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塔里木河中游土地沙漠化与环境因子关系研究
引用本文:赵元杰,王让会.塔里木河中游土地沙漠化与环境因子关系研究[J].干旱区地理,1999,22(3):57-63.
作者姓名:赵元杰  王让会
作者单位:中国科学院新疆生态与地理研究所,乌鲁木齐,830011
基金项目:“九五”国家重点科技攻关项目专题!(96-912-02-02)
摘    要:根据已有的和大量的调查地贡巴扎地区沙漠化与主导环境因子之间的关系进行了研究,结果表明:沙漠化形成主要因子的重要性依次为地下水位,植被,微地貌类型、土壤质地。以沙漠化研究为基础的维护合理的生态水位应为4.4米左右。

关 键 词:塔里木河  沙漠化  生态环境  保护
修稿时间:1999年3月16日

STUDY ON RELATION BETWEEN LAND DESERTIFICATION AND ENVIRONMENT FACTORS IN MIDDLE STREAM REGION OF TARIM RIVER
ZHAO Yuanjie,Wang Ranghui.STUDY ON RELATION BETWEEN LAND DESERTIFICATION AND ENVIRONMENT FACTORS IN MIDDLE STREAM REGION OF TARIM RIVER[J].Arid Land Geography,1999,22(3):57-63.
Authors:ZHAO Yuanjie  Wang Ranghui
Abstract:Yinbazha district is located in the middle stream of Tarim river with such characters as extreme drought, salinization, strong wind-sand, soil of light texture, sparse plant and desertification. Basis on the existing and a great deal of data surveyed on the field, this paper studies the relationship between the desertification and the important environmental factors. Results of the studies show that the factors obviously to impact on the formation and improvement of desertification in the region of Yingbazha are underground water level, plant, micro- geomorphy, and soil texture in turn. Plant situation plays an important role in restraining the formation and improvement of the desertfication. The relationship between the middle value of the plant coverage and the desertification degree can be described as follow: Y= 0.428-0. 078X. The general regulation of the change of desertification with the change of the underground water level are: (1 ) With the increment of the desertification degree, the scale of underground water level is from the wide to narrow; (2) The underground water level of the emergence of every desertification is from the shallow to the deep. The relationship between the mean quantity of underground water level and the desertification degree is: Y = 4. 258 - 0. 778X. Although the strongest desertification can be formed on the condition of underground water level of 4 m, on the other hand the non - desertification also can be formed on the condition of underground water level of 9 m, which only shows that underground water level does not obviously influence on the desertification in short time because of the course change of Tarim river, the underground water level of 4. 4m is suitable to maintain the ecological environment in general and in a long term on the basis of desertification study. Results of the studies provide the basis for improving the operationablity of ecological environment conservation in the basin of Tarim.
Keywords:Tarim river  Desertification Ecological environment Conservation  
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