Variation in soil properties and its influence on the dynamic change of soil erosion resistance to overland flow in the water-level fluctuation zone of the Three Gorges Reservoir, China

•Dynamic change of soil erosion resistance were quantified.•Soil erosion resistance showed more spatial variation than temporal variation.•Mean weight diameter was the optimal index to describe the soil erodibility.•The critical shear stress was only affected by clay content.•Data strongly support a...

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Published inCatena (Giessen) Vol. 213; p. 106141
Main Authors Xiao, Hai, Guo, Ping, Zhang, Qianheng, Hu, Huan, Hong, Huan, Zhang, Lun, Yang, Yueshu, Xia, Zhenyao, Li, Mingyi, Kang, Hongliang, Zhang, Guanhua
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.06.2022
Subjects
catenas
clay
clay fraction
erodibility
overland flow
phytomass
Rill erodibility
sand fraction
shear stress
silt
Soil detachment capacity
soil erosion
soil organic matter
Spatial and temporal variations
Three Gorges Reservoir
Water-level fluctuation zone
Spatial and temporal variations
Soil detachment capacity
Three Gorges Reservoir
Rill erodibility
Water-level fluctuation zone
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Abstract •Dynamic change of soil erosion resistance were quantified.•Soil erosion resistance showed more spatial variation than temporal variation.•Mean weight diameter was the optimal index to describe the soil erodibility.•The critical shear stress was only affected by clay content.•Data strongly support an important effect of plant life-period on soil resistance. The water level fluctuations, rainstorms, and plants could lead to the variation in soil properties in the water-level fluctuation zone (WLFZ) and thus may influence the soil erosion resistance (soil erodibility, Kr, and critical shear stress, τc). However, variation in soil properties and its influence on the dynamic change of soil erosion resistance to overland flow in the WLFZ of the Three Gorges Reservoir (TGR) still unclear and need to be further quantified. Therefore, soil samples from different elevations were collected along a slope profile at different times in the WLFZ of the TGR, then the soil properties and plant biomass were measured and the soil detachment capacity (Dc) were estimated by conducting a scouring experiment. Then the Kr and τc were obtained according to the linear relationship between Dc and shear stress. The results indicated that most measured soil properties suffered low variability but organic matter content showed the moderate variability. Kr varied from 0.10 to 0.17 s m−1 and τc varied in the range of 1.56–2.24 Pa for all sampling points, and both showed spatial and temporal variations. Kr decreased with increasing elevation until reaching a minimum value and then increased spatially, while it showed a decreasing trend or a decreasing trend followed by an increasing trend over time for different elevation segments temporally. τc increased with increasing elevation spatially and increased or showed an increase followed by a decrease over time for different elevation segments temporally. Kr was significantly influenced by clay, silt, and sand content, mean weight diameter and soil organic matter content, while τc was only affected by clay content. These research results highlight the dynamic change of soil erosion resistance and are helpful for understanding the spatial and temporal variations in soil erosion resistance in the WLFZ of the TGR area.
AbstractList The water level fluctuations, rainstorms, and plants could lead to the variation in soil properties in the water-level fluctuation zone (WLFZ) and thus may influence the soil erosion resistance (soil erodibility, Kᵣ, and critical shear stress, τc). However, variation in soil properties and its influence on the dynamic change of soil erosion resistance to overland flow in the WLFZ of the Three Gorges Reservoir (TGR) still unclear and need to be further quantified. Therefore, soil samples from different elevations were collected along a slope profile at different times in the WLFZ of the TGR, then the soil properties and plant biomass were measured and the soil detachment capacity (Dc) were estimated by conducting a scouring experiment. Then the Kᵣ and τc were obtained according to the linear relationship between Dc and shear stress. The results indicated that most measured soil properties suffered low variability but organic matter content showed the moderate variability. Kᵣ varied from 0.10 to 0.17 s m⁻¹ and τc varied in the range of 1.56–2.24 Pa for all sampling points, and both showed spatial and temporal variations. Kᵣ decreased with increasing elevation until reaching a minimum value and then increased spatially, while it showed a decreasing trend or a decreasing trend followed by an increasing trend over time for different elevation segments temporally. τc increased with increasing elevation spatially and increased or showed an increase followed by a decrease over time for different elevation segments temporally. Kᵣ was significantly influenced by clay, silt, and sand content, mean weight diameter and soil organic matter content, while τc was only affected by clay content. These research results highlight the dynamic change of soil erosion resistance and are helpful for understanding the spatial and temporal variations in soil erosion resistance in the WLFZ of the TGR area.
