摘要
艾比湖与苏联境内的萨司克湖、阿拉湖同属于一个断裂构造带的陷落湖,形成于新生代第三纪喜马拉雅运动期内,现湖水面积542km^2,湖底平坦,据艾比湖盐场测量,坡度在0.15‰～0.37‰(表1),最大水深约2.8m,平均水深约1.4m,储水量约7.6亿m^3。湖面12月封冻,翌年3月解冻,最大冰厚0.32m,汽车可在冰上行驶。
From 1950 to 1977 Ebinur lake had been changed greatly by the effect of human activ-ities and its area had decreased from 1070km^2. The ecological environment around the lakehad been changed violcntly for the period ,Since 1980's the lake tended to be rclatively sta-bie on account of small influence of human activities.
出处
《干旱区地理》
CSCD
北大核心
1990年第4期45-50,共6页
Arid Land Geography
