img

官方微信

高级检索

中国沙漠 ›› 2000, Vol. 20 ›› Issue (3): 238-242.

• 论文 • 上一篇    下一篇

10世纪末西辽河流域沙漠化的突进及其原因

王守春   

  1. 中国科学院 地理科学和资源研究所, 北京 100101
  • 收稿日期:2000-02-03 修回日期:2000-04-24 出版日期:2000-09-20 发布日期:2000-09-20
  • 作者简介:王守春(1940-),男(汉族),辽宁省大连人,研究员,主要从事历史地理研究。
  • 基金资助:
    国家自然科学基金(49831080)

Fastly Development and Causes of Desertification in West Liao River Basin of Inner Mongolia during the Later 10 Century

WANG Shou-chun   

  1. Institute of Geographical Science and Resource, Chinese Academy of Sciences, Beijing 100101, China
  • Received:2000-02-03 Revised:2000-04-24 Online:2000-09-20 Published:2000-09-20

摘要: 西辽河流域在辽代早期和辽代之前,是自然环境较好的"辽泽",其自然景观为面积广大的平沙地,其上生长乔木、灌木和草本,为疏林草原,还有较大面积的下湿地和较多湖泊,没有出现流动沙丘。在11世纪期间的文献中,记载了西辽河流域有明显的沙漠化表现。10世纪末西辽河流域环境可能出现突变,是历史时期西辽河流域沙漠化的开始时间。沙漠化的原因,主要为自然原因,即气候变化。

关键词: 西辽河流域, 辽代, 沙漠化, 环境变迁

Abstract: The main part of the plain formed by west Liao river in the east of Inner Mongolia Autonomous Region is occupied by the famous Korqin desert today.But Qi Dan nation rose and established very strong Liao Dynasty in the west Liao river basin and controlled almost the north of China during 10 Century,thus left a lot of historical writings(historical books and travels) and ruins.These historical materials contain a lot of information on natural environment.The historical records and environmental archeology showed that the environment of west Liao river basin was fairly advantageous,and the landscape of this basin was plat sand land covered by grass and sparse woods such as some species of elms,willow and apricot,and there were vast marshland grasslands and many lakes before 1000 A.D..And this superior environment provided favorable condition for rising of Qi Dan nation.These historical records also showed that the environment of west Liao river basin was some worsening at the beginning of 11 Century.Sand dunes were recorded on different part of the basin by several travelers and historical books.The changes of environment and desertification were shown more clearly.The desertification appeared at the end of 10 Century according to these historical records,and the cause of desertification was that the cold north-west wind from Mongolia plateau was strengthened and climate tended to dry.The role of human activities on desertification was the second and locally in the middle ages,but this role was incorrectly emphasized by some researchers as the first position in the early desertification process of Korqin desert,in fact human activities in desertification of Korqin desert have played a important role mainly in recent 300 a.

Key words: west Liao river basin, Liao Dynasty, desertification, environmental changes

中图分类号: