高级搜索

滇东北毛坪铅锌矿区水化学特征及成因

,  ,  ,  ,  ,  ,  , 

downloadPDF

上一篇

下一篇

王剑, 罗朝晖, 陈植华, 王涛, 黄荷, 项彩娟, 孙帮涛, 王勇. 滇东北毛坪铅锌矿区水化学特征及成因[J]. 环境化学, 2018, 37(6): 1421-1431. doi: 10.7524/j.issn.0254-6108.2017083102
引用本文: 王剑, 罗朝晖, 陈植华, 王涛, 黄荷, 项彩娟, 孙帮涛, 王勇. 滇东北毛坪铅锌矿区水化学特征及成因[J]. 环境化学, 2018, 37(6): 1421-1431. doi: 10.7524/j.issn.0254-6108.2017083102
shu
WANG Jian, LUO Zhaohui, CHEN Zhihua, WANG Tao, HUANG He, XIANG Caijuan, SUN Bangtao, WANG Yong. Characteristics and controlling factors of water chemistry in maoping lead-zinc mine area, Northeastern Yunnan, China[J]. Environmental Chemistry, 2018, 37(6): 1421-1431. doi: 10.7524/j.issn.0254-6108.2017083102
Citation: WANG Jian, LUO Zhaohui, CHEN Zhihua, WANG Tao, HUANG He, XIANG Caijuan, SUN Bangtao, WANG Yong. Characteristics and controlling factors of water chemistry in maoping lead-zinc mine area, Northeastern Yunnan, China[J]. Environmental Chemistry, 2018, 37(6): 1421-1431. doi: 10.7524/j.issn.0254-6108.2017083102
shu

滇东北毛坪铅锌矿区水化学特征及成因

  • 1.

    中国地质大学(武汉)环境学院, 武汉, 430074;

  • 2.

    彝良驰宏矿业有限公司, 彝良, 657600

Characteristics and controlling factors of water chemistry in maoping lead-zinc mine area, Northeastern Yunnan, China

  • 1.

    School of Environmental Studies, China University of Geosciences, Wuhan, 430074, China;

  • 2.

    Yi Liang Chihong Mining Co., Ltd, Yiliang, 657600, China

  • 摘要: 地下水水化学是研究矿区复杂水文地质与水-岩作用过程的重要手段.本文采用水文地球化学与环境同位素研究相结合的方法，系统探讨了滇东北毛坪矿区地下水水化学特征及成因.结果表明研究区不同含水系统之间的水化学分布特征差异显著，指示了其不同的来源或经历了不同的水文地球化学作用过程.针对水化学特征的因子分析表明，该区水化学主要受地下水径流途径、碳酸盐岩的水岩作用、硫化物矿物的氧化溶解及农业活动等因素控制.本研究对探究西南地区复杂岩溶金属矿区地下水组分的来源及形成机制具有重要参考意义.
    Abstract: Groundwater chemistry is an important and efficient tool to study the water-rock interaction and the complex hydrogeological conditions in mining areas. Hydrogeochemical and isotopic studies were conducted to understand the generation mechanism of groundwater chemistry of Maoping lead-zinc miming area. The groundwater from different aquifer system has totally different characteristics of water chemistry indicating these groundwaters has different recharge source or/and has experienced different water-rock interaction processes. The results of factor analysis suggest that groundwater flow pathway, water-rock interaction of carbonate rock, oxidation of sulfide minerals and agriculture activity are the dominated factors controlling the chemistry of groundwater. This study will significantly improve the understand the generation mechanism of groundwater chemistry in Karst polymetallic sulfides mining area, Southwestern China.
  • 加载中
  • [1] 卢丽, 王喆, 裴建国, 等. 红水河中上游流域岩溶地下水水质影响因素的R型因子分析[J]. 中国岩溶, 2015,34(4):415-419.

    LI L, WANG Z, PEI J G, et al. R-type factor analysis of influencing factors of karst groundwater quality in middle and upper reaches of Hongsui River[J]. Carsologica Sinica, 201534(4):415-419(in Chinese).

    [2] 杨平恒, 袁道先, 叶许春, 等. 降雨期间岩溶地下水化学组分的来源及运移路径[J]. 科学通报, 2013,58(18):1755-1763.

