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Chinese Agricultural Science Bulletin ›› 2020, Vol. 36 ›› Issue (18): 87-92.doi: 10.11924/j.issn.1000-6850.casb19030062

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Loess Slope Crust: Effects on the Stability and Erodibility of Soil Water-stable Aggregates

Chen Lin1, Wang Jian2(), Song Pengshuai1, Zhao Yu2, Ma Yuhong3   

  1. 1Institute of Soil and Water Conservation, Northwest A&F University, Yangling Shaanxi 712100
    2College of Natural Resources and Environment, Northwest A&F University, Yangling Shaanxi 712100
    3Xi’an Water Conservancy and Soil Conservation General Station, Xi’an 710000
  • Received:2019-03-15 Revised:2019-09-17 Online:2020-06-25 Published:2020-07-10
  • Contact: Wang Jian E-mail:wangjian@nwsuaf.edu.cn;184388610@qq.com

Abstract:

The paper aims to explore the crust types and the aggregates composition differences in micro-topographic soil attacked by raindrops. We studied the distribution characteristics, stability and soil erodibility of crust soil water-stable aggregates at different locations on slopes by simulated rainfall. The results showed that: (1) the water-stable aggregates of undisturbed soil, structural crust, sedimentary crust, transitional zone crust>0.25 mm were 37.28%, 43.58%, 36.69% and 40.34%, respectively; (2) taking the rainfall for 5 min as an example, the PAD of water-stable aggregates of undisturbed soil, structural crust, sedimentary crust and transitional zone crust were 51.49%, 46.00%, 62.76%, 51.02%, respectively; (3) the MWD of water-stable aggregates of undisturbed soil, structural crust, sedimentary crust and transitional zone crust were 0.15, 0.20, 0.14, 0.17 mm, respectively; (4) the erodibility K values of undisturbed soil, structural crust, sedimentary crust and transitional zone crust were 0.223, 0.200, 0.229, 0.205, respectively. The crust differences under micro-topography make the distribution of water-stable aggregates different, so the stability and erodibility of soil water-stable aggregates are different.

Key words: soil aggregates, soil erodibility, Yoder wet screening, crust types, simulated rainfall, micro-topography

CLC Number: