作者：侯甬坚;

机构：陕西师范大学西北历史环境与经济社会发展研究中心暨中国历史地理研究所;

中文关键词：西昆仑山;;尼雅河;;尼雅遗址

英文关键词：West Kunlun Mountains;Niya River;Niya Settlements;Niya Site

中文摘要：西昆仑山脉出山径流尼雅河,系依赖上游源区冰川融化及山区降雨才得以形成。进入平川区、尾闾地区后,在塔克拉玛干沙漠气象条件及其下垫面作用下,尼雅河水渐渐消失。一百年来的尼雅遗址考察、考古及历史研究成果丰硕,尼雅从聚落到废墟的演变过程,反映了尼雅河来水等水源逐渐匮乏的事实,魏晋后尼雅行政建置丧失于交通价值的下降,喀帕克阿斯干村以北居民点,则最后废弃于彻底无水接济。

英文摘要：Niya River, a runoff from West Kunlun Mountains, is formed by glacial meltwater from the upper reaches of Niya River and rainfall in West Kunlun Mountains. It gradually dried up after entering plain and tail areas, caused by dry climate of the Taklimakan Desert. Over the last 100 years, great successes were achieved in archaeological and historical research on Niya site. The change from settlements to ruins in Niya indicates the fact of water sources scarcity of Niya River. After the Wei and Jin dynasties, due to the decrease of its transportation importance, the administration organization in Niya was abandoned. The settlement to the north of the Kapak-askan village was abandoned because of the scarcity of water sources too.

[中文刊名]：西域研究 [出版日期]：2009-01-15 [CN]：65-1121/C [ISSN]：1002-4743

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