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Volume 43 Issue 6
Dec.  2024
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Article Navigation >  CARSOLOGICA SINICA  > 2024  >  43(6): 1223-1234
WANG Yu. Study on complexity of groundwater systems in the karst mining areas with abundant water on the Yunnan plateau[J]. CARSOLOGICA SINICA, 2024, 43(6): 1223-1234. doi: 10.11932/karst20240601
Citation: WANG Yu. Study on complexity of groundwater systems in the karst mining areas with abundant water on the Yunnan plateau[J]. CARSOLOGICA SINICA, 2024, 43(6): 1223-1234. doi: 10.11932/karst20240601
shu

Study on complexity of groundwater systems in the karst mining areas with abundant water on the Yunnan plateau

doi: 10.11932/karst20240601
  • 1.

    Key Laboratory of Geohazard Forecast and Geoecological Restoration in Plateau Mountainous Area, MNR, Kunming, Yunnan 650216, China

  • 2.

    Yunnan Key Laboratory of Geohazard Forecast and Geoecological Restoration in Plateau Mountainous Area, Kunming, Yunnan 650216, China

  • 3.

    Yunnan Geological Survey, Kunming, Yunnan 650051, China

  • Received Date: 2023-12-02
  • Accepted Date: 2024-07-02
  • Rev Recd Date: 2024-06-13
    • Available Online: 2025-03-21
    Abstract
  • A mining area with abundant water usually refers to the mine with a pit water inflow greater than 10,000 m3·d−1. In view of the unevenness of the water-richness of karst aquifers and the poor accuracy of predicting water inflow, the definition of a mining area with abundant water should not be confined to the specific values of water inflow. Instead, it should be defined mainly based on the conditions of high water-richness, abundant recharge and pipeline flow of aquifers. According to the standard of hydrogeological terminology, a hydrogeological unit is defined as a groundwater system characterized by uniform recharge boundaries and conditions of recharge, runoff, and discharge. The groundwater systems described in this paper belong to the same object and category. The Yunnan plateau refers to the western section of the Yunnan-Guizhou Plateau, and, in a broad sense, encompasses Yunnan Province, which covers an area of 39.4×104 km2. The karst contiguous areas on the Yunnan plateau are mainly located in the east area of 102°E and north of the Yuanjiang river in eastern Yunnan, and the northwest and the west from Baoshan to Cangyuan. These karst contiguous areas total 11.09×104 km2, corresponding to the upper Yangtze massif, South China massif, Sanjiang orogenic belt and Tengchong orogenic belt, with superior mineralization conditions and abundant mineral resources. Historically, minerals in karst areas are primarily exploited above the erosion base. The mountainous terrain typically facilitates natural drainage, which has led to a lack of emphasis on and research into the complexity of groundwater systems in mining areas. With the growing economic and social demands, the exploration areas and mining areas are continually expanded, and are increasingly extending to deeper areas. Some deposits with abundant water that were previously challenging in exploitation have been developed. This shift has transformed hydrogeological conditions, evolving from simple to complex or even extremely complex scenarios. As a result, the challenges associated with mine water control have intensified, and the requirements for exploration have correspondingly increased. Therefore, it is both necessary and urgent to study the complexity of groundwater systems in karst mining areas with abundant water, enhance the research level, and strengthen measures for exploration control.The complexity of a system encompasses the characteristics such as disorder, sudden change, detection errors, and inference errors, which arise from the pluralism, nonlinearity, and randomness of its constituent elements, organizational structures, influencing factors, and their interrelations and interactions with the environment. Based on existing research and exploration findings, the complexity of groundwater systems in karst mining areas with abundant water is mainly reflected in the intricate and variable characteristics of system boundary conditions, hydrogeological structures, properties of water-bearing media, and the effects of mining activities.In karst areas, the geological processes of mineralization and subsequent transformation are highly intense, and the geological conditions are exceedingly complex, no matter whether the deposits are endogenous, exogenous, or metamorphic. The complexity of boundary conditions of groundwater systems in karst mining areas with abundant water is mainly manifested in the irregularity of topographic watersheds, the multistage nature of erosion datum, the diversity and invisibility of genesis–tectonic types of geological boundary, and the variability of boundary hydrodynamic properties. The complexity of groundwater system structure is mainly manifested in the diversity and variability of karst aquifers, non-soluble rock aquifers (bodies), primary and secondary structural properties and their mutual relationship. The complexity of the properties of water-bearing media is mainly manifested in karst aquifers, which are not only strongly developed but also exhibit significant variability. This variability includes the direction, scale, density, and connectivity of karst caves, conduits and fissures. The characteristics of water richness, permeability, and hydraulic connections also display prominent anisotropy. The influence of mining engineering and mining activities on groundwater systems in mining areas is huge and far-reaching. In addition, the design of mine shafts, mining pits, and development engineering often requires real-time adjustments in response to changes in ore bodies and mining technical conditions during the mining process. The disturbances and impacts of mining engineering and activities on the water environment and groundwater systems are also difficult to predict accurately. These influences have increased the complexity of groundwater systems in mining areas to varying degrees.This paper systematically examines the complexity of groundwater systems in karst mining areas with abundant water. It provides a detail analysis of typical examples, along with a visual representation of the distinctive characteristics of these systems. This paper discusses the complexity of groundwater systems in mining areas with abundant water. It addresses the challenges encountered in hydrogeological exploration within mining areas. The discussion focuses on optimizing and adjusting the evaluation indices for the complexity of hydrogeological conditions as outlined in current specifications. Furthermore, it emphasizes the need for quantifying evaluation standards and establishing a reasonable assessment scale for the exploration control of complex hydrogeological conditions in mining areas. Besides, the paper offers recommendations for revising and improving the existing specifications.

