| 注册
首页|期刊导航|干旱区地理|内蒙古十大孔兑流域地貌演化格局及其成因机制

内蒙古十大孔兑流域地貌演化格局及其成因机制

顾畛逵 师长兴 阳辉 刘晓菲

干旱区地理2017,Vol.40Issue(6):1188-1197,10.
干旱区地理2017,Vol.40Issue(6):1188-1197,10.

内蒙古十大孔兑流域地貌演化格局及其成因机制

Landform evolution pattern of the ten Kongdui basins and its genetic mechanisms in Inner Mongolia of China

顾畛逵 1师长兴 2阳辉 1刘晓菲2

作者信息

  • 1. 中国科学院地理科学与资源研究所,陆地水循环及地表过程重点实验室,北京100101
  • 2. 中国科学院大学,北京100049
  • 折叠

摘要

Abstract

Geomorphic evolution is an important part of geomorphology.According to some indices including longitudinal section gradient,area-altitude curve,entropy of erosion basin (H (S)),entropy of longitudinal profile (H (N)) and others,this paper studies the evolution of the main channel and basins of the Inner Mongolia based on a 30-m resolution DEM.Firstly,the index values and simulated their spatial variation trends were calculated by Grey model (GM (1,1)),then this paper discussed the formation mechanism of watershed landscape pattern associated with the tectonic activities,lithology characters and the climatic evolution.The results show that the ten Kongdui (seasonal river) basins are mostly in the mature stage of landform evolution except Hantaichuan basin (R5) and Haoqinghe basin (R6) being in the youth and old stages respectively,it means that there will be a high potential of sediment yield for a long time in the future.Sediment carried by the Kong dui is mainly consist of the coarse sands coming from Mesozoic loose sandstone (named as "Pisha"in Chinese) area in its upstream and desert sands coming from Kubuqi Desert.The erosion intensity of the west Kongdui basins is higher than that of the east and the main reason is that the uplift of the ground is higher than that of the west side,while the influence of climatic factors is less relatively.In contrast,as a result of the lower tectonic uplift and probably is also related to the slightly more rainfall and lithologic properties in the east basins,the evolution of longitudinal profiles of the main channel of the east area is characterized by a higher degree than the west.The formation of the existing landscape pattern of low in the east and high in the west might mainly occur in the Quaternary,and the landform evolution rate probably altered with climate change at the same time.

关键词

十大孔兑/地貌演化/GM(1,1)模型/构造活动/岩性/气候效应

Key words

geomorphic evolution/the ten Kongdui basins/GM (1,1)/tectonic activity/lithologic property/climate change

分类

天文与地球科学

引用本文复制引用

顾畛逵,师长兴,阳辉,刘晓菲..内蒙古十大孔兑流域地貌演化格局及其成因机制[J].干旱区地理,2017,40(6):1188-1197,10.

基金项目

国家自然科学基金面上项目(41371036) (41371036)

干旱区地理

OA北大核心CSCDCSTPCD

1000-6060

访问量0
|
下载量0
段落导航相关论文