遥感影像上的罗布泊及其变迁
The Environmental Evolutions of Lake Lop-nor as Seen on the Remote Sensing Images
- 1987年第4期 页码:285-295
纸质出版日期: 1987
DOI: 10.11834/jrs.1987039
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纸质出版日期: 1987 ,
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[1]粱匡一.遥感影像上的罗布泊及其变迁[J].环境遥感,1987(04):285-295+325.
Liang Kuangyi. The Environmental Evolutions of Lake Lop-nor as Seen on the Remote Sensing Images[J]. Journal of Remote Sensing, 1987,(4):285-295.
很长时间以来罗布泊被误认为游移湖
而且在各种文献上所论述及标绘的位置、大小、形状全然不对。60年代拍摄的航空像片及70年代拍摄的卫星像片准确地反映了罗布泊的各种自然条件。它是一个稳定的、受地质构造和新构造运动控制的、补给的水量急剧减少而最后干涸的一个大内陆湖。湖的中心部份正位于阿奇克地堑的不断沉陷区。笔者认为通过对这些遥感影像的深入分析和论证
将不会再被“游移说”所误。 罗布泊由两个水系所补给:一是从北西入湖的孔雀河水;二是从西南入湖的塔里木河与车尔臣河水
前者只占极小的比例。历史上最大湖面面积是12600平方公里
内湖潴水时间较长
为5140平方公里。塔里木河水在入湖前受新构造运动的影响
共形成五级三角洲
其第五级正在现代的湖沿上。全湖于1970年前后彻底干涸。 地垒的存在为本文的判读结论
它就是遥感影像上看到的不正常湖形的原因。除地垒形成的早期有孔雀河水流到北缘上外
湖水未曾停于其上。F
2
断裂之西形成陡坎
塔里木河水在陡坎下向北流
但未流入湖内。
Lop-nor has long been misunderstood as a "wandering lake". Its location
size
shape as shown on old maps and in past literatures are not correct. Began from the sixties
the aero-photos
and seventies
the Landsat images were obtained. They showed accurately all the detailed natural criteria of the Lop-nor: it had been a very stable
in-land lake
and was controlled by geo-tectonic and neo-tectonic in shape and evolutions. The water pouring into the lake from the rivers enormously deduced
and finally the lop-nor dried out totally at the beginning of seventies.The centeral part of the lake is located in the successive subsidence area of "Aqik Gra-ben". The author considers that this study has used all the recent remote sensing images with high precision so there should be no further rumor that the Lop-nor had been a wandering lake.Lop-nor was fed by two water systems
one of it was the river water that entered the NW part of Lop-nor-namely Kon-quie Dyria
the other was the river water both from Tarim and Cher-cheng
the discharge from the former was only a small proportion. The biggest surface area of the lake in the history had been about 12600 km
the lake in laterstage had a longer period of water storage
the water surface area was about 5140 km2. Before the Tarim river flew into the lake
it formed 5 overlapping
advancing alluvial fans
which meant 5 stages of sinking of Lop-nor.The occurence of "horst" in the W and NW part of Lop-nor is the conclusion of the author’s image interpretation. On the image
one cannot find a normal western lake margin. There had been small amount of water immersions on the most northern part of the horst that fed by the Konquie Dyria
but there was no trace of lake water that had immersed the whole horst. At the west wall (steep-bank) of the Fa
the Tarim River water flew along the bank towards N
but could not enter the lake.
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