Comparing surface erosion processes in four soils from the Loess Plateau under extreme rainfall events

被引:46
作者
Sun, Liying [1 ,2 ]
Zhou, John L. [3 ]
Cai, Qiangguo [1 ,2 ]
Liu, Suxia [1 ,2 ]
Xiao, Jingan [1 ,2 ]
机构
[1] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing 100101, Peoples R China
[2] Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100049, Peoples R China
[3] Univ Technol Sydney, Sch Civil & Environm Engn, 15 Broadway, Sydney, NSW 2007, Australia
基金
中国国家自然科学基金;
关键词
Soil erosion process; Particle size; Surface erosion; Cropland management; Loess Plateau; INTERRILL EROSION; RILL EROSION; SLOPE GRADIENT; RAINDROP-IMPACT; WATER EROSION; AGGREGATE STABILITY; SPLASH EROSION; SIZE-SELECTIVITY; SEDIMENT YIELD; SEAL FORMATION;
D O I
10.1016/j.iswcr.2021.06.008
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This research aims to improve erosion control practice in the Loess Plateau, by studying the surface erosion processes, including splash, sheet/interrill and rill erosion in four contrasting soils under high rainfall intensity (120 mm h(-1)) with three-scale indoor artificial experiments. Four contrasting soils as sandy loam, sandy clay loam, clay loam and loamy clay were collected from different parts of the Loess Plateau. The results showed that sediment load was significantly impacted by soil properties in all three sub-processes. Splash rate (4.0-21.6 g m(-2).min(-1)) was highest in sandy loam from the north part of the Loess Plateau and showed a negative power relation with the mean weight diameter of aggregates after 20 min of rainfall duration. The average sediment load by sheet/interrill erosion (6.94 -42.86 g m(-2).min(-1)) was highest in clay loam from middle part of the Loess Plateau, and the stable sediment load after 20 min showed a positive power relation with the silt content in soil. The average sediment load increased dramatically by rill and interrill erosion (21.03-432.16 g m(-2).min(-1)), which was highest in loamy clay from south part of the Loess Plateau. The average sediment load after the occurrence of rill showed a positive power relation with clay content and a negative power relation with soil organic matter content. The impacts of slope gradient on the runoff rate and sediment load also changed with soil properties. The critical factors varied for different processes, which were the aggregate size for splash erosion, the content of silt particles and slope gradient for sheet/interrill erosion, and the content of clay particles, soil organic matter and slope gradient for rill erosion. Based on the results of the experiments, specific erosion control practices were proposed by targeting certain erosion processes in areas with different soil texture and different distribution of slope gradient. The findings from this study should support the improvement of erosion prediction and cropland management in different regions of the Loess Plateau. (C) 2021 International Research and Training Center on Erosion and Sedimentation, China Water & Power Press. Publishing services by Elsevier B.V. on behalf of KeAi Communications Co. Ltd.
引用
收藏
页码:520 / 531
页数:12
相关论文
共 74 条
  • [1] Splash erosion under natural rainfall on three soil types in NE Spain
    Angulo-Martinez, M.
    Begueria, S.
    Navas, A.
    Machin, J.
    [J]. GEOMORPHOLOGY, 2012, 175 : 38 - 44
  • [2] Flow-driven soil erosion processes and the size selectivity of sediment
    Asadi, H.
    Moussavi, A.
    Ghadiri, H.
    Rose, C. W.
    [J]. JOURNAL OF HYDROLOGY, 2011, 406 (1-2) : 73 - 81
  • [3] Effects of rainfall intensity and slope gradient on the dynamics of interrill erosion during soil surface sealing
    Assouline, S.
    Ben-Hur, A.
    [J]. CATENA, 2006, 66 (03) : 211 - 220
  • [4] Rates of sheet and rill erosion in Germany - A meta-analysis
    Auerswald, K.
    Fiener, P.
    Dikau, R.
    [J]. GEOMORPHOLOGY, 2009, 111 (3-4) : 182 - 193
  • [5] RILL EROSION AS A FUNCTION OF THE CHARACTERISTICS OF CULTIVATED CATCHMENTS IN THE NORTH OF FRANCE
    AUZET, AV
    BOIFFIN, J
    PAPY, F
    LUDWIG, B
    MAUCORPS, J
    [J]. CATENA, 1993, 20 (1-2) : 41 - 62
  • [6] Rill development and soil erosion: a laboratory study of slope and rainfall intensity
    Berger, Catherine
    Schulze, Marcel
    Rieke-Zapp, Dirk
    Schlunegger, Fritz
    [J]. EARTH SURFACE PROCESSES AND LANDFORMS, 2010, 35 (12) : 1456 - 1467
  • [7] Brunton DA, 2000, EARTH SURF PROC LAND, V25, P783, DOI 10.1002/1096-9837(200007)25:7<783::AID-ESP106>3.0.CO
  • [8] 2-W
  • [9] Soil erodibility and processes of water erosion on hillslope
    Bryan, RB
    [J]. GEOMORPHOLOGY, 2000, 32 (3-4) : 385 - 415
  • [10] Runoff features for interrill erosion at different rainfall intensities, slope lengths, and gradients in an agricultural loessial hillslope
    Chaplot, VAM
    Le Bissonnais, Y
    [J]. SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 2003, 67 (03) : 844 - 851