雨强和坡度对嵌套砾石红壤坡面产流产沙的影响

王蕙; 胡秀君; 山成菊

doi:10.13870/j.cnki.stbcxb.2018.04.005

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雨强和坡度对嵌套砾石红壤坡面产流产沙的影响

更新时间：2025-03-12

- 雨强和坡度对嵌套砾石红壤坡面产流产沙的影响
- Effect of Rainfall Intensity and Slope Gradient on Runoff and Sediment Yield on the Red Soil Slope Nested Gravel-sand
- 水土保持学报 2018年32卷第4期页码：24-29
- 作者机构：
  
  浙江水利水电学院水利与环境工程学院,杭州,310018
- 作者简介：
  
  [ "王蕙(1979-),女,汉族,讲师,博士,主要从事水土保持与生态水文学研究。E-mail:wanghui@zjweu.edu.cn" ]
- 基金信息：
  
  国家自然科学基金项目（41701312）浙江省自然科学基金项目（LQ16D010004）
- DOI：10.13870/j.cnki.stbcxb.2018.04.005
  中图分类号：
- 纸质出版：2018
- 稿件说明：
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王蕙, 胡秀君, 山成菊. 雨强和坡度对嵌套砾石红壤坡面产流产沙的影响[J]. 水土保持学报, 2018,32(4):24-29.

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.
王蕙, 胡秀君, 山成菊. 雨强和坡度对嵌套砾石红壤坡面产流产沙的影响[J]. 水土保持学报, 2018,32(4):24-29. DOI： 10.13870/j.cnki.stbcxb.2018.04.005.

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.

摘要

采用人工模拟降雨的方法研究了嵌套砾石红壤坡面的产流产沙特征，分析了雨强（60，120 mm/h）和坡度（10°，15°，20°，25°）条件下嵌套砾石和无砾石红壤坡面的产流和产沙过程差异。结果表明：（1）产流开始时间T嵌套砾石 < T无砾石，60 mm/h雨强条件下嵌套砾石较无砾石坡面在10°，15°，20°，25°坡度分别延迟4.20，2.95，2.23，1.03 min；（2）坡度相同时，嵌套砾石坡面较无砾石坡面产流率明显减少，但雨强的增大会掩盖嵌套砾石对坡面产流率减小的影响；（3）嵌套砾石红壤坡面在60 mm/h雨强、坡度10°条件下平均产流率最小，在120 mm/h雨强、25°坡面下平均产流率是前者的4.5倍；无砾石红壤坡面在120 mm/h雨强、坡度25°条件下平均产流率最大，为最小平均产流率的4.8倍；（4）各坡面产沙强度、次降雨产沙量随雨强和坡度增大而增大，60 mm/h雨强、坡度10°和25°时，嵌套砾石坡面平均产沙强度为无砾石坡面的6.0%和28.4%；120 mm/h雨强时，此两个坡度的嵌套砾石坡面为无砾石坡面平均产沙强度的33.9%和25.3%。

Abstract

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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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.

雷志栋,胡和平,杨诗秀.土壤水研究进展与评述[J].水科学进展,1999,10(3):311-318.

Ma D, Shao M. Simulating infiltration into stony soils with a dual-porosity model[J].European Journal of Soil Science,2008,59(5):950-959.

符素华,段淑怀,刘宝元.密云石匣小流域土地利用对土壤粗化的影响[J].地理研究,2001,20(6):697-702.

李燕,高明,魏朝富.土壤砾石的分布及其对水文过程的影响[J].中国农学通报,2006,6(5):271-276.

吕忠恕,陈邦瑜.甘肃砂田的研究[J].农业学报,1955,6(3):299-312.

Li X Y. Gravel-sand mulch for soil and water conservation in the semiarid loess region of northwest China[J].Catena,2003,52:105-127.

刘谦和,李志强.砂田土壤的水蒸发特征和温度变化[J].甘肃农业科技,1993(8):27-28.

陈士辉,谢忠奎,王亚军,等.砂田西瓜不同粒径砂砾石覆盖的水分效应研究[J].中国沙漠,2005,25(30):433-436.

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.

付兴涛,张丽萍.红壤丘陵区坡长对作物覆盖坡耕地土壤侵蚀的影响[J].农业工程学报,2014,30(5):91-98.

耿晓东,郑粉莉,刘力.降雨强度和坡度双因子对紫色土坡面侵蚀产沙的影响[J].泥沙研究,2010(6):48-53.

陈正发,郭宏忠,史东梅,等.地形因子对紫色土坡耕地土壤侵蚀作用的试验研究[J].水土保持学报,2010,24(5):83-87.

史倩华,王文龙,郭明明,等.模拟降雨条件下含砾石红壤工程堆积体产流产沙过程[J].应用生态学报,2015,26(9):2673-2680.

邵明安,王全九,黄明斌,等.土壤物理学[M].北京:高等教育出版社,2006:57-58.

张会茹,郑粉莉.不同降雨强度下地面坡度对红壤坡面土壤侵蚀过程的影响[J].水土保持学报,2011,25(3):40-43.

梁洪儒,余新晓,樊登星,等.砾石覆盖对坡面产流产沙的影响[J].水土保持学报,2014,28(3):57-61.

王丽园,查轩,黄少燕,等.不同雨强条件下坡度对红壤坡面侵蚀的影响[J].水土保持学报,2017,31(5):40-44.

王小燕,李朝霞,徐勤学,等.砾石覆盖对土壤水蚀过程影响的研究进展[J].中国水土保持科学,2011,9(1):115-120.

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.

刘宏伟,余钟波,崔广柏.湿润地区土壤水分对降雨的响应模式研究[J].水利学报,2009,40(7):822-829.

王志伟,陈志成,艾钊,等.不同雨强与坡度对沂蒙山区典型土壤坡面侵蚀产沙的影响[J].水土保持学报,2012,26(6):17-20.

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.

毛天旭,朱元骏,邵明安,等.模拟降雨条件下含砾石土壤的坡面产流和入渗特征[J].土壤通报,2011,42(5):1214-1218.

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