吉林大学学报(地球科学版) ›› 2022, Vol. 52 ›› Issue (3): 955-966.doi: 10.13278/j.cnki.jjuese.20200258

• 地质工程与环境工程 • 上一篇    下一篇

基于GMS的长春齐家地下水水源地二级保护区划分

鲍新华1, 于瀚博1, 计量2   

  1. 1.吉林大学新能源与环境学院,长春130021

    2.中国电力工程顾问集团东北电力设计院有限公司,长春130021


  • 出版日期:2022-05-26 发布日期:2024-01-05
  • 基金资助:

    国家自然科学基金项目(41202166)


Division of Two-Level Protection Area of Changchun Qijia Groundwater Source Based on GMS

Bao Xinhua1, Yu Hanbo1, Ji Liang2   

  1. 1. College of New Energy and Environment, Jilin University, Changchun 130021, China

    2. Northeast Electric Power Design Institute Co., Ltd., China Electric Power Engineering Consulting Group, Changchun 130021, China


  • Online:2022-05-26 Published:2024-01-05
  • Supported by:
    Supported by the National Natural Science Foundation of China (41202166)

摘要:

长春市双阳齐家水源地临近油田,原有的水源地一级保护区不足以调和油田开采与水源地水质安全之间日益突出的矛盾。为了保护地下水饮用水水源地不受油田开发活动的影响,为饮用水水源地所在地区的油田开发布局提出规划建议,首先查明研究区内水文地质条件,然后在原有的一级水源地保护区基础上利用数值法软件GMS(groundwater model system)中的MODFLOW和MT3DMS模块对水源地建立地下水流模型和溶质运移模型,并以此对长春市双阳齐家水源地进行二级保护区划分研究,明确油田开发活动对地下水环境和水源地可能产生的污染程度和范围。模拟结果表明,污染物在地下水中运移1 000 d时距离污染源400~800 m,以此为据共划定二级保护区33.5 km2,并将原规划在划定的二级保护区内和边缘的油井给出取消建设或适当迁建的建议。

关键词: 长春齐家水源地, 地下水流模拟, 溶质运移模拟, 保护区划分, GMS

Abstract:

Shuangyang Qijia water source in Changchun City is close to the oil field, and the original division of one-level water source protection zone is not enough to reconcile the increasingly prominent contradiction between oilfield exploitation and water quality safety of water sources. In order to protect the groundwater drinking water source from the influence of oilfield development activities, a new division is needed to help the oilfield development layout in the area where the drinking water source is located. Firstly, the hydrogeological conditions in the study area were analyzed, the groundwater flow models and solute transport models of the water sources were established by using the MODFLOW and MT3DMS modules in the numerical software GMS (groundwater model system) on the basis of the original primary water source protection area. Then the secondary protected area division study was carried out in Shuangyang Qijia water source area in Changchun City to determine the degree and scope of pollution caused by the oilfield development activities. The simulation results show that after 1 000 d transportation in groundwater, the pollutants are 400-800 m away from the pollution source. On this basis, a total of 33.5 km2 of the secondary protected area is designated, and the oil wells originally planned in and around the designated area should be cancelled or properly relocated.


Key words: Qijia water source in Changchun, groundwater flow simulation, solute transport simulation, division protection area, groundwater model system

中图分类号: 

  • P641
[1] 骆祖江, 曾峰, 郭华, 吴刚. 地下饮用水水源保护区划分三维渗流与溶质运移耦合数值模型[J]. J4, 2010, 40(6): 1353-1358.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 尤敏鑫,刘建民. 同位素地球化学在峨眉山大火成岩省研究中的应用现状与进展[J]. 吉林大学学报(地球科学版), 2014, 44(4): 1231 -1243 .
[2] 杨春梅, 李洪奇,陆大卫,张方礼,高 原,邵英超. 不同驱替方式下岩石电阻率与饱和度的关系[J]. J4, 2005, 35(05): 667 -671 .
[3] 祝洪臣,张炯飞,权 恒. 大兴安岭中生代两期成岩成矿作用的元素、同位素特征及其形成环境[J]. J4, 2005, 35(04): 436 -0442 .
[4] 朱建伟, 赵刚, 刘博, 郭巍, 成俊. 油页岩测井识别技术及应用[J]. J4, 2012, 42(2): 289 -295 .
[5] 陈力,梁海安,张文娟,荣帆. 模糊数学方法在城市工程地质环境区划中的应用--以抚顺市城区为例[J]. J4, 2008, 38(5): 837 -0840 .
[6] 高桂梅,苏 克,王文颖,甘树才,刘招君. 吉林省桦甸油页岩中稀土元素和微量元素的研究[J]. J4, 2006, 36(6): 974 -0979 .
[7] 吴孔运,蒋忠诚,叶 晔. 不同植物群落对灰岩试块溶蚀速率的影响[J]. J4, 2007, 37(5): 967 -0971 .
[8] 周彦章,迟宝明,刘中培. 山东夏甸金矿床充水机理构造控制模式[J]. J4, 2008, 38(2): 255 -0260 .
[9] 张渊,刘连登,孙景贵,陈国华,张洪喜,闫复传,杨开春. 胶东西北部黄埠岭金矿床两期次叠加成矿[J]. J4, 2008, 38(1): 21 -0026 .
[10] 鲁程鹏, 束龙仓, 苑利波, 张蓉蓉, 黄币娟, 王彬彬. 基于示踪试验求解岩溶含水层水文地质参数[J]. J4, 2009, 39(4): 717 -721 .