J4 ›› 2009, Vol. 39 ›› Issue (5): 863-867.

• 地质工程与环境工程 • 上一篇    下一篇

基岩三维流数学模型求解的广义差分法及应用

马瑞杰1| 赵宇琦2| |张静1| 黄平3   

  1. 1.吉林大学 数学学院|长春 130012;2.长春市水利局|长春 130022;3.吉林大学 环境与资源学院,长春 130026
  • 收稿日期:2009-03-12 出版日期:2009-09-26 发布日期:2009-09-26
  • 通讯作者: 马瑞杰(1965-),女,吉林长春人,副教授,博士,主要从 事应用数学研究 E-mail:marj@jlu.edu.cn
  • 作者简介:马瑞杰(1965-)|女|吉林长春人|副教授|博士|主要从 事应用数学研究|E-mail:marj@jlu.edu.cn
  • 基金资助:

    “十一·五”国家科技支撑计划项目(2006BAB04A09-02,2007BAB28B04-03)

Generalized Finite Difference Method and Its Application of Bedrock Waterflow |Three-Dimensional Mathematical Model Solving

MA Rui-jie1, ZHAO Yu-qi2,ZHANG Jing1,HUANG Ping3   

  1. 1.College of Math, Jilin University, Changchun 130012,China;2.Changchun |Water Conservancy Bureau, Changchun 130022,China;3.College of Environment and Resources, Jilin University, Changchun 130026, China
  • Received:2009-03-12 Online:2009-09-26 Published:2009-09-26

摘要:

白垩系基岩孔隙裂隙承压含水层为研究区地下水主要含水层之一,水文地质模型概化为各项异性非均质。根据地下水系统运动规律及分布特征建立三维非稳定流数学模型,采用广义差分法对其求解,并以长春市区为例对模型进行识别验证。结果表明,计算模型与实际水文地质条件比较接近,计算水位与实测水位相吻合;为研究区地下水系统可持续管理提供了科学理论依据。

关键词: 基岩, 孔隙裂隙, 广义差分法, 计算水位, 实测水位

Abstract:

Confined pore and fissure aquifer in Cretaceous bedrock is one of the main aquifers in Changchun area and the hydrogeological conceptural model can be simplified as anisotropy and heterogeneity. According to the movement’s feature of groundwater system, the mathematic model of three-dimensional transient flow is assumed and generalized difference method is used to solve the flow equations and the groundwater flow model has been calibrated and verified. The model simulation result is in accordance to the actual hydrogeologic condition and the caculated water table is consistent to the monitored water table. The results can provide a scientific theoretical foundation for sustainable management of groundwater resources in the study area.

Key words: bedrock, pore and fissue, generalized difference, caculated water table, measured water table

中图分类号: 

  • P641.1
[1] 李鹏, 苏生瑞, 马驰, 黄璜, 徐继维. 堆积层-基岩接触面滑坡的形成机理——以祖师庙滑坡为例[J]. 吉林大学学报(地球科学版), 2017, 47(5): 1471-1479.
[2] 巨银娟, 张小莉, 张永庶, 陈琰. 柴达木盆地昆北地区基岩储层裂缝特征[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1660-1671.
[3] 曾玉超, 苏正, 吴能友, 王晓星, 胡剑. 漳州地热田基岩裂隙水系统温度分布特征[J]. J4, 2012, 42(3): 814-820.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!