文献类型： 外文期刊

作者： Guo, Geng ¹ ; Kong, Yu ¹ ; Xu, Yanyin ² ; Peng, Xiaoying ¹ ; Niu, Manting ² ; Zeng, Guangruo ³ ; Ouyang, Zhen ¹ ; Liu, Jun ⁴ ; Zhang, Chen ⁵ ; Lin, Jie ¹ ;

作者机构： 1.Nanjing Forestry Univ, Coinnovat Ctr Sustainable Forestry southern China, Key Lab Soil & Water Conservat & Ecol Restorat Jia, Nanjing 210037, Jiangsu, Peoples R China

2.Yunnan Inst Trop Crops, Jinghong 666100, Yunnan, Peoples R China

3.Acad Forestry Jian City, Jian 343000, Jiangxi, Peoples R China

4.Soil & Water Conservat Ctr Xingguo Cty, Ganzhou 341000, Jiangxi, Peoples R China

5.Jiangxi Inst Red Soil, Jinxian Cty 330045, Jiangxi, Peoples R China

关键词： Soil aggregate stability; Water erosion; Landscape positions; Soil organic matter fractions; Iron and aluminum oxides

期刊名称：JOURNAL OF HYDROLOGY （ 影响因子：5.9； 五年影响因子：6.4 ）

ISSN： 0022-1694

年卷期： 2024 年 639 卷

页码：

收录情况： SCI

摘要： Water erosion considerably affects the stability and particle size distribution of soil aggregates, but the underlying mechanisms of water erosion remain unclear. To this end, we selected four landscape positions (top-, up-, mid-, and toe-slope) with distinct erosion and deposition characteristics on a typical eroded slope in southern China to conduct experiments- aiming to investigate the main drivers of soil aggregate stability during erosion and deposition processes. Soil samples were collected from 12 sites, and 4 size classes (>2, 2-0.25, 0.25-0.053, and <0.053 mm) of soil aggregates were obtained using the wet sieving method. The composition and stability of the soil aggregates, as well as the contents of organic (organic matter components) and inorganic (iron-aluminum oxides) cementing materials of different particle sizes, were determined. The results indicated that erosion significantly reduced the aggregate stability and the >0.25 mm water-stable aggregate content (WR0.25) (P < 0.05). The mean weight diameter (MWD) and geometric mean diameter (GMD) values of the soil aggregates at the eroding site decreased, and the fractal dimension (FD) increased. Furthermore, erosion markedly reduced the humic acid (HA) and fulvic acid (FA) contents in the bulk soils and soil aggregates, while the HA content showed no obvious difference between the eroding and depositional sites. In addition to the presence of complexed iron/alumina oxides (Fe-p/Al-p), erosion markedly reduced the contents of amorphous (Fe-o/Al-o) and free-form (Fe-d/Al-d) iron/alumina oxides in the bulk soils and size fractions. Moreover, Fe-d/Al-d, Fe-p and Fe-o/Al-o were present in the microaggregates, while Al-p was found in the macroaggregates. Additionally, boosted regression tree (BRT) analysis indicated that FA (36.70 %), Fe-o (19.00 %), and Al-d (12.71 %) were the crucial predictors of soil aggregate stability. These findings further confirm that the organic and inorganic cementing materials in red soils collectively contribute to aggregate stabilization under the impact of erosion. This study facilitates a deeper understanding of the mechanisms governing soil aggregate stability in eroded landscapes, and provides a theoretical basis for biogeochemical cycling processes.