Effects of physical crust on soil detachment by overland flow in the Loess Plateau region of China

被引:7
|
作者
Liu, Jiaxin [1 ,2 ]
Chen, Liding [1 ]
Wang, Bing [2 ,3 ]
Peng, Xiaoyu [1 ]
机构
[1] Yunnan Univ, Sch Ecol & Environm Sci, Kunming 650091, Peoples R China
[2] Northwest A&F Univ, Inst Soil & Water Conservat, State Key Lab Soil Eros & Dryland Farming Loess Pl, Yangling 712100, Shaanxi, Peoples R China
[3] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
基金
中国国家自然科学基金;
关键词
Physical soil crust formation; Soil heterogeneity; Rill erodibility; Critical shear stress; SIMULATED RAINFALL; EROSION RESISTANCE; CONCENTRATED FLOW; SPLASH EROSION; RILL; CAPACITY; MECHANISM; MOISTURE; RUNOFF;
D O I
10.1016/j.iswcr.2023.05.006
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Physical soil crust (PSC), a key component of surface soil structure, exists extensively in loess areas. PSC is considered to have a significant effect on soil detachment processes. However, the long-term effects and the corresponding mechanisms of PSC on soil detachment by overland flow are still not well understood, especially in natural environments. To investigate temporal variation in soil erosion resistance and the underlying factors during PSC formation, an 8 x 8-m soil plot was exposed to natural conditions in the Loess Plateau over a 524-day period spanning two rainy seasons and a winter between them. A flume test was conducted to determine soil detachment capacity (Dc) under six designed flow shear stress levels (5.66-22.11 Pa) using crusted (SC) and non-crusted (NSC) soil samples at different PSC development stages. Subsequently, two soil erosion resistance parameters, rill erodibility (Kr) and critical shear stress (Tc), were calculated. Over time, in the SC and NSC treatments, Kr decreased from 0.516 to 0.120 s m-1 and 0.521 to 0.223 s m-1, respectively, while Tc increased from 0.49 to 4.42 Pa and 0.26-2.46 Pa, respectively. Variation in soil erosion resistance was rapid in the first one to two months, and then slowed down, with slight fluctuations afterwards. In the SC treatment, Kr was 42% lower and Tc was 67% greater than those in the NSC treatment. Soil properties changed greatly for both treatments. SCT increased from 0 to 7.09 mm in the SC treatment. Coh increased from 2.91 to 9.04 kPa and 3.01-4.78 kPa in SC and NSC treatments, respectively. Both soil erosion resistance parameters could be well predicted by SCT and Coh in the SC treatment (R2 >= 0.82), while their best predictor was Coh in the NSC treatment (R2 >= 0.90). The results demonstrate that PSC formation enhances soil erosion resistance in the soil detachment process in the loess region under natural conditions. Our study revealed the important role and complexity of PSC in the process of soil erosion, and provided theoretical and data support for accurate understanding and prediction of soil erosion.(c) 2023 International Research and Training Center on Erosion and Sedimentation, China Water and Power Press, and China Institute of Water Resources and Hydropower Research. Publishing services by Elsevier B.V. on behalf of KeAi Communications Co. Ltd. This is an open access article under the CC BY -NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).
引用
收藏
页码:107 / 120
页数:14
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