中国西北黄土高原植被恢复过程中土壤有机碳稳定机制研究进展。

Q3 Environmental Science
Shao-Shan An, Yang Hu, Bao-Rong Wang
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引用次数: 0

摘要

黄土高原以其深厚的土层和丰富的有机碳(C)而闻名于世。近年来,黄土高原开展了大量生态恢复项目,对土壤有机碳(SOC)的稳定性产生了影响。然而,有关黄土高原植被恢复过程中土壤有机碳稳定性的特征及其机制的全面综述尚不多见。因此,我们总结了黄土高原植被恢复过程中 SOC 稳定的动态变化,讨论了 SOC 稳定的机制,包括矿物保护、物理保护和生物机制。此外,我们还展望了黄土高原植被恢复过程中SOC稳定性研究的未来发展方向和研究重点,为植被恢复过程中土壤固碳稳定的理论和技术提供科学支持,为实现 "双碳 "目标提供科学参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Research advance on soil organic carbon stabilization mechanisms during vegetation restoration on the Loess Plateau, Northwest China.

The Loess Plateau is renowned for its deep soil layer and rich in organic carbon (C). In recent years, numerous ecological restoration projects have been undertaken on the Loess Plateau, with consequence on the stability of soil organic carbon (SOC). The SOC stability is pivotal for its capacity to sequestrate and store C. However, comprehensive review on the characteristics of SOC stability and its mechanisms during vegetation restoration on the Loess Plateau is scarce. Therefore, we summarized the dynamics of SOC stability during vegetation restoration on the Loess Plateau, discussed the mechanisms of SOC stabilization, including mineral protection, physical protection, and biological mechanisms. Furthermore, we prospected the future development directions and research focus of SOC stability research during vegetation restoration on the Loess Plateau to provide scientific support for theory and technology of soil C sequestration and stabilization during vegetation restoration, and to provide scientific reference for achieving the "double-carbon" goals.

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应用生态学报
应用生态学报 Environmental Science-Ecology
CiteScore
2.50
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0.00%
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11393
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