天山北麓前山带对平原区水文过程的影响
收稿日期: 2001-02-02
修回日期: 2001-06-27
网络出版日期: 2001-08-15
基金资助
国家重点基础研究发展规划项目(G1999043507)
Effect of foothill belt on hydro-process of plain area in the northern slope of Tianshan Mountains
Received date: 2001-02-02
Revised date: 2001-06-27
Online published: 2001-08-15
程维明, 周成虎, 汤奇成, 张百平, 姚永慧 . 天山北麓前山带对平原区水文过程的影响[J]. 地理研究, 2001 , 20(4) : 439 -445 . DOI: 10.11821/yj2001040007
The Foothill Belt in the northern slope of the Tianshan Mountains is a transitional znoebetween mountains and plains.It is about 400 km long and 60 km broad from Wusu city to Jimusar city, appearing in three rows of folds with different morphologies and with their age becoming younger from south to north. Based on Geological Information System (GIS) and Remote Sensing (RS) methods, as well as previous research results, this paper systematically discusses the effects of foothill belt on hydro process in plain area. There are four facets of effects. Firstly, the foothill belt can prevent shallowgroundwater from flowing into plains directly, and turn it into surface water flow so as to increasestream runoff. The percentage of groundwater to surface river flow with foothill belt can reach about 47%, but percentage of groundwater to that without foothill belt is only about 37%. Secondly, the foothill belt can enhance annual adjustment abilityof surface rivers, making oasis developsteadily, e.g. the oasis area is about 7 539km 2 in ManasRiver basin with foothill belt is available, but in Sikeshu River basin, the foothill belt oasis area is only about 134km 2 . Thirdly, the foothill belt can prevent floodwateror mud rock flow from entering into plains directly and protect oasis safety. Fourthly,the foothill belt can affect distributions of aquifer'soverflow and buried depth of groundwater level in the plain area,and can control spill amount of groundwater. The foothill beltis importantto surrounding environment, as it can protect the surrounding ecoenvironment, influence land use and land cover change in the plains. Every vertical spectrum with foothill belt is100~200m lower than that without foothill belt. The purpose of this paper is to affer anew understanding about the foothill belt andits functions to environment, especially to hydro process in the plains, and a new idea about how to study interaction between highland and lowlandor mountains and plains. And it can provide scientific basis for utilizing water resources rationally and achievingsustainable development of oasis.
Key words: Tianshan Mountains; northern slope; foothill Belt; hydro process
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