天山北麓低山丘陵地区春季融雪洪水的研究——以三工河古河道为例  

STUDY ON THE SPRING FLOODS CAUSED BY SNOW MELT WATER IN LOW-MOUNTAIN AND HILL REGIONS OF NORTHERN PIEDMONT OF THE TIANSHAN MOUNTAINS—A Case Study in the Paleochannels of Sangong River

作　　者：王志杰[1] 迪里木拉提[1] 李从林[2] 

机构地区：[1]新疆水文水资源局,乌鲁木齐830000 [2]新疆水文水资源局三工河地下水环境监测试验站,阜康831505

出　　处：《干旱区地理》2002年第4期302-308,共7页Arid Land Geography

摘　　要：通过对天山北麓低的丘陵地区春季融雪洪水的成因的分析 ,利用数理统计方法 ,以三工河流域为代表区域 ,分析出制约三工河古河春季融雪洪水量的 5个重要因素后 ,进而探讨天山北麓低山、丘陵地区春季融雪洪水产流成因机理 。The northern piedmont of the Tianshan Mountains and the southern marginal zone of Junggar Basin are the regions with the most developed economy in Xinjiang. However, the frequent occurrence of spring floods caused by snowmelt water threatens directly the safety of the communications and traffic facilities, reservoirs, irrigation canals, water conservancy and hydropower works, and even people's life and property in north Xinjiang. Starting from the formation causes, this paper analyzes the 5 main factors resulting in the spring floods caused by snowmelt water in the Sangong River watershed. The 5 main factors include the precipitation during the stable snow cover period, precipitation within 25 days before the stable snow cover day, precipitation within 25～85 days before the stable snow cover day, the three day accumulated temperature before the stable snow cover day, and the change of the winter negative accumulated temperature related to the vegetation conditions in the watershed and the climate warming. Among which the winter negative accumulated temperature changes the area and the intensity of the impervious and poor pervious strata, cuts off and reduce the pathways of permeation of snow melt water. The purposes of the study are to research the mechanism of the formation causes of spring floods caused by snow melt water in the low mountain and hill regions of northern piedmont of the Tianshan Mountains and to develop the prediction models.

关 键 词：春季 天山 低山丘陵地区 融雪洪水 成因机理 下垫面 入渗强度 

分 类 号：TV122[水利工程—水文学及水资源]