CAO Yuan, SUN Peng, YAO Rui, et al. Effects of Engineering Measures on the Runoff and Sediment Yield in Slope Land Under Different Rainfall Intensities[J]. 2020, 34(6): 1-7.
DOI:
CAO Yuan, SUN Peng, YAO Rui, et al. Effects of Engineering Measures on the Runoff and Sediment Yield in Slope Land Under Different Rainfall Intensities[J]. 2020, 34(6): 1-7. DOI: 10.13870/j.cnki.stbcxb.2020.06.001.
Effects of Engineering Measures on the Runoff and Sediment Yield in Slope Land Under Different Rainfall Intensities
Based on the daily precipitation and runoff sediment yield data in 2016 and 2017 under different slope land measures (slope farmland and changing slope to terrace) in the test station
the law characteristics of runoff sediment yield under different slope land measures and rainfall intensities were studied. The impact of changing slope to terrace and slope farmland on runoff and sediment was quantitatively revealed. The results showed that: (1) In July
the average rainfall intensity I
the maximum rainfall intensity I30 and the slope land runoff were the largest
and in August
the maximum rainfall intensity I60 and the slope land sediment yield were the largest
indicating that the peak of runoff and sediment was the same as the peak of rainfall intensities. (2) The correlations between runoff and sediment yield in spring and summer and I
I30 and I60 were significant (more than 95% confidence test). The correlation coefficients in slope land were higher than those in changing slope to terrace land. In spring and summer
the sediment yields in slope land were 3.91 and 7.85 times of those in changing slope to terrace land. (3) The rainfall was mainly concentrated in I: 1~3 mm/h
I30: 3~29 mm/h
I60: 2~27 mm/h
and the runoff and sediment yield in slope land was positively correlated with the maximum rainfall intensity I30 and I60 at 95% confidence level. When I30 reached 29.0 mm/h
I60 reached 26.6 mm/h
the runoff and sediment yield in slope land reached the maximum. The peak values of runoff and sediment yield in slope land were 2.43
7.52 times higher than those in changing slope to terrace land. The variation coefficients of runoff and sediment yield in the whole year were higher than those in changing slope to terrace land. Thus
changing slope land to terrace could prevent soil erosion to a certain extent
and reduce the variation of runoff and sediment yield.
Meester T. Soil erosion and conservation[J].Earth Science Reviews,1987,24(1):68-69.
Oosten V, Ary M. The political economy of soil erosion in developing countries[J].Land Use Policy,1985,2(4):355-356.
Liu D D, She D L, Yu S E, et al. Rainfall intensity and slope gradient effects on sediment losses and splash from a saline-sodic soil under coastal reclamation[J].Catena,2015,128:54-62.
Jia C F, Sun B P, Yu X X, et al. Analysis of runoff and sediment losses from a sloped roadbed under variable rainfall Intensities and vegetation conditions[J].Sustainability,2020,12(5). DOI:10.3390/su12052077.
Tarolli P. Agricultural terraces special issue preface[J].Land Degradation and Development,2018,29(10):3544-3548.
Baets S, Poesen J, Knapen A, et al. Root characteristics of representative Mediterranean plant species and their erosion-reducing potential during concentrated runoff[J].Plant and Soil,2007,294:169-183.
Bissonnais Y, Renaux B, Delouche H. Interactions between soil properties and moisture content in crust formation, runoff and interrill erosion from tilled loess soils[J].Catena,1995,25(1):33-46.