     

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    • References(41)
  • [1]
    GB/T12719-2021. 矿区水文地质工程地质勘查规范[S].

    GB/T12719-2021. Exploration specification of hydrogeology and engineering geology in mining areas[S].
    [2]
    AQ2061-2018. 金属非金属地下矿山防治水安全技术规范[S].

    AQ2061-2018. Safety technical specifications for water prevention and control in metal and nonmetal underground mines[S].
    [3]
    DZ/T0342-2020. 矿坑涌水量预测计算规程[S].

    DZ/T0342-2020. Specification for water yield estimation of mine[S].
    [4]
    GB/T14157-93. 水文地质术语[S].

    GB/T14157-93. Hydrogeologic terminology[S].
    [5]
    王宇. 岩溶区地表水与地下水资源及环境统一评价的流域边界划分研究[J]. 中国岩溶, 2019, 38(6):823-830. doi: 10.11932/karst2019y08

    WANG Yu. Study on watershed boundary division for unified evaluation of surface water and groundwater resources and environment in karst areas[J]. Carsologica Sinica, 2019, 38(6): 823-830. doi: 10.11932/karst2019y08
    [6]
    王宇. 岩溶高原地下水径流系统垂向分带[J]. 中国岩溶, 2018, 37(1):1-8. doi: 10.11932/karst20180101

    WANG Yu. Vertical zoning of groundwater runoff system in karst plateau[J]. Carsologica Sinica, 2018, 37(1): 1-8. doi: 10.11932/karst20180101
    [7]
    王宇. 西南岩溶地区岩溶水系统分类、特征及勘查评价要点[J]. 中国岩溶, 2002, 21(2):114-119. doi: 10.3969/j.issn.1001-4810.2002.02.008

    WANG Yu. Classification, features of karst water system and key point for the evaluation to karst water exploration in Southwest China karst area[J]. Carsologica Sinica, 2002, 21(2): 114-119. doi: 10.3969/j.issn.1001-4810.2002.02.008
    [8]
    施玉北, 卢映祥, 李文昌, 程胜辉, 王宇, 等. 中国矿产地质志·云南卷[R]. 昆明:云南省地质调查局, 2021.
    [9]
    王宇, 侯曙光, 曾文涛, 等. 云南省矿山地质环境调查成果报告[R]. 昆明:云南省地质调查局, 2018.
    [10]
    王宇, 张贵、柴金龙, 等. 云南岩溶石山地区重大环境地质问题及对策[M]. 昆明:云南科技出版社, 2013.

