Advanced Search
  • Included in CSCD
  • Chinese Core Journals
  • Included in WJCI Report
  • Included in Scopus, CA, DOAJ, EBSCO, JST
  • The Key Magazine of China Technology
Volume 38 Issue 4
Aug.  2019
Turn off MathJax
Article Contents
Article Navigation >  CARSOLOGICA SINICA  > 2019  >  38(4): 532-538
LIU Ruitong, WANG Jinguo, ZHOU Yun, HUANG Hua, CHEN Changsheng. Simulation of karst groundwater balance in the Westshan mountains, Heqing county, Yunnan Province[J]. CARSOLOGICA SINICA, 2019, 38(4): 532-538. doi: 10.11932/karst20190409
Citation: LIU Ruitong, WANG Jinguo, ZHOU Yun, HUANG Hua, CHEN Changsheng. Simulation of karst groundwater balance in the Westshan mountains, Heqing county, Yunnan Province[J]. CARSOLOGICA SINICA, 2019, 38(4): 532-538. doi: 10.11932/karst20190409
shu

Simulation of karst groundwater balance in the Westshan mountains, Heqing county, Yunnan Province

doi: 10.11932/karst20190409
  • 1.

    School of Earth Sciences and Engineering, Hohai University, Nanjing, Jiangsu 210098,China

  • 2.

    Three Gorges Geotechnical Consultants Co., Ltd., Wuhan, Hubei, 430074,China

  • Publish Date: 2019-08-25
    Abstract
  • The karst groundwater in the Westshan mountains of Heqing county is an important water resource for local residents. To carry out studies on groundwater balance, flow simulation and the karst groundwater dynamics is of great significance to improve management of the karst groundwater in this area. Based on available data, the physiography, lithology, structure, and hydrogeology of the area are analyzed and the karst groundwater system is demarcated. Numerical simulation is conducted, the result of which is compared with the conventional water balance method. The results show that the karst groundwater system in the study area can be reasonably divided into six sub-systems. The recharge and discharge of each karst subsystem are largely balanced, and the discharge is dominated by a concentrating manner, which accounts for 67%-92% of the total amount. The connectivity test confirms the existence of karst pipelines in the subsystem V, in which the difference between the simulated discharge and the measured spring discharge is minimal, indicating that the model considering the concentrated drainage is more suitable.

     

