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DOI10.1016/j.jenvman.2023.119945
High organic carbon content constricts the potential for stable organic carbon accrual in mineral agricultural soils in Finland
Soinne, Helena; Hyyrynen, Matti; Jokube, Medile; Keskinen, Riikka; Hyvaluoma, Jari; Pihlainen, Sampo; Hyytiainen, Kari; Miettinen, Arttu; Rasa, Kimmo; Lemola, Riitta; Virtanen, Eetu; Heinonsalo, Jussi; Heikkinen, Jaakko
发表日期2024
ISSN0301-4797
EISSN1095-8630
起始页码352
卷号352
英文摘要Sequestering carbon into agricultural soils is considered as a means of mitigating climate change. We used agronomic soil test results representing c. 95% of the farmed land area in Finland to estimate the potential of the uppermost 15 cm soil layer of mineral agricultural soils to sequester organic carbon (OC) and to contribute to the mitigation of climate change. The estimation of the maximum capacity of mineral matter to protect OC in stable mineral -associated form was based on the theory that clay and fine -sized (fines = clay + silt) particles have a limited capacity to protect OC. In addition, we used the clay/OC and fines/OC ratios to identify areas with a risk of erosion and reduced productivity, thus indicating priority areas potentially benefitting from the increased soil OC contents. We found that 32-40% of the mineral agricultural soils in Finland have the potential to further accumulate mineral -associated OC (MOC), while in the majority of soils, the current OC stock in the uppermost 15 cm exceeded the capacity of mineral matter to protect OC. The nationwide soil OC sequestration potential of the uppermost 15 cm in mineral agricultural soils ranged between 0.21 and 0.26 Tg, which corresponds to less than 2% of annual greenhouse gas emissions in Finland. The fields with the highest potential for SOC accrual were found in the southern and southwestern parts of the country, including some of the most intensively cultivated high -clay soils. Although the nationwide potential for additional OC sequestration was estimated to be relatively small, the current OC storage in Finnish arable mineral soils (0-15 cm) is large, 128 Tg. Farming practices enabling maximum OC input into the soil play an important role as a tool for mitigating the loss of carbon from high-OC soils in the changing climate. Furthermore, especially in high -clay areas with potential for MOC accrual, efforts to increase soil OC could help improve soil structural stability and therefore reduce erosion and the loss of nutrients to the aquatic environments.
英文关键词Mineral -associated organic carbon; Particulate organic carbon; Carbon sequestration; Carbon sink; Clay/OC ratio
语种英语
WOS研究方向Environmental Sciences & Ecology
WOS类目Environmental Sciences
WOS记录号WOS:001164027000001
来源期刊JOURNAL OF ENVIRONMENTAL MANAGEMENT
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/291634
作者单位Natural Resources Institute Finland (Luke); University of Helsinki; Natural Resources Institute Finland (Luke); Hame University of Applied Sciences; Finnish Environment Institute; University of Helsinki
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GB/T 7714
Soinne, Helena,Hyyrynen, Matti,Jokube, Medile,et al. High organic carbon content constricts the potential for stable organic carbon accrual in mineral agricultural soils in Finland[J],2024,352.
APA Soinne, Helena.,Hyyrynen, Matti.,Jokube, Medile.,Keskinen, Riikka.,Hyvaluoma, Jari.,...&Heikkinen, Jaakko.(2024).High organic carbon content constricts the potential for stable organic carbon accrual in mineral agricultural soils in Finland.JOURNAL OF ENVIRONMENTAL MANAGEMENT,352.
MLA Soinne, Helena,et al."High organic carbon content constricts the potential for stable organic carbon accrual in mineral agricultural soils in Finland".JOURNAL OF ENVIRONMENTAL MANAGEMENT 352(2024).
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