    WANG Yu, ZHANG Gui, CHAI Jinlong, et al. The serious environmental geological problems and countermeasures in karst area of Yunnan Province[M]. Kunming: Yunnan Science and Technology Press, 2013.
    [11]
    王宇, 张贵, 张华, 等. 云南省岩溶水文地质环境地质调查与研究[M]. 北京:地质出版社, 2018.
    [12]
    李金秀. 滇东北毛坪铅锌矿区深部开采条件下矿坑水防治研究[D]. 昆明:昆明理工大学, 2016:10-60.
    [13]
    张亮. 毛坪铅锌矿岩溶地下水系统及结构辨识研究[D]. 武汉:中国地质大学, 2021:10-40.

    ZHANG Liang. Study on karst groundwater system and structure identification in Maoping lead-zinc mine, Southwest China[D]. Wuhan: China University of Geosciences, 2021: 10-40.
    [14]
    项彩娟, 陈植华, 王涛, 黄荷, 孙帮涛, 王勇. 基于小波分析的滇东北毛坪铅锌矿充水水源识别[J]. 地质科技情报, 2019, 38(6):231-240.

    XIANG Caijuan, CHEN Zhihua, WANG Tao, HUANG He, SUN Bangtao, WANG Yong. Recognition of water source of Maoping lead zinc mine in northeast Yunnan based on wavelet analysis[J]. Geological Science and Technology Information, 2019, 38(6): 231-240.
    [15]
    宋煜. 云南会泽铅锌矿区深部岩溶水特征及矿井涌水预测[D]. 昆明:昆明理工大学, 2016:6-50.

    SONG Yu. Lead-zinc mine deep karst water features and the mine water gushing prediction in Huize, Yunnan[D]. Kunming: Kunming University of Science and Technology, 2016: 6-50.
    [16]
    陈彦美, 陈植华, 於开炳. 南方岩溶金属矿区地下水非均质性及防治水意义:以福建马坑铁矿为例[J]. 地球科学, 2016, 41(4):692-700.

    CHEN Yanmei, CHEN Zhihua, YU Kaibing. Heterogeneity and water prevention of karst water system in metal mine areas in Southern China: A case study of Makeng iron mine, Fujian Province[J]. Earth Science, 2016, 41(4): 692-700.
    [17]
    朱远峰, 崔光中, 庞景细. 北山矿区岩溶系统的划分及岩溶发育期的厘定[J]. 中国岩溶, 1991, 10(4):327-334.

    ZHU Yuanfeng, CUI Guangzhong, PANG Jingxi. Karst system in Beishan mine district and its stages of karstification[J]. Carsologica Sinica, 1991, 10(4): 327-334.
    [18]
    李贵仁, 赵珍, 陈植华. 复杂岩溶矿区疏干条件下的地下水数值模拟:以福建省马坑铁矿为例[J]. 中国岩溶, 2012, 31(4):382-387.

    LI Guiren, ZHAO Zhen, CHEN Zhihua. Numerical simulation for groundwater under draining condition in complex karst mining area: An example from the Makeng iron mine in Fujian Province[J]. Carsologica Sinica, 2012, 31(4): 382-387.
    [19]
    宋学锋. 复杂性、复杂系统与复杂性科学[J]. 中国科学基金, 2003, 17(5):262-269. doi: 10.3969/j.issn.1000-8217.2003.05.002

    SONG Xuefeng. Complexity, complex systems and the science of complexity[J]. Bulletin of National Natural Science Foundation of China, 2003, 17(5): 262-269. doi: 10.3969/j.issn.1000-8217.2003.05.002
    [20]
    范智伟. 复杂系统的时空结构与动力学研究[D]. 杭州:浙江大学, 2022:10-30.