    YANG P H, YUAN D X, YE XC, et al. Source and migration path of karst groundwater chemical components during rainfall[J]. Chinese Science Bulletin, 2013, 58(18):1755-1763(in Chinese).

    [3] 曹新元, 吕古贤, 朱裕生. 我国主要金属矿产资源及区域分布特点[J]. 资源·产业, 2004,6(4):22-24.

    CAO X Y, LV G X, ZHU Y S. Measurement of main metal mineral resources and regional distribution in China[J]. Resources & Industries, 2004, 6(4):22-24(in Chinese).

    [4] 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 Y M, CHEN Z H, YU K B. Geogeneity of groundwater in south karst metal mine area and its significance in controlling water:A case study of Maokeng iron mine in Fujian[J]. Earth Science, 2016, 41(4):692-700(in Chinese).

    [5] 侯昭华, 徐海, 安芷生. 青海湖流域水化学主离子特征及控制因素初探[J]. 地球与环境, 2009,37(1):11-19.

    HOU Z H, XU H, AN Z S. Study on main ion characteristics and controlling factors of water chemistry in Qinghai Lake Basin[J].Journal of Earth and Environment, 2009, 37(1):11-19(in Chinese).

    [6] 胡云虎. 皖北地下水源地水环境地球化学特征研究[D]. 淮南:安徽理工大学, 2015.

    Hu Y H. Study on water environment geochemical characteristics of groundwater source in northern Anhui[D]. Huainan:Anhui University of Science &Technology (in Chinese).

    [7] 王亚平, 王岚, 许春雪, 等. 长江水系水文地球化学特征及主要离子的化学成因[J]. 地质通报, 2010, 29(Z1):446-456.

    WANG Y P, WANG L, XU C X, et al. Characteristics of hydroge and geochemistry of the Yangtze River and the chemical origin of the main ions[J]. Geological Bulletin of China, 2010, 29(Z1):446-456(in Chinese).

    [8] LI J, YUAN G, DENG X, et al. Major ion geochemistry of the Nansihu Lake basin rivers, North China:chemical weathering and anthropogenic load under intensive industrialization[J]. Environmental Earth Sciences, 2016,75(6):453.
    [9] 沈照理, 王焰新. 水_岩相互作用研究的回顾与展望[J]. 地球科学:中国地质大学学报, 2002,27(2):127-133.

    Shen Z L, Wang Y X. Retrospect and prospect fresh water rock interaction[J]. Earth Science:China University of Geosciences, 2002, 27(2):127-133(in Chinese).

    [10] 袁建飞, 邓国仕, 徐芬, 等. 毕节市北部岩溶地下水水化学特征及影响因素的多元统计分析[J]. 中国地质, 2016,43(4):1446-1456.

    YUAN J F, DENG G S, XU F, et al. Such as water chemistry of karst groundwater in the northern city of Bijie and influencing factors of multivariate statistical analysis[J]. Geology in China, 2016, 43(4):1446-1456(in Chinese).

    [11] ZHANG X, LI X, GAO X. Hydrochemistry and coal mining activity induced karst water quality degradation in the Niangziguan karst water system, China[J]. Environmental Science and Pollution Research, 2016, 23(7):6286-6299.
    [12] 代俊鸽, 郭纯青, 裴建国, 等. 基于SPSS岩溶地下水水化学特征的多元统计分析——以红水河刁江流域为例[J]. 工业安全与环保, 2015,41(4):81-83.

    DAI J G, GUO C Q, PEI J G, et al. Multi-statistical analysis of hydrochemical characteristics of groundwater based on SPSS-A case study of Diaojiang River Basin in Hongshui River[J]. Industrial Safety and Environmental Protection, 2015,41(4):81-83(in Chinese).

    [13] 林永生, 裴建国, 杜毓超, 等. 基于多元统计方法的岩溶地下水化学特征及影响因素分析[J]. 环境化学, 2016, 35(11):2394-2401.

    LIN Y S, Pei J G, DU Y C, et al. Analysis of chemical characteristics and influencing factors of karst groundwater based on multivariate statistical method[J]. Environmental Chemistry, 2016,35(11):2394-2401(in Chinese).

