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塔里木盆地南缘古绿洲分布与河流、冰川的关系
  • ISSN号:1000-6060
  • 期刊名称:《干旱区地理》
  • 时间:0
  • 分类:P941.71[天文地球—自然地理学]
  • 作者机构:[1]北京联合大学应用文理学院,北京100083, [2]新疆绿洲生态重点实验室.新疆830046, [3]南京大学海岸与海岛开发教育部重点实验室,南京210093
  • 相关基金:国家自然科学基金(40771194);教育部绿洲重点实验室(XJDX0208-2004-07);教育部春晖计划(72004-1-65009).
中文摘要:

依据野外实地考察和考古资料对塔里木盆地南缘河流与其流域内的古绿洲分布情况进行了研究,着重探讨了历史时期以来古绿洲分布规律、迁移过程与河流、冰川特点之间的耦合关系。研究表明,盆地南缘东侧的且末、若羌地区河流及冰川规模小,数量少;其中下游形成的绿洲小,且从汉代至今都在河流出山口处分布,变化不大,而西侧的和田地区反之,河流下游的沙漠中分布着数量较多的大规模古绿洲;汉代的古绿洲多分布在冲积平原下部的沙漠中心,中部则是以唐代古绿洲遗址为主,上部沙漠边缘多为近代和现代绿洲;古绿洲迁移最大距离可达200km左右;河流年径流量与古绿洲在沙漠分布的距离呈正相关关系。

英文摘要:

According to the field work, the document record and the archeology resource on the rivers in the Tarim basin and on the basic of the comprehensive study on the distance, the scale and the location of the ancient oases, this paper discusses the relationship between the distribution regularity and development process of the ancient oases and the rivers and glaciers. The characteristics of the ancient oases depend on the size of the rivers. The rivers in Qiemo and Ruoqiang region at the southeast of the Tarim basin are of small scale and runoff but in the Hetian region and in the west of the Tarim basin the rivers are of big scale and runoff. Therefore, the oases in the Altun Mountains are small and change little. The oases lie on the edge of the alluvial plain in front of the mountains from Han Dynasty to nowadays. The large ancient oases mostly are located on the northern slope of the Kunlun Mountain. The ancient oases have large areas and scales and change in a large scale. The oases mostly are sited at the lower reaches of the local rivers in the Han Dynasty and sited at the middle reaches in Tang Dynasty and the modem oasis sited at some middle reaches and the upper reaches. The abandon of the oases were taken place gradually from the lower reaches to the upper reaches. The maximal moving distance is about 200 km. So the temporal and spatial changes of the ancient oases are obviously regular. The different distances of the ancient oases going into the deserts are based on the different amount of fiver runoff and they have significant positive correlation. Their relationship is positive related. In the south of Tarim basin, each 1 x l0s m3 fiver runoff can push the ancient oasis going forward to desert 20.726 km averagely according the regressive model. The capacity and the area of glacier have the similar relationship with the distance and scales of the ancient oasis in desert. The high elevation mountain provides good condition for glacier exist- ence and development. The greater the capacity of glacier, the

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期刊信息
  • 《干旱区地理》
  • 北大核心期刊(2011版)
  • 主管单位:中国科学院出版委
  • 主办单位:中国科学院新疆生态与地理研究所 新疆地理学会
  • 主编:陈曦
  • 地址:乌鲁木齐北京南路818号
  • 邮编:830011
  • 邮箱:aridlg@ms.xjb.ac.cn
  • 电话:0991-7885506
  • 国际标准刊号:ISSN:1000-6060
  • 国内统一刊号:ISSN:65-1103/X
  • 邮发代号:58-45
  • 获奖情况:
  • 1994-1996、1997-1999年度科技期刊质量评比优秀期...,1999-2000年度科技期刊质量评比优秀期刊二等奖
  • 国内外数据库收录:
  • 英国农业与生物科学研究中心文摘,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版),中国北大核心期刊(2000版)
  • 被引量:18207