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Responses of Soil Labile Organic Carbon on Aggregate Stability across Different Collapsing-Gully Erosion Positions from Acric Ferralsols of South China

文献类型： 外文期刊

作者： Tang, Xian 1 ; Alhaj Hamoud, Yousef 3 ; Shaghaleh, Hiba 4 ; Zhao, Jianrong 2 ; Wang, Hong 2 ; Wang, Jiajia 5 ; Zhao, Tao 6 ; Li, Bo 1 ; Lu, Ying 1 ;

作者机构： 1.South China Agr Univ, Coll Nat Resources & Environm, Guangzhou 510642, Peoples R China

2.Anhui Sci & Technol Univ, Coll Nat Resources & Environm, Chuzhou 233100, Peoples R China

3.Hohai Univ, Coll Hydrol & Water Resources, Nanjing 210098, Peoples R China

4.Hohai Univ, Coll Environm, Nanjing 210098, Peoples R China

5.Anhui Acad Agr Sci, Inst Soil & Fertilizer, Anhui Prov Key Lab Nutrient Cycling Resources & En, Hefei 230031, Peoples R China

6.Aerosp Environm Engn Co Ltd, Tianjin 300301, Peoples R China

关键词： soil LOC; C pool management index; collapsing gully erosion; aggregate stability; Acric Ferralsols

期刊名称：AGRONOMY-BASEL （ 影响因子：3.7； 五年影响因子：4.0 ）

ISSN：

年卷期： 2023 年 13 卷 7 期

页码：

收录情况： SCI

摘要： Soil labile organic carbon (LOC) is a valuable and sensitive parameter of the changes in soil carbon (C) pools and further affects soil structural stability. However, the influences of soil-aggregate stability on LOC fractions under erosion conditions are still unclear, especially under the collapsing gully area of south China. Soils of five positions of collapsing gully erosion, including the upper catchment (UC), collapsing wall (CW), colluvial deposit (CD), scour channel (SC) and alluvial fan (AF) from Acric Ferralsols were investigated and sampled. Soil aggregate stability and LOC fractions were measured and analyzed. Soil water-stable aggregate and passive C (passive-C) contents significantly increased by 67-76% and 8.7-13.0% at the UC, CW, CD and SC positions, respectively, while soil labile C (labile-C) content was lower at these positions as compared to the AF position (p < 0.05). Moreover, the UC position's soil C pool management index (CPMI) significantly increased by 37-40% compared to CW, CD, SC and AF soils, indicating that the soil of the UC position had a more stable C pool due to its stronger structural stability. SOC, silt, and amorphous iron oxide (Fea) contents significantly contributed to aggregate stability. We demonstrated that the depletion of soil aggregate stability could result in the decreases in soil LOC fractions, while soil properties of the OC but not the LOC pool regulated aggregate stability and thus affected soil structure across different collapsing gully erosion positions in the subtropical Acric Ferralsols region of south China. This study contributes to developing strategies to prevent soil erosion and improve global C cycle and soil quality, which could be beneficial to strengthen soil and water conservation, and improve soil fertility (e.g., SOC) and vegetation recovery, such as tea and tobacco.

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