    • FullText(HTML)
  • loading
    • References(29)
  • [1]
    徐恒力. 水资源开发与保护［M］.北京:地质出版社, 2001.
    [2]
    李伯权. 地下水资源评价中有关概念的讨论［J］. 工程勘察, 2001(3):20-24.
    [3]
    李晓英, 顾文钰. 水均衡法在区域地下水资源量评价中的应用研究［J］. 水资源与水工程学报, 2014，25(1)：87-90.
    [4]
    张先, 周亮. 许昌麦岭水源地可开采量的水均衡法计算［J］. 水文地质工程地质, 2004, 31(2):83-87.
    [5]
    张江华, 陈国亮. 水均衡法预测岩溶区坑道涌水量的一些见解［J］. 中国岩溶, 1988,7(3):273.
    [6]
    高殿琪, 颜景生. 利用水均衡法求算明水岩溶区降水入渗系数［J］. 山东地质, 1991(2):107-113.
    [7]
    任增平, 李广贺, 于莉,等. 开采条件下多时段水量均衡法的应用研究［J］. 现代地质, 1998(3):425-430.
    [8]
    Moiwo J P , Tao F , Lu W . Estimating soil moisture storage change using quasi-terrestrial water balance method［J］. Agricultural Water Management, 2011, 102(1):25-34.
    [9]
    吴文强, 李文文, 刘君利. 水均衡与数值模拟法在地下水资源评价中对比应用［J］. 中国农村水利水电, 2009(6): 45-48.
    [10]
    汪洋, 李娟, 席北斗, 等. 基于数值模拟的岩溶地下水源保护区划分技术研究［J］. 中国岩溶, 2018, 37(6):799-809.
    [11]
    梁永平, 韩行瑞, 时坚,等. 鄂尔多斯盆地周边岩溶地下水系统模式及特点［J］. 地球学报, 2005, 26(4):365-369.
    [12]
    裴建国，梁茂珍，陈阵西南岩溶石山地区岩溶地下水系统划分及其主要特征值统计［J］. 中国岩溶, 2008, 27(1):6-10.
    [13]
    赵永贵，蔡祖煌. 岩溶地下水系统的研究：以太原地区为例［M］.北京:科学出版社，1990.
    [14]
    郭纯青, 时坚, 裴建国. 岩溶地下水系统中快速流与慢速流的模拟［J］. 中国岩溶, 1985,4(4):21-29.
    [15]
    罗利川, 梁杏, 李扬,等. 基于GMS的岩溶山区三维地下水流模式识别［J］. 中国岩溶, 2018, 37(5):44-53.
    [16]
    Xi L W . Approach on boundary condition in numerical simulation of groundwater flows［J］. Journal of Hydraulic Engineering, 2003, 34(3):33-36.
    [17]
    陈宏峰, 张发旺, 何愿, 等. 地质与地貌条件对岩溶系统的控制与指示［J］. 水文地质工程地质, 2016(5):42-47.
    [18]
    莫美仙,王 宇,李 峰,等. 云南南洞地下河系统边界及性质研究［J］. 中国岩溶, 2019,38(2): 173-185.
    [19]
    陈崇希. 岩溶管道-裂隙-孔隙三重空隙介质地下水流模型及模拟方法研究［J］. 地球科学, 1995(4):361-366.
    [20]
    田娟,董贵明,束龙仓.孔隙-管道型西南岩溶地下河系统参数与流量衰减系数关系的数值试验研究［J］.水文地质工程地质,2013,40(2):13-18.
    [21]
    赵坚, 赖苗, 沈振中. 适于岩溶地区渗流场计算的改进折算渗透系数法和变渗透系数法［J］. 岩石力学与工程学报, 2005, 24(8):1341-1347.
    [22]
    Ashraf A, Ahmad Z. Regional groundwater flow modelling of Upper Chaj Doab of Indus Basin, Pakistan using finite element model (Feflow) and geoinformatics［J］. Geophysical Journal of the Royal Astronomical Society, 2010, 173(1):17-24.
    [23]
    王景瑞, 胡立堂, 尹文杰. 甘肃北山地区三维地质建模方法对比研究［J］. 北京师范大学学报(自然科学版), 2014，50(5):478-482.
    [24]
    王刚. 酒泉盆地地下水系统数值模拟研究［D］. 兰州：兰州大学, 2007.
    [25]
    交通部第一铁路设计院. 铁路工程地质手册［M］. 北京：人民交通出版社, 1975.
    [26]
    齐登红. 降水入渗补给地下水系统分析［M］. 郑州：黄河水利出版社，2007.
    [27]
    Shi L S, Cai S Y, Yang J Z. Study on spatial variability of subrainfall infiltration coefficient and simulation of the stochastic field［J］. Journal of Hydraulic Engineering, 2007, 38(1):79-85.
    [28]
    Yi L, Shao M. Experimental study on influence factors of rainfall and infiltration under artificial grassland coverage［J］. Transactions of the Chinese Society of Agricultural Engineering, 2007, 23(3):18-23.
    [29]
    申豪勇, 梁永平, 唐春雷,等. 应用氯量平衡法估算娘子关泉域典型岩溶区的降水入渗系数［J］. 水文地质工程地质, 2018, 45(6):37-41.
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索
    Get Citation
    PDF(19624.0KB)
    XML

    Article Metrics

    Article views (2309) PDF downloads(478) Cited by()
    Proportional views
    Related

    Website Copyright © CARSOLOGICA SINICA 桂ICP备05009877号-1

    Sponsor: Chinese Academy of Geological Sciences Sponsored by: Institute of Karst Geology, Chinese Academy of Geological Sciences Address: No.50, Qixing Road, Guilin, Guangxi

    Post Code: 541004 Tel: 0773-5812949 7796657 Email: zgyr@mail.cgs.gov.cn; zgyrbjb@163.com

    Supported by: Beijing Renhe Information Technology Co., Ltd.    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return