    [14] 刘大金, 陈华北. 某铅锌矿床深部承压水来源及通道浅析[J]. 现代矿业, 2017,33(2):89-91.

    LIU D J, CHEN H N. Evaluation and channel analysis of deep confined water in a lead-zinc deposit[J]. Express Information of Mining Industry, 2017, 33(2):89-91(in Chinese).

    [15] 肖可. 金佛山地区地下水与地表水水文地球化学及氢氧同位素特征分析[D]. 重庆:西南大学, 2015. XIAO K G hydro-geochemical and hydrogen and oxygen isotopic characteristics of groundwater and surface water in Jinfo Mountain area[D]. Chongqing:Southwest University, 2015(in Chinese).
    [16] 黄华诚. 昆明市黑龙潭岩溶泉水氢氧稳定同位素特征分析[D]. 昆明:云南大学, 2015. HUANG L C. Analysis of hydrogen and oxygen stable isotope characteristics of karst spring in Heilongtan, Kunming[D]. Kunming:Yunnan University, 2015(in Chinese).
    [17] 许琦, 李建鸿, 孙平安, 等. 西江水氢氧同位素组成的空间变化及环境意义[J]. 环境科学, 2017,38(6):2308-2316.

    XU Q, L J H, SUN P G, et al. Spatial variation of hydrogen and oxygen isotopes in the Xijiang River and its environmental significance[J].Chinese Journal of Environmental Science, 2017, 38(6):2308-2316(in Chinese).

    [18] 陆徐荣, 周爱国, 王茂亭, 等. Piper图解淮河流域江苏地区浅层地下水水质演化特征[J]. 工程勘察, 2010,38(2):42-47.

    XU R L, ZHOU A G, WANG M T, et al. Illustrating evolution of other Piper shallow groundwater quality Jiangsu Huaihe River region[J]. Geotechnical Investigation & Surveying, 2010, 38(2):42-47(in Chinese).

    [19]
    [20] 吴月. 巴丹吉林沙漠地下水同位素特征与地下水年龄研究[D]. 兰州:兰州大学, 2014. WU Y. Study on Isotopic characteristics of groundwater and groundwater age in Badain Jaran Desert[D]. Lanzhou:Lanzhou University, 2014(in Chinese).
    [21]
    [22] 宋献方, 李发东, 于静洁, 等. 基于氢氧同位素与水化学的潮白河流域地下水水循环特征[J]. 地理研究, 2007, 26(1):11-21.

    SONG X F, Li F D, Yu J J, et al. Characteristics of groundwater cycle in the Chaobai River Basin based on hydrogen and oxygen isotope and water chemistry[J]. Geographical Research, 2007, 26(1):11-21(in Chinese).

    [23] 刘彦广. 基于水化学和同位素的高寒山区雨季径流过程示踪[D]. 武汉:中国地质大学, 2013. LIU Y G.Study on runoff process of rainy season in alpine mountain based on water chemistry and isotope[D]. Wuhan:China University of Geosciences, 2013(in Chinese).
    [24] 吴春勇, 苏小四, 郭金淼, 等. 鄂尔多斯沙漠高原白垩系地下水水化学演化的多元统计分析[J]. 世界地质, 2011, 30(2):244-253.

    WU C Y, SU X S, GUO J M, et al. Multi-statistical analysis of cortical groundwater hydrochemical evolution in ordos desert plateau[J]. Global Geology, 2011,30(2):244-253(in Chinese).

    [25] 沈照理, 朱宛华. 水文地球化学基础[M]. 北京:地质出版社, 1999. SHEN Z L, ZHU W H. Hydrological and geochemical basis[M]. Beijing:Geological Publishing House, 1999(in Chinese).
    [26] 张慧颖. 会泽铅锌矿区水文地质条件及地下水环境质量评价[D].昆明:昆明理工大学, 2002. ZHANG H Y. Hydelite Lead-Zinc Mining Area hydrogeological conditions and groundwater environmental quality evaluation[D]. Kunming, Kunming University of Science and Technology, 2002(in Chinese).
    [27] 马燕华, 苏春利, 刘伟江, 等. 水化学和环境同位素在示踪枣庄市南部地下水硫酸盐污染源中的应用[J]. 环境科学, 2016,37(12):4690-4699.

