Deng Lei, Li Ji-Wei, Qu Qing, Shi Jing-Wei, Shangguan Zhou-Ping
State Key Laboratory for Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University, Yangling 712100, Shaanxi, China.
College of Soil and Water Conservation Science and Engineering (Institute of Soil and Water Conservation), Northwest A&F University, Yangling 712100, Shaanxi, China.
Ying Yong Sheng Tai Xue Bao. 2024 Nov;35(11):3208-3216. doi: 10.13287/j.1001-9332.202411.009.
Grazing exclusion is the most effective measure to restore the structure and function of degraded grasslands, and plays a crucial role in increasing ecosystem carbon (C) sequestration capacity. The dynamics and dri-ving mechanisms of soil organic carbon (SOC) after grazing exclusion have attracted great concerns, especially in the context of global change. By reviewing the current research on the SOC sequestration dynamics and its driving mechanisms after grazing exclusion, we aimed to clarify the SOC sequestration dynamics, explore the influencing mechanisms of plant C input and microbial community on SOC, analyze the driving mechanisms of photosynthetic C input and litter decomposition on SOC sequestration, and explore the contribution of plant and microbial necromass C to SOC sequestration after grazing exclusion. Long-term grazing exclusion improve the structure and function of soil microorganisms by increasing plant carbon inputs, and increase the content and proportion of soil stable organic C (such as mineral-associated organic C, plant and microbial necromass C, etc.), reducing mineralization efficiency of SOC and improving microbial C utilization efficiency, and consequently promoting SOC accumulation. In addition, SOC sequestration shows two trends of "first increasing and then stabilizing" and "first decreasing, following increasing and then stabilizing", which are affected by the initial SOC level. Future studies should be strengthened in the SOC fraction dynamics, the C flow of SOC input, the decomposition process of SOC, and the microbial dri-ving mechanism after grazing exclusion.
禁牧是恢复退化草原结构和功能的最有效措施,对提高生态系统碳固存能力起着关键作用。禁牧后土壤有机碳(SOC)的动态变化及其驱动机制备受关注,尤其是在全球变化背景下。通过综述当前关于禁牧后SOC固存动态及其驱动机制的研究,我们旨在阐明SOC固存动态,探究植物碳输入和微生物群落对SOC的影响机制,分析光合碳输入和凋落物分解对SOC固存的驱动机制,并探讨禁牧后植物和微生物残体碳对SOC固存的贡献。长期禁牧通过增加植物碳输入改善土壤微生物的结构和功能,增加土壤稳定有机碳(如矿物结合有机碳、植物和微生物残体碳等)的含量和比例,降低SOC的矿化效率,提高微生物碳利用效率,从而促进SOC积累。此外,SOC固存呈现“先增加后稳定”和“先减少、后增加再稳定”两种趋势,这受初始SOC水平的影响。未来研究应加强禁牧后SOC组分动态、SOC输入的碳流、SOC分解过程以及微生物驱动机制方面的研究。