摘要
冰沟流域的降水对地面径流、表层径流和地下径流的补给比例,在春季时分别为0.45,0.55和0,夏秋季分别为0.08,0.65和0.28。用线性水库模式模拟冰沟流域的表层径流时,其储蓄系数春季为8,夏秋季为11。这是因为冻土活动层随季节的变化对径流各分量的影响所致。
The runoff forming principle and its estimation in cold region is one of the major contents on hydrology of cold region. This paper deals with, taking Binggou Basin of the Qilian Mountain as the object of study, the characteristic and regularity of the runoff forming under the condition of the cold regions, especially the effects of the variations of frozen soil upon the runoff forming. The result shows that frozen soil changes with season is one of the main factors affecting runoff forming. In the Binggou Basin, the thawed depth of frozen soil is shallow in spring. The proportions of surface runoff and subsurface that supply stream runoff during this time are about 0.45 and 0.55 respectively. As a result of thawed depth increasing after spring, 0.08, 0.65 and 0.28 of the stream runoff are supplied by surface, subsurface and groundwater runoff separately. In addition, when simulating the daily discharge of the subsurface and groundwater runoff with a linear reservoir model the storage constant K is variable with season. The K for subsurface runoff is equal to 8 in spring and then rises to 11 after spring. In contrast, the K for groundwater runoff is 60 and the variation is smaller in summer and autumn.
出处
《冰川冻土》
CSCD
北大核心
1992年第3期251-257,共7页
Journal of Glaciology and Geocryology
基金
国家自然科学基金课题
关键词
冰沟
冻土
活动层
径流
参数变化
Binggou, active layer of frozen soil, runoff, variation of parameter
