水文地质工程地质2001，Vol.28Issue(2)：18-20,3.
山西柳林泉域地下水流数值模拟
吴吉春 1薛禹群 1黄海 1张政治 2王玉海2
作者信息
- 1. 南京大学地球科学系,
- 2. 山西省电力勘测设计院,
- 折叠
摘要
Abstract
Liulin spring is fracture-karst spring, with the area of about 2727km2 . There is a large area of brackish and salt water in the fracture-karst aquifer along the west, northwest of Liulin spring. In this situation, a regional two-dimensional groundwater flow mathematical model is presented. This model is applied to describe the transport of groundwater of Liulin spring area. The simulated values agree very well with the field data. In the calibration step and examination step, the average absolute errors between the simulated and the observed values for the hydraulic head are 0.46m and 0.51m, respectively. Good comparison between these values demonstrates that the model can be applied to solving practical problems. Thus, the model is used to detect the effect on the regional distribution of hydraulic level and the effect on the flow rate of Linlin spring when the spring is used to as a water supply center for the Liulin power plant.关键词
裂隙-岩溶/地下水流/数值模拟分类
天文与地球科学引用本文复制引用
吴吉春,薛禹群,黄海,张政治,王玉海..山西柳林泉域地下水流数值模拟[J].水文地质工程地质,2001,28(2):18-20,3.