    FAN Zhiwei. Study on spatiotemporal structure and dynamics of complex systems[D]. Hangzhou: Zhejiang University, 2022: 10-30.
    [21]
    魏一鸣. 自然灾害复杂性研究[J]. 地理科学, 1998, 18(1):25-31.

    WEI Yiming. A research on the complexity of natural disasters[J]. Scientia Geographica Sinica, 1998, 18(1): 25-31.
    [22]
    宋长青, 程昌秀, 史培军. 新时代地理复杂性的内涵[J]. 地理学报, 2018, 73(7):1204-1213. doi: 10.11821/dlxb201807002

    SONG Changqing, CHENG Changxiu, SHI Peijun. Geography complexity: New connotations of geography in the new era[J]. Acta Geographica Sinica, 2018, 73(7): 1204-1213. doi: 10.11821/dlxb201807002
    [23]
    袁道先. 论岩溶环境系统[J]. 中国岩溶, 1988, 7(3):179-186.

    YUAN Daoxian. On the karst environmental system[J]. Carsologica Sinica, 1988, 7(3): 179-186.
    [24]
    彭必建, 李四堂. 个旧矿区水文地质现状及地下水保护与利用[J]. 云南地质, 2014, 33(4):594-600. doi: 10.3969/j.issn.1004-1885.2014.04.025

    PENG Bijian, LI Sitang. The present hydrogeology and protection, utilization of underground water in Guijiu orefield[J]. Yunnan Geology, 2014, 33(4): 594-600. doi: 10.3969/j.issn.1004-1885.2014.04.025
    [25]
    崔灿文. 云南西邑铅锌矿复杂岩溶充水矿床涌水量预测[D]. 昆明:昆明理工大学, 2018:42-113.

    CUI Canwen. Prediction of water inflow of complex karst water-filled deposit in Xiyi lead-zinc mine, Yunnan[D]. Kunming: Kunming University of Science and Technology, 2018: 42-113.
    [26]
    赵雪琼, 程先锋, 李广涛, 王明伟, 齐武福. 滇西某铅锌矿床矿坑涌水量预测与分析[J]. 地下水, 2011, 33(6):15-17, 67.
    [27]
    何智, 杨苏焕. 云南保山市金厂矿区矿坑充水因素浅析[J]. 云南地质, 2016, 35(2):292-295.

    HE Zhi, YANG Suhuan. A preliminary analysis of water filling factor in pit of Jinchang orefield in Baoshan, Yunnan Province[J]. Yunnan Geology, 2016, 35(2): 292-295.
    [28]
    陈思颖, 张颖. 滇西红牛铜矿区巷道水文地质特征浅析[J]. 云南地质, 2021, 40(4):484-489. doi: 10.3969/j.issn.1004-1885.2021.04.016

    CHEN Siying, ZHANG Ying. A preliminary analysis on hydrogeological feature in tunnel of Hongniu Cu orefield in W Yunnan[J]. Yunnan Geology, 2021, 40(4): 484-489. doi: 10.3969/j.issn.1004-1885.2021.04.016
    [29]
    台宁宁. 云南建水县挣财洞铅锌矿区岩溶发育特征及1800m中段涌水量预测[D]. 昆明:昆明理工大学, 2020:27-88.
    [30]
    段乔文, 吴继明, 冷吉诚. 滇东南高原岩溶盆地区普阳煤矿的深层涌水趋势分析[J]. 中国岩溶, 2021, 40(2):189-197.

    DUAN Qiaowen, WU Jiming, LENG Jicheng. Trend of water inrush at depth in the Puyang coal mine, karst basin area, southeastern Yunnan plateau[J]. Carsologica Sinica, 2021, 40(2): 189-197.
    [31]
    王宇, 康晓波, 张华, 王燕. 昆明地热田的成因与外延[J]. 中国岩溶, 2016, 35(2):125-133.

