侵蚀-沉积过程通过团聚体的分解和堆积驱动土壤有机碳矿化

IF 5.7 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Lulu Bai , Jinxiao Duan , Peng Shi , Jun Xiao , Zhanbin Li , Peng Li
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引用次数: 0

摘要

水蚀对陆地生态系统横向土壤有机碳(SOC)再分配和CO2排放具有重要影响。虽然有机碳再分配模式已被广泛研究,但侵蚀沉积通过团聚体周转(分解和积累)调节有机碳矿化的机制仍不清楚。本研究采用稀土氧化物示踪、30分钟水槽模拟侵蚀沉积实验和56天土壤培养监测团聚体流动,以研究土壤团聚体流动介导的有机碳矿化。侵蚀区(SE)土壤的累积团粒破碎率(CBD)和累积团粒积聚率(CBU)分别为10.49%和13.26%,显著高于沉积区(SD)(分别为9.55%和9.83%),表明SE土壤的团粒动力学更为强烈。侵蚀和沉积均增强了有机碳矿化,其强弱顺序依次为SE (41.39 mg kg - 1) > SD (30.37 mg kg - 1) >;对照(CK) (24.21 mg kg - 1)。动力学模型y = K(1-e-bx) (R2 > 0.90)有效地描述了有机碳矿化动力学,参数K和K·b表明东南盆地有机碳矿化潜力大于SD和CK。结构方程模型确定了团聚体破碎是矿化的主要驱动因素,其路径系数在SE(0.703)高于SD(0.110)。而骨料堆积则通过物理保护抑制矿化,其作用在SD(通径系数为0.334)大于SE(通径系数为0.215)。这些结果证实了团聚体分解是侵蚀-沉积过程中有机碳动态的关键调节因子,为碳管理提供了重要的见解。我们建议实施流域尺度的工程结构(例如,拦河坝、沟槽稳定系统和沉积物保留盆地)来创建沉积带,这可以减少有机碳的损失和减少二氧化碳的排放,从而增强有机碳的固存。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Erosion-deposition processes drive soil organic carbon mineralization through aggregate breakdown and buildup
Water erosion critically influences lateral soil organic carbon (SOC) redistribution and CO2 emissions in terrestrial ecosystems. While SOC redistribution patterns have been extensively studied, the mechanisms by which erosion–deposition regulates SOC mineralization via aggregate turnover (breakdown and buildup) remain unclear. This study integrated rare earth oxides tracing, 30-minute flume experiments for simulate erosion–deposition, and 56-day soil incubation for monitor aggregate turnover over time to investigate soil aggregate turnover-mediated SOC mineralization. Cumulative aggregate breakdown (CBD) and buildup (CBU) rates were significantly higher in soils from the erosional area (SE) (CBD: 10.49 %; CBU: 13.26 %) than in those from the depositional area (SD) (9.55 % and 9.83 %, respectively), indicating more intense aggregate dynamics in SE. Both erosion and deposition enhanced SOC mineralization, showing a descending order: SE (41.39 mg kg−1) > SD (30.37 mg kg−1) > control (CK) (24.21 mg kg−1). The kinetic model y = K(1-e-bx) (R2 > 0.90) effectively described SOC mineralization dynamics, with parameters K and K·b indicating greater SOC mineralization potential in SE than in SD and CK. Structural equation modeling identified aggregate breakdown as the primary driver of mineralization, with a much higher path coefficient in SE (0.703) than in SD (0.110). In contrast, aggregate buildup suppressed mineralization via physical protection, with a stronger effect in SD (path coefficient: 0.334) than in SE (0.215). These results confirm that aggregate breakdown is a key regulator of SOC dynamics during erosion–deposition, providing critical insights for carbon management. We propose implementing watershed-scale engineering structures (e.g., check dams, gully stabilization systems, and sediment retention basins) to create depositional zones, which can reduce SOC loss and mitigate CO2 emissions, thereby enhancing SOC sequestration.
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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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