•Dynamic change of soil erosion resistance were quantified.•Soil erosion resistance showed more spatial variation than temporal variation.•Mean weight diameter was the optimal index to describe the soil erodibility.•The critical shear stress was only affected by clay content.•Data strongly support an important effect of plant life-period on soil resistance. The water level fluctuations, rainstorms, and plants could lead to the variation in soil properties in the water-level fluctuation zone (WLFZ) and thus may influence the soil erosion resistance (soil erodibility, Kr, and critical shear stress, τc). However, variation in soil properties and its influence on the dynamic change of soil erosion resistance to overland flow in the WLFZ of the Three Gorges Reservoir (TGR) still unclear and need to be further quantified. Therefore, soil samples from different elevations were collected along a slope profile at different times in the WLFZ of the TGR, then the soil properties and plant biomass were measured and the soil detachment capacity (Dc) were estimated by conducting a scouring experiment. Then the Kr and τc were obtained according to the linear relationship between Dc and shear stress. The results indicated that most measured soil properties suffered low variability but organic matter content showed the moderate variability. Kr varied from 0.10 to 0.17 s m−1 and τc varied in the range of 1.56–2.24 Pa for all sampling points, and both showed spatial and temporal variations. Kr decreased with increasing elevation until reaching a minimum value and then increased spatially, while it showed a decreasing trend or a decreasing trend followed by an increasing trend over time for different elevation segments temporally. τc increased with increasing elevation spatially and increased or showed an increase followed by a decrease over time for different elevation segments temporally. Kr was significantly influenced by clay, silt, and sand content, mean weight diameter and soil organic matter content, while τc was only affected by clay content. These research results highlight the dynamic change of soil erosion resistance and are helpful for understanding the spatial and temporal variations in soil erosion resistance in the WLFZ of the TGR area.
ArticleNumber 106141
Author Zhang, Qianheng
Yang, Yueshu
Kang, Hongliang
Zhang, Guanhua
Guo, Ping
Hu, Huan
Zhang, Lun
Xia, Zhenyao
Li, Mingyi
Xiao, Hai
Hong, Huan
Author_xml – sequence: 1
  givenname: Hai
  surname: Xiao
  fullname: Xiao, Hai
  organization: Key Laboratory of Geological Hazards on Three Gorges Reservoir Area, Ministry of Education, Yichang 443002, PR China
– sequence: 2
  givenname: Ping
  surname: Guo
  fullname: Guo, Ping
  organization: Key Laboratory of Geological Hazards on Three Gorges Reservoir Area, Ministry of Education, Yichang 443002, PR China
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  surname: Zhang
  fullname: Zhang, Qianheng
  organization: Key Laboratory of Geological Hazards on Three Gorges Reservoir Area, Ministry of Education, Yichang 443002, PR China
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  givenname: Huan
  surname: Hu
  fullname: Hu, Huan
  organization: Key Laboratory of Geological Hazards on Three Gorges Reservoir Area, Ministry of Education, Yichang 443002, PR China
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  givenname: Huan
  surname: Hong
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  organization: Key Laboratory of Geological Hazards on Three Gorges Reservoir Area, Ministry of Education, Yichang 443002, PR China
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  givenname: Lun
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  organization: Key Laboratory of Geological Hazards on Three Gorges Reservoir Area, Ministry of Education, Yichang 443002, PR China
– sequence: 7
  givenname: Yueshu
  surname: Yang
  fullname: Yang, Yueshu
  organization: Key Laboratory of Geological Hazards on Three Gorges Reservoir Area, Ministry of Education, Yichang 443002, PR China
– sequence: 8
  givenname: Zhenyao
  surname: Xia
  fullname: Xia, Zhenyao
  email: xzy_yc@126.com
  organization: Key Laboratory of Geological Hazards on Three Gorges Reservoir Area, Ministry of Education, Yichang 443002, PR China
– sequence: 9
  givenname: Mingyi
  surname: Li
  fullname: Li, Mingyi
  email: limingyictgu@163.com
  organization: Key Laboratory of Geological Hazards on Three Gorges Reservoir Area, Ministry of Education, Yichang 443002, PR China
– sequence: 10
  givenname: Hongliang
  surname: Kang
  fullname: Kang, Hongliang
  organization: State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, PR China
– sequence: 11
  givenname: Guanhua
  surname: Zhang
  fullname: Zhang, Guanhua
  organization: Soil and Water Conservation Department, Changjiang River Scientific Research Institute, Wuhan 430010, PR China
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Keywords Spatial and temporal variations
Soil detachment capacity
Three Gorges Reservoir
Rill erodibility
Water-level fluctuation zone
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Snippet •Dynamic change of soil erosion resistance were quantified.•Soil erosion resistance showed more spatial variation than temporal variation.•Mean weight diameter...
The water level fluctuations, rainstorms, and plants could lead to the variation in soil properties in the water-level fluctuation zone (WLFZ) and thus may...
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SubjectTerms catenas
clay
clay fraction
erodibility
overland flow
phytomass
Rill erodibility
sand fraction
shear stress
silt
Soil detachment capacity
soil erosion
soil organic matter
Spatial and temporal variations
Three Gorges Reservoir
Water-level fluctuation zone
Title Variation in soil properties and its influence on the dynamic change of soil erosion resistance to overland flow in the water-level fluctuation zone of the Three Gorges Reservoir, China
URI https://dx.doi.org/10.1016/j.catena.2022.106141
https://www.proquest.com/docview/2675561449
Volume 213
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