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中国沙漠 ›› 2000, Vol. 20 ›› Issue (1): 45-50.

• 论文 • 上一篇    下一篇

塔里木河下游近50a来沙质荒漠化演变规律

王让会, 樊自立   

  1. 中国科学院 新疆生态与地理研究所, 新疆 乌鲁木齐 830011
  • 收稿日期:1999-05-08 修回日期:1999-06-29 出版日期:2000-03-20 发布日期:2000-03-20
  • 作者简介:王让会(1963-),男(汉族),陕西岐山人,副研究员,博士生,主要从事干旱区资源环境遥感研究工作。
  • 基金资助:
    中国科学院资源与生态环境研究重大项目(KZ951-B1-213)及国家重点基础研究项目(G19990435)

Evolution Patterns of Sandy Desertification in the Lower Reaches of Tarim River Basin in Recent 5 Decades

WANG Rang-hui, FAN Zi-li   

  1. Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
  • Received:1999-05-08 Revised:1999-06-29 Online:2000-03-20 Published:2000-03-20

摘要: 荒漠化是人为强烈活动与脆弱生态环境相互作用的产物,是人地关系矛盾的结果。我国最长的内陆河-塔里木河下游卡拉的来水量,由50年代的14.80亿m3减少到90年代的2.38亿m3,造成地下水位下降,植被衰败。同时,受过度放牧、开垦、樵采等原因的影响,下游地区土地沙质荒漠化十分严峻,宏观格局上表现为绿色走廊由上段至下段,由中间至两侧沙漠化程度趋于加强。通过1959、1983、1992及1996年遥感信息制图定量研究表明,50年代至90年代沙漠化年均增长率达0.24%,其面积扩大的同时,程度也在加剧,自然景观也发生了一系列变化。应用GM(1,1)模型、非线性回归模型及多元线性回归模型趋势分析表明,以土地沙质荒漠化为主的环境问题仍十分突出。科学规划,整治上、中游河道,合理利用水资源,以解决下游生态及生产、生活用水。应用RS、GIS监测沙漠化变化,通过增加生态用水,恢复铁干里克-阿拉干段的天然植被,遏制沙漠化扩展,同时利用工程措施,保护阿拉干以下绿洲走廊及218国道安全畅道,防止脆弱生态环境继续恶化。

关键词: 塔里木河下游, 沙质荒漠化, 演变规律, 控制途径

Abstract: Desertification is the result of interaction between human being and fragile eco-environment.It is also the consequence of the contradiction between human being and land.The water amount in Qiala station at the lower reaches of Tarim River is reduced from 14.80×108 m3 in 1950s to 2.38×108m3 in 1990s,which causes the reduction of underground water table and the degradation of vegetation.Meanwhile,under the influences of extreme raising living stock,reclaiming wasteland and cutting off firewood,sandy desertification developes seriously in the lower reaches area,whose degree is becoming strongly and strongly from upper section to lower section and from the middle to both sides of the Green Corridor on macro pattern.Mapping with remote sensing information of 1959,1983,1992 and 1996,the result shows that the annual mean growth rate of sandy desertification area is 0.24 percent from 1950s to 1990s.With area increasing the degree is strengthened.At the same time,a series of changes in natural landscape have occurred.The result of trend analyses with models of GM(1,1),non linear regression and multi-factor regression reveals that environment problems predominated by land desertification are quite out-standing.In order to solve the problem of water resources in ecology,production and life in the lower reaches area,it should be available to plan scientifically,use water resources rationally and control river courses in the upper and middle reaches of Tarim River.In addition to recover natural vegetation and prevent sandy desertification from expanding between Qieganlike and Alagan,monitoring sandy desertification changes by RS and GIS as well as increasing ecological water amount are very important.Meanwhile,in order to protect the Green Corridor and safeguard the No.218 national highway in the lower reaches of Tarim River area,some engineering measurements should be adopted.

Key words: the lower reaches of Tarim River, sandy desertification, evolution pattern, controlling approaches

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