AUTHOR=Chen Jie , Biswas Asim , Su Haohai , Cao Jianjun , Hong Shuyan , Wang Hairu , Dong Xiaogang 

TITLE=Quantifying changes in soil organic carbon density from 1982 to 2020 in Chinese grasslands using a random forest model

JOURNAL=Frontiers in Plant Science

VOLUME=Volume 14 - 2023

YEAR=2023

URL=https://www.frontiersin.org/journals/plant-science/articles/10.3389/fpls.2023.1076902

DOI=10.3389/fpls.2023.1076902

ISSN=1664-462X

ABSTRACT=China has the second-largest grassland area in the world. Soil organic carbon storage (SOCS) in grasslands plays a critical role in maintaining carbon balance and mitigating climate change, both nationally and globally. Soil organic carbon density (SOCD) is an important indicator of SOCS. Exploring the spatiotemporal dynamics of SOCD helps policymakers to develop strategies to reduce carbon emissions meeting the goals of “emission peak” in 2030 and “carbon neutrality” in 2060 proposed by the Chinese government. The objective of this study was to quantify the dynamics of SOCD (0–100 cm) in Chinese grasslands from 1982 to 2020 and identify the dominant factors driving SOCD change using a random forest model. The results showed that the mean SOCD in Chinese grasslands was 7.791 kg C m-2 in 1982 and 8.525 kg C m-2 in 2020, with a net increase of 0.734 kg C m-2 with regional variability. The areas with increased SOCD were mainly distributed in the southern (0.411 kg C m-2), northwestern (1.439 kg C m-2) and Qinghai-Tibetan (0.916 kg C m-2) regions, while those with the decreased SOCD were mainly found in the northern (0.172 kg C m-2) region. Temperature, normalized difference vegetation index, elevation and wind speed were the dominant factors driving grassland SOCD change, explaining 73.23% of SOCD’s total variation. During the study period, grassland SOCS increased in the northwestern region, and decreased in the other three regions across China. Overall, SOCS of Chinese grasslands in 2020 was 22.623 Pg, a net decrease of 1.158 Pg since 1982 of 23.780 Pg. Over the past few decades, the reduction in grassland SOCS caused by grassland degradation may have contributed to CO2 emissions and created a negative climate impact. The results clearly highlight the urgency of strengthening soil carbon management in these grasslands and improve SOCS towards a positive climate impact.