论文

塔里木河水化学变化及其控制途径

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  • 中国科学院新疆生物土壤沙漠研究所,乌鲁木齐

网络出版日期: 1991-07-15

THE HYDROCHEMICAL CHANGE OF TARIM RIVER AND ITS CONTROL WAY

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  • Xinjiang Institute of Biology, Pedology and Desert Research, Chinese Academy of Sciences, Urumqi

Online published: 1991-07-15

摘要

内陆干旱地区的生态环境退化,除沙漠化、盐渍化外,水质盐化也是一个十分突出的问题。塔里木河1958年前是一条淡水河,全河各段河水矿化度没有超过1g/l的。现塔里木河每年只有3个月的淡水期,3个月是1—3g/l的微咸水,6个月为大于3g/l的咸水。塔里木河水质盐化主要是人为活动改变了地区性的水盐与水量平衡,所以,今后在干旱地区进行水土资源开发,必须注意水盐与水量平衡。

关键词: 塔里木河; 水化学; 变化

本文引用格式

樊自立 . 塔里木河水化学变化及其控制途径[J]. 地理学报, 1991 , 46(3) : 319 -326 . DOI: 10.11821/xb199103007

Abstract

As a problem of the degredation of ecotope in the arid areas of inland, the salinization of water quality is as serious as the desertification and salinization of soil. Before 1958, Tarim River was a freshwater river with the general minieralization rate lower than 1 g/1.
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