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干旱区地理 ›› 1991, Vol. 14 ›› Issue (2): 41-47.doi: 10.13826/j.cnki.cn65-1103/x.1991.02.007

• • 上一篇    下一篇

1989年察尔汗盐湖地区暴发的特大洪水

胡东生   

  1. 中国科学院盐湖研究所
  • 出版日期:1991-06-25 发布日期:2025-12-25

A CATASTROPHIC FLOOD IN CHARHAN SALT LAKE DURING 1989

Hu Dongseng   

  1. Institute of Salt Lake, Chinese Academy of Sciences
  • Published:1991-06-25 Online:2025-12-25

摘要: 通过野外地质调查和地球观测卫星同步跟踪预接收遥感信息资料,对察尔汗盐湖1989年夏秋之交暴发的特大洪水进行洪水特征、洪水效应、洪水周期以及洪水事件、洪水成盐、洪水控制等方面的系统研究,对盐湖地区的洪水评价及资源开发具有重要意义。

关键词: 特大洪水, 洪水事件, 察尔汗盐湖

Abstract: Charhan Salt lake, locating in the middle of Qaidamu basin, consists of the shallow depression which is fed by phreatic water and outside water system, and salt marsh. Its areas is 5856 km , and the highest ratio of solid/liquid of salt mineral resorces is 1/3.46 . the lowestl/1. 28. The salt-out action is a typical process of charhan lake, and so it is a "live"mineral.
In this paper , the property and effect of catastrophic flood that have occured in 1989 is studied by satelliate remote image and field exploration. The flood is the largest one since there are a hydrologic record and have made the lake expension, desalination and karst. Germu river Whose 70% water flows into the lake is the cause of the flood. The data of hydrology and meteorology in Germu river during past 28 year shows that bigger flood (about 300±m/S) in the area will occur with the interval of 7or8year, and the Catastrophic fiood is about 300 year. The author Considers that the flood over 200 m/S will occur for 2to 3times and that of 500 m/S occur 1 times in the next decade.
The Suggestion of studing the dynamic balances of the flood-salt lake by using remote Sensing methods are proposed.