Literature DB >> 29758856

Relative contributions of wind and water erosion to total soil loss and its effect on soil properties in sloping croplands of the Chinese Loess Plateau.

Dengfeng Tuo1, Mingxiang Xu2, Guangyao Gao3.   

Abstract

Wind and water erosion are two dominant types of erosion that lead to soil and nutrient losses. Wind and water erosion may occur simultaneously to varying extents in semi-arid regions. The contributions of wind and water erosion to total erosion and their effects on soil quality, however, remains elusive. We used cesium-137 (137Cs) inventories to estimate the total soil erosion and used the Revised Universal Soil Loss Equation (RUSLE) to quantify water erosion in sloping croplands. Wind erosion was estimated from the subtraction of the two. We also used 137Cs inventories to calculate total soil erosion and validate the relationships of the soil quality and erosion at different slope aspects and positions. The results showed that wind erosion (1460tkm-2a-1) on northwest-facing slope was responsible for approximately 39.7% of the total soil loss, and water erosion (2216tkm-2a-1) accounted for approximately 60.3%. The erosion rates were 58.8% higher on northwest- than on southeast-facing slopes. Northwest-facing slopes had lower soil organic carbon, total nitrogen, clay, and silt contents than southeast-facing slopes, and thus, the 137Cs inventories were lower, and the total soil erosions were higher on the northwest-facing slopes. The variations in soil physicochemical properties were related to total soil erosion. The lowest 137Cs inventories and nutrient contents were recorded at the upper positions on the northwest-facing slopes due to the successive occurrence of more severe wind and water erosion at the same site. The results indicated that wind and water could accelerate the spatial variability of erosion rate and soil properties and cause serious decreases in the nutrient contents in sloping fields. Our research could help researchers develop soil strategies to reduce soil erosion according to the dominant erosion type when it occurs in a hilly agricultural area.
Copyright © 2018 Elsevier B.V. All rights reserved.

Entities:  

Keywords:  (137)Cs; Erosion rate; RUSLE model; Slope aspect; Soil organic carbon

Year:  2018        PMID: 29758856     DOI: 10.1016/j.scitotenv.2018.03.237

Source DB:  PubMed          Journal:  Sci Total Environ        ISSN: 0048-9697            Impact factor:   7.963


  4 in total

1.  Tracking the Deposition and Sources of Soil Carbon and Nitrogen in Highly Eroded Hilly-Gully Watershed in Northeastern China.

Authors:  Na Li; Yanqing Zhang; Zhanxiang Sun; John Yang; Enke Liu; Chunqian Li; Fengming Li
Journal:  Int J Environ Res Public Health       Date:  2021-03-14       Impact factor: 3.390

2.  Temporal and Spatial Variation and Driving Forces of Soil Erosion on the Loess Plateau before and after the Implementation of the Grain-for-Green Project: A Case Study in the Yanhe River Basin, China.

Authors:  Jiaying He; Xiaohui Jiang; Yuxin Lei; Wenjuan Cai; Junjun Zhang
Journal:  Int J Environ Res Public Health       Date:  2022-07-11       Impact factor: 4.614

3.  Effects of Vegetation Restoration on Soil Erosion on the Loess Plateau: A Case Study in the Ansai Watershed.

Authors:  Hui Wei; Wenwu Zhao; Han Wang
Journal:  Int J Environ Res Public Health       Date:  2021-06-10       Impact factor: 3.390

4.  Effectiveness of protection areas in safeguarding biodiversity and ecosystem services in Tibet Autonomous Region.

Authors:  Kaipeng Xu; Xiahui Wang; Jinnan Wang; Jingjing Wang; Rongfeng Ge; Rensheng Tian; Huixia Chai; Xin Zhang; Le Fu
Journal:  Sci Rep       Date:  2022-01-21       Impact factor: 4.379

  4 in total

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