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Mineral protection controls soil organic carbon stability in permafrost wetlands

Mineral protection can slow the effect of warming on the mineralization of organic carbon (OC) in permafrost wetlands, which has an important impact on the dynamics of soil OC. However, the response mechanisms of wetland mineral soil to warming in permafrost areas are unclear. In this study, the soi...

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Published in:The Science of the total environment 2023-04, Vol.869, p.161864-161864, Article 161864
Main Authors: Wang, Yao, Guo, Yuedong, Wang, Xianwei, Song, Changchun, Song, Yanyu, Liu, Zhendi, Wang, Shujie, Gao, Siqi, Ma, Guobao
Format: Article
Language:English
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Summary:Mineral protection can slow the effect of warming on the mineralization of organic carbon (OC) in permafrost wetlands, which has an important impact on the dynamics of soil OC. However, the response mechanisms of wetland mineral soil to warming in permafrost areas are unclear. In this study, the soil of the southern edge of the Eurasian permafrost area was selected, and bulk and heavy fraction (HF) soil was subjected to indoor warming incubation experiments using physical fractionation. The results showed that the HF accounted for 51.25 % of the total OC mineralization in the bulk soil, and the δ13C value of the CO2 that was emitted in the HF soil was higher than that of the bulk soil. This indicates the potential availability of mineral soil and that the mineralized OC in the HF was the more stable component. Additionally, the mineralization of the mineral subsoil after warming by 10 °C was only about half of the increase in the organic topsoil, and the temperature sensitivity was significantly negatively correlated with the Fe/Al oxides to OC ratio. The results indicate that under conditions of permafrost degradation, the physical protection of mineral soil at high latitudes is essential for the stability of OC, which may slow the trend of permafrost wetlands becoming carbon sources. [Display omitted] •Soil minerals promote the conservation of soil organic carbon.•Warming stimulates the decomposition of recalcitrant components rich in the δ13C value.•Mineral protection can reduce the temperature sensitivity of soil organic carbon.•Mineral protection can inhibit the degree of organic carbon mineralization.
ISSN:0048-9697
1879-1026
DOI:10.1016/j.scitotenv.2023.161864