions. In Poland, peatlands are drained in 86% of the area, and most of them are used as grasslands. The aim of the study was to analyze changes in agriculturally used organogenic soils between 1975 and 2017 using data from 476 reference soil profiles. The results showed a significant decrease in organic soils (≥ 12% SOC), with an increase in percentage organo‐mineral and mineral soils ( −1 (from 500.4 Mg C·ha −1 to 228.0 Mg C·ha −1 ), with the median being four times lower, and it was observed in 64% of sites. The most significant decrease in SOC stock, by 64.7% compared to 1975, occurred in organic soils (from 762.2 Mg C·ha −1 to 269.3 Mg C·ha −1 ). Our analyses show that with increasing degradation of organic soils, factors that influence carbon content in soil change. In general, after 50 years, for organic soils, drainage was important, while for organo‐mineral and mineral soils, chemical properties, especially nutrient availability, were crucial. Carbon loss was most evident in the driest region of the country. The results indicate that continuous grassland use on organic soils does not offset SOC losses caused by drainage. At the same time, in organo‐mineral and mineral soils, a restraint of SOC stock loss was observed. This suggests that over 50 years of agricultural use of organogenic soils (mainly peat) along with their transformation, a balance between carbon output and input has been established. Considering this, it is an urgent task to update the area covered by organic soils used for agriculture, as it is important for reliable emission reporting and setting goals of organic soil protection and restoration

Agriculture · Agroforestry · Archaeology · Carbon fibers · Geography · Soil carbon · Soil water · Total organic carbon · Chemistry · Environmental Science · Integrated Water Resources Management · Mathematics · Peatlands and Wetlands Ecology · Soil Carbon and Nitrogen Dynamics · Environmental Chemistry · Forestry · Soil Science

  • Temperature sensitivity of soil carbon decomposition and feedbacks to climate change

    Open Access•Eric A Davidson, Ivan A Janssens•Nature•2006

  • The underappreciated potential of peatlands in global climate change mitigation strategies

    Open Access•Jens Leifeld, Lorenzo Menichetti•Nature Communications•2018

  • Soil carbon stocks and land use change

    Open Access•L B Guo, Roger M Gifford•Global Change Biology•2002

  • Global peatland dynamics since the Last Glacial Maximum

    Open Access•Zicheng Yu, Julie Loisel et al.•Geophysical Research Letters•2010

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