[1]BAI Hua,MU Xing-min,WANG Shuang-yin.Impact of Soil and Water Conservation on River Flow of Tuwei River[J].Research of Soil and Water Conservation,2010,17(01):40-44.
Copy
Impact of Soil and Water Conservation on River Flow of Tuwei River
Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume:
17
Number of periods:
2010 01
Page number:
40-44
Column:
Public date:
2010-02-20
- Title:
- Impact of Soil and Water Conservation on River Flow of Tuwei River
- Keywords:
- rainfall; run-off; soil and water erosion; soil and water consevation; similar rainfall; Tuwei river; the Loess Plateau
- CLC:
- S157.2;P333.1
- DOI:
- -
- Abstract:
- In view of the factors affecting run-off,it is effective to reflect the soil and water conservation’s contribution to the run-off by analysis and comparison of changes in the run-off before and after soil erosion control.Based on the data of rainfall runoff storm and flood,the characters of rainfall runoff storm and flood in the catchment have been comprehensively analyzed through the method of Mann-kendall etc.According to the turning point of rainfall-runoff cumulative curve,the changes in the volume of runoff have been restored caused by the dynamic changes in precipitation and the changes in the run-off elements has been calculated owing to the water and soil conservation.The standard of judging the similar rainfall has been worked out,by which the changes of the flood’s elements and progress has been analyzed among different periods.Analysis showed:the turning point of the annual average flow sequence is in 1977.After this turning point,multi-year average runoff depth and proportion of run-off during the flood season decreases.Proportion of run-off during the dry season increases.The degree of inter-annual dramatic changes decline,the flood volume and peak flow has reduced and flood process has been averaged.
- References:
-
[1] 朱恒峰,赵文武,康慕宜,等.水土保持地区人类活动对汛期径流影响的估算[J].水科学进展,2008,19(3):400-405.
[2] 汪岗,范昭.黄河水沙变化研究[M].(2卷).郑州:黄河水利出版社,2002.
[3] 姚文艺,李占斌,康玲玲.黄土高原土壤侵蚀治理的生态环境效应[M].北京:科学出版社,2005.
[4] 冉大川,柳林旺,赵力仪,等.黄河中游河口镇至龙门区间水土保持与水沙变化[M].郑州:黄河水利出版社,2000.
[5] 李勇,董雪娜,张晓华,等.黄河水沙特性变化研究[M].郑州:黄河水利出版社,2004.
[6] 许炯心.黄河中游多沙粗沙区水土保持减沙的近期趋势及其成因[J].泥沙研究,2004(2):5-10.
[7] 穆兴民.黄土高原水土保持对河川径流及土壤水文的影响[D].陕西杨陵:西北农林科技大学,2001.
[8] 李占斌,符素华,鲁克新.秃尾河流域暴雨洪水产沙特性的研究[J].水土保持学报,2001,15(2):88-91.
[9] 穆兴民,李靖.黄河天然径流量年际变化过程分析[J].干旱区资源与环境,2003,17(2):1-5.
[10] 穆兴民.黄土高塬沟壑区水土保持对小流域地表径流的影响[J].水利学报,1999,(2):71-75.
[11] 穆兴民,陈霁巍,王文龙,等.水利水保工程对佳芦河流域暴雨洪水的影响分析[J].水土保持通报,2000,20(7):24-27.
- Similar References:
Memo
-
Last Update:
1900-01-01