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高有机碳含量限制了芬兰矿物农业土壤中稳定有机碳积累的潜力。

High organic carbon content constricts the potential for stable organic carbon accrual in mineral agricultural soils in Finland.

机构信息

Natural Resources Institute Finland Luke, Latokartanonkaari 9, FI-00790, Helsinki, Finland.

Natural Resources Institute Finland Luke, Latokartanonkaari 9, FI-00790, Helsinki, Finland.

出版信息

J Environ Manage. 2024 Feb 14;352:119945. doi: 10.1016/j.jenvman.2023.119945. Epub 2024 Jan 12.

Abstract

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.

摘要

将碳封存到农业土壤中被认为是缓解气候变化的一种手段。我们利用代表芬兰约 95%农田面积的农艺土壤测试结果,估算了矿物农业土壤最上层 15cm 土壤层中有机碳(OC)的固碳潜力,以及对缓解气候变化的贡献。对稳定矿物结合形式下矿物质最大 OC 保护能力的估算,基于以下理论:即粘土和细颗粒(细颗粒=粘土+粉土)对 OC 的保护能力有限。此外,我们还利用粘土/OC 和细颗粒/OC 的比值,确定了具有侵蚀和生产力降低风险的区域,从而表明了那些可能受益于增加土壤 OC 含量的优先区域。我们发现,芬兰 32-40%的矿物农业土壤具有进一步积累矿物结合 OC(MOC)的潜力,而在大多数土壤中,最上层 15cm 的 OC 储量超过了矿物质保护 OC 的能力。芬兰矿物农业土壤最上层 15cm 的土壤 OC 固碳潜力全国范围在 0.21 到 0.26Tg 之间,这相当于芬兰温室气体年排放量的不到 2%。SOC 积累潜力最大的领域位于该国南部和西南部,包括一些最具集约化耕作的高粘土土壤。尽管全国范围内额外 OC 固存的潜力估计相对较小,但芬兰耕地矿物土壤(0-15cm)中目前的 OC 储量很大,为 128Tg。使 OC 最大程度输入土壤的耕作实践,作为减缓气候变化中高 OC 土壤碳损失的工具,发挥着重要作用。此外,特别是在具有 MOC 积累潜力的高粘土地区,增加土壤 OC 的努力可以帮助提高土壤结构稳定性,从而减少侵蚀和养分向水生环境的流失。

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