    WANG Yu, KANG Xiaobo, ZHANG Hua, WANG Yan. The genesis and extension of Kunming geothermal field[J]. Carsologica Sinica, 2016, 35(2): 125-133.
    [32]
    李灿辉, 董绍华, 邹绍丹, 徐兴业. 云南香格里拉市热林铅锌矿水文地质条件分析[J]. 云南地质, 2020, 39(1):98-102.

    LI Canhui, DONG Shaohua, ZOU Shaodan, XU Xingye. An analysis of the hydrogeological conditions in Relin Pb-Zn deposit of Xianggelila[J]. Yunnan Geology, 2020, 39(1): 98-102.
    [33]
    虞慧, 莫美仙, 庞君, 杨光亮. 云南省威信县李子埂煤矿突水与龙洞坝泉断流原因分析[J]. 矿业安全与环保, 2014, 41(1):102-105. doi: 10.3969/j.issn.1008-4495.2014.01.031

    YU Hui, MO Meixian, PANG Jun, YANG Guangliang. Cause analysis on water inrush in Lizigeng coal mine and Longdongba spring cut-off in Weixin county of Yunnan Province[J]. Mining Safety and Environmental Protection, 2014, 41(1): 102-105. doi: 10.3969/j.issn.1008-4495.2014.01.031
    [34]
    和祥, 董学兰, 杨超, 刘鹏, 薛博强. 云南鹤庆县北衙金矿岩溶发育及富水特征[J]. 中国岩溶, 2023, 42(6):1173-1182. doi: 10.11932/karst2023y025

    HE Xiang, DONG Xuelan, YANG Chao, LIU Peng, XUE Boqiang. Characteristics of karst development and water abundance of the Beiya gold deposit in Heqing county of Yunnan[J]. Carsologica Sinica, 2023, 42(6): 1173-1182. doi: 10.11932/karst2023y025
    [35]
    董书宁, 虎维岳. 中国煤矿水害基本特征及其主要影响因素[J]. 煤田地质与勘探, 2007, 35(5):34-37. doi: 10.3969/j.issn.1001-1986.2007.05.009

    DONG Shuning, HU Weiyue. Basic characteristics and main controlling factors of coal mine water hazard in China[J]. Coal Geology and Exploration, 2007, 35(5): 34-37. doi: 10.3969/j.issn.1001-1986.2007.05.009
    [36]
    虎维岳, 田干. 我国煤矿水害类型及其防治对策[J]. 煤炭科学技术, 2010, 38(1):92-96.

    HU Weiyue, TIAN Gan. Mine water disaster type and prevention and control countermeasures in China[J]. Coal Science and Technology, 2010, 38(1): 92-96.
    [37]
    缪钟灵. 岩溶矿区突水水文地质探讨[J]. 化工矿山技术, 1979(3):21-26, 14.
    [38]
    袁道先. 论岩溶水的不均匀性[C]//岩溶地区水文地质及工程地质工作经验汇编(第二辑). 北京:地质出版社, 1978:1-19.
    [39]
    任美锷, 刘振中, 王飞燕, 等. 岩溶学概论[M]. 北京:商务印书馆, 1983.
    [40]
    罗明明, 尹德超, 张亮, 陈植华, 周宏, 韩兆丰, 史婷婷. 南方岩溶含水系统结构识别方法初探[J]. 中国岩溶, 2015, 34(6):543-550. doi: 10.11932/karst20150602

    LUO Mingming, YIN Dechao, ZHANG Liang, CHEN Zhihua, ZHOU Hong, HAN Zhaofeng, SHI Tingting. Identifying methods of karst aquifer system structure in South China[J]. Carsologica Sinica, 2015, 34(6): 543-550. doi: 10.11932/karst20150602
    [41]
    王宇. 南方岩溶地区水文地质调查的问题与改进措施[J]. 中国岩溶, 2023, 42(4):627-635. doi: 10.11932/karst20230401

    WANG Yu. Problems and their countermeasures in a hydrogeological survey of karst areas in South China[J]. Carsologica Sinica, 2023, 42(4): 627-635. doi: 10.11932/karst20230401
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