Relation Between Control in Loess Plateau and No-flow in the Yellow Rever

Li Yushan

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Relation Between Control in Loess Plateau and No-flow in the Yellow Rever

- Relation Between Control in Loess Plateau and No-flow in the Yellow Rever
- Bulletin of Soiland Water Conservation Vol. 16, Issue 6, Pages: 41-44(1997)
- 作者机构：
  
  中国科学院水土保持研究所陕西杨陵,712100
- 作者简介：
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- Published：1997
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Li Yushan. Relation Between Control in Loess Plateau and No-flow in the Yellow Rever[J]. Bulletin of Soiland Water Conservation, 1997, 16(6): 41-44.
DOI：

Li Yushan. Relation Between Control in Loess Plateau and No-flow in the Yellow Rever[J]. Bulletin of Soiland Water Conservation, 1997, 16(6): 41-44. DOI：

摘要

该文从陆地表层资源是一个整体系统观点出发，探讨了黄土高原治理与开发引起的水文循环变化，及其和下游断流的关系。详细分析了植被增加、作物高产、梯坝地建设三个因素，因具有增强水分小循环功能，引起中游径流量减少的结果。特别对农作物和植被作用下，因蒸发蒸腾增强所造成的土壤水文过程干燥化，给予了深入的分析。从机理上探讨黄土高原综合治理开发和下游断流的关系。同时也指出固中游减沙，部分冲沙水量可转入开发水量，因而认为，关于黄土高原综合治理开发对河川水资源量的总效应，需要进行全面深入地研究。

Abstract

On the base of summarizing the cause and treatments of the no-flow in the lower Yellow River

the key aim of this paper is to explore influences of comprehensive control inLoess Plateau on water cycle of Loess plateau and no-flow in the lower Yellow River.Effects of vegetation

high yield of crops

construction of terrace and dam-sludge-land on heightening in small cycle of water and weakening in large cycle of water and reduction of runoff in middle reaches are given in depth analysis.At the same time it is pointed out that a part of water used to wish silt away can transform into use in the lower reaches.Therefore

it is suggested that general effects of comprehensive control in Loess Plateau on water resource in the middle and lower yellow r1ver should be studied deeply.

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