WANG Hui, HU Xiujun, SHAN Chengju. Effect of Rainfall Intensity and Slope Gradient on Runoff and Sediment Yield on the Red Soil Slope Nested Gravel-sand[J]. 2018, 32(4): 24-29.
DOI:
WANG Hui, HU Xiujun, SHAN Chengju. Effect of Rainfall Intensity and Slope Gradient on Runoff and Sediment Yield on the Red Soil Slope Nested Gravel-sand[J]. 2018, 32(4): 24-29. DOI: 10.13870/j.cnki.stbcxb.2018.04.005.
Effect of Rainfall Intensity and Slope Gradient on Runoff and Sediment Yield on the Red Soil Slope Nested Gravel-sand
The characteristics of runoff and sediment yield on the red soil slope nested gravel-sand were studied through artificial simulated rainfall
and the differences of runoff and sediment yield between nested gravel red soil slope and no gravel slope under the conditions of rainfall intensity (60
120 mm/h) and slope gradient (10°
15°
20° and 25°) were analyzed. The results were as follows:(1) The start time of production runoff (T) on the nested gravel slope was less than that on the no gravel slope
and compare with no gravel slope
the runoff production time on the nested gravel slope was delayed 4.20
2.95
2.23 and 1.03 min
respectively
when the slope gradient was 10°
15°
20° and 25° under the rainfall intensity 60 mm/h. (2) When the slope gradient was the same
the runoff rate of the nested gravel-sand slope was less than that of no gravel slope obviously
but the increase of rainfall intensity could cover up the influence of nested gravel-sand on the decrease of runoff rate. (3) When the rainfall intensity was 60 mm/h and the slope was 10°
the average runoff rate of nested gravel-sand slope was the lowest
while the average runoff rate was 4.5 times higher than the lowest value when the rainfall intensity was 120 mm/h and the slope gradient was 25°. When the rainfall intensity was 120 mm/h and the slope gradient was 25°
the average runoff rate of no gravel-sand slope was 4.8 times higher than the lowest. (4) The sediment yield intensity and the amount of sediment yield increased with the increasing of rainfall intensity and slope gradient. When the rainfall intensity was 60 mm/h and the gradient was 10° and 25°
the average sediment yield intensity of nested gravel-sand slope was 6.0% and 28.4% of the no gravel slope
respectively. When the rainfall intensity was 120 mm/h
the value was 33.9% and 25.3%
respectively.
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Keywords
references
Miller F T, Guthrie R L. Classification and distribution of soils containing rock fragments in the United States[J]. Soil Science Society America Journal Special Publication,1984,13:1-6.
Cerda A. Effects of rock fragment cover on soil infiltration, interrill runoff and erosion[J].European Journal of Soil Science,2001,52:59-68.
Diaz F, Jimenez C C, Tejedor M. Influence of the thickness and grain size of tephra mulch on soil water evaporation[J]. Agricultural Water Management,2005,74(1):47-55.
Poesen J, Ingelmo-Sanchez F, Mucher H. The hydrological response of soil surfaces to rainfall as affected by cover and position of rock fragments in the top layer[J]. Earth Surface Processes and Landforms,1990,15(7):653-671.
Zhao X, Wu P, Chen X, et al. Runoff and sediment yield under simulated rainfall on hillslopes in the Loess Plateau of China[J]. Soil Research, 2013,51:50-58.
Effect of Slope Gradients on Erosion from a Red Soil Hillslope under Different Rainfall Intensity
Characteristics of the Runoff and Sediment Yield of Sloping Farmland in the Purple Soil Area Under Different Rainfall Patterns
Characteristics of Rainfall Runoff and Hydrological Dynamics on the Erosive Weathered Granite Slope
Effects of Slope Gradient and Rainfall Intensity on Nitrogen Loss Under Artificial Simulated Rainfall
Experimental Study on Sheet Flow Resistance Coefficient of Grassland in Loess Area
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Related Institution
ZHANG Hui-ru1,2,ZHENG Fen-li2,3(1.Yanan Soil and Water Conservation Monitoring Sub-station,Yanan,Shaanxi 716000,2.College of Resources and Environment,Northwest A&F University,Yangling,Shaanxi 712100,3.State Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau,Institute of Soil and Water Conservation,CAS&MWR,)
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