黄河宁蒙河段二次冲淤成因及近期变化  

Reasons and Recent Changes of Secondary Scour and Silting of the Channel in Ningxia-Inner Mongolia Reach of the Yellow River

作　　者：颜明[1] 王随继[1] 闫云霞[1] 许炯心[1] 师长兴[1] 贺莉[1] 

机构地区：[1]中国科学院地理科学与资源研究所,北京100101

出　　处：《人民黄河》2015年第4期46-49,54,共5页Yellow River

基　　金：国家"973"计划项目(2011CB403305);国家自然科学基金资助项目(41371037)

摘　　要：基于宁蒙河段的水沙和河道断面资料,分析了该河段主要水文站年内的冲淤过程、规律和近期变化情况。结果表明:1宁蒙河段河道在年内经历两次冲淤平衡,一次是冬季的冲淤平衡,一次是春、夏、秋季的冲淤平衡,后者水量较为丰沛且对河道冲淤起主要作用;2宁蒙河段淤积主要发生在内蒙古河段,石嘴山和头道拐水文站的断面冲淤变化不大,其余水文站断面均发生了明显淤积;3近期河道淤积的主要原因是径流量较少和大流量洪峰日数显著减少。Based on the detailed data on runoff,sediment and cross-section,process,pattern and recent changes of scour and silting within the reach of Ningxia-Inner Mongolia had been analyzed. The result indicates that 1)Ningxia-Inner Mongolia reach has twice balances of erosion and deposition,one occurs in winter and another one is in spring-summer-autumn respectively. The latter one has more runoff,so it is vital effect on balance of reach;2)the deposition mainly occurs in the Inner Mongolia section. River sections almost kept balance in scour and siltation at Shizuishan and Toudaoguai hydrometric stations. The others have significant deposition;3)recent siltation of channel is mainly due to significantly reduction of volume of runoff and number of days of flood peaks.

关 键 词：水沙过程 冲淤平衡 二次冲淤 宁蒙河段 黄河 

分 类 号：P333[天文地球—水文科学] TV882.1[水利工程—水文学及水资源]