Similarity Between Erosion and Sediment Yield Processes on Steep Slopes with Simulated Rainfalls Under Indoor and Outdoor Condition
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Similarity Between Erosion and Sediment Yield Processes on Steep Slopes with Simulated Rainfalls Under Indoor and Outdoor Condition
Bulletin of Soiland Water ConservationVol. 30, Issue 5, Pages: 191-195(2011)
作者机构:
1. 郑州大学水利与环境学院
2. 黄河水利科学研究院
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Published:2011
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Guan Xin-jian, Li Mian, Hu Cai-hong, et al. Similarity Between Erosion and Sediment Yield Processes on Steep Slopes with Simulated Rainfalls Under Indoor and Outdoor Condition[J]. Bulletin of Soiland Water Conservation, 2011, 30(5): 191-195.
DOI:
Guan Xin-jian, Li Mian, Hu Cai-hong, et al. Similarity Between Erosion and Sediment Yield Processes on Steep Slopes with Simulated Rainfalls Under Indoor and Outdoor Condition[J]. Bulletin of Soiland Water Conservation, 2011, 30(5): 191-195.DOI:
Similarity Between Erosion and Sediment Yield Processes on Steep Slopes with Simulated Rainfalls Under Indoor and Outdoor Condition
In order to study the chatacteristics of different soil erosion and sediment yield indoor and outdoor under rainfall condition
the erosion processes of Mangshan mountain loess were tested under laboratory and undisturbed conditions on 25°steep slopes under artificial simulated rainfalls.The similarity characteristics of the indoor and outdoor process of erosion and sediment yield were analyzed by the fuzzy closeness degree calculation method.The results show that with the rains of same intensity
runoff amount
sediment concentration
shear stress
and sediment yield of different soil bulk densities were fairly low at the initial stage and increased gradually over time;when the rain intensity reached the hyperplastic spot
these indicators increased sharply to the steady state within a few minutes.On 25°steep slopes
the nearness degree of the shear strength
runoff rate
sediment concentration and sediment yield of both indoor and outdoor simulation were very similar for the two kinds of soil bulk densities.The nearness degree of the high bulk density(1.2 g/cm3)soil was greater than the low bulk density(1.0g/cm3)soil.This implies that in order to achieve a laboratory condition similar to the field condition
the soil with higher bulk density should be applied in the simulations.