    MA Y H, SU C L, LIU W J, et al. Application of water chemistry and environmental isotope in tracing sulphate pollution source in southern Zaozhuang city[J]. Environmental Science, 2016,37(12):4690-4699(in Chinese).

    [28] 李小彦, 崔永君, 杜新锋, 等. 一种值得关注的高效洁净煤资源——云南昭通小法路矿无烟煤性能研究[J]. 中国煤田地质, 2003,15(1):16-17.

    LI X Y, CUI Y J, DU X F, et al. Study on the performance of anthracite in Zhaotong Xiaofa Road, Yunnan Province[J]. Coal Geology of China, 2003,15(1):16-17(in Chinese).

    [29]
    [30] 乔军伟, 张光超. 火山活动对彝良向斜煤矿区成煤环境的影响[J]. 中国煤炭地质, 2012,24(3):1-4.

    QIU J W, ZHANG G C. Effects of volcanic activity on the coal-forming environment in the Yiliang oblique mining area[J]. Coal Geology of China, 2012, 24(3):1-4(in Chinese).

    [31] 张光超, 乔军伟, 李聪聪. 云南省昭通地区宣威组C_5煤层硫分分布特征[J]. 中国煤炭地质, 2012, 24(4):14-17.

    ZHANG G C, QIAO J W, LI C C. Characteristics of sulfur distribution in C_5 coal seam of Xuanwei Formation in Zhaotong area, Yunnan Province[J]. Coal Geology of China, 2012,24(4):14-17(in Chinese).

    [32]
    [33] EVANS C D, REYNOLDS B, CURTIS C J, et al. A conceptual model of spatially heterogeneous nitrogen leaching from a welsh moorland catchment[J]. Water, Air, & Soil Pollution:Focus, 2005,4(6):97-105.
  • 加载中
WeChat 点击查看大图
计量
  • 文章访问数:  1247
  • HTML全文浏览数:  1219
  • PDF下载数:  196
  • 施引文献:  0
出版历程
  • 收稿日期:  2017-08-31
  • 刊出日期:  2018-06-15
王剑, 罗朝晖, 陈植华, 王涛, 黄荷, 项彩娟, 孙帮涛, 王勇. 滇东北毛坪铅锌矿区水化学特征及成因[J]. 环境化学, 2018, 37(6): 1421-1431. doi: 10.7524/j.issn.0254-6108.2017083102
引用本文: 王剑, 罗朝晖, 陈植华, 王涛, 黄荷, 项彩娟, 孙帮涛, 王勇. 滇东北毛坪铅锌矿区水化学特征及成因[J]. 环境化学, 2018, 37(6): 1421-1431. doi: 10.7524/j.issn.0254-6108.2017083102
shu
WANG Jian, LUO Zhaohui, CHEN Zhihua, WANG Tao, HUANG He, XIANG Caijuan, SUN Bangtao, WANG Yong. Characteristics and controlling factors of water chemistry in maoping lead-zinc mine area, Northeastern Yunnan, China[J]. Environmental Chemistry, 2018, 37(6): 1421-1431. doi: 10.7524/j.issn.0254-6108.2017083102
Citation: WANG Jian, LUO Zhaohui, CHEN Zhihua, WANG Tao, HUANG He, XIANG Caijuan, SUN Bangtao, WANG Yong. Characteristics and controlling factors of water chemistry in maoping lead-zinc mine area, Northeastern Yunnan, China[J]. Environmental Chemistry, 2018, 37(6): 1421-1431. doi: 10.7524/j.issn.0254-6108.2017083102
shu

滇东北毛坪铅锌矿区水化学特征及成因

  • 1.  中国地质大学(武汉)环境学院, 武汉, 430074;
  • 2.  彝良驰宏矿业有限公司, 彝良, 657600
  • 收稿日期:  2017-08-31

摘要: 地下水水化学是研究矿区复杂水文地质与水-岩作用过程的重要手段.本文采用水文地球化学与环境同位素研究相结合的方法，系统探讨了滇东北毛坪矿区地下水水化学特征及成因.结果表明研究区不同含水系统之间的水化学分布特征差异显著，指示了其不同的来源或经历了不同的水文地球化学作用过程.针对水化学特征的因子分析表明，该区水化学主要受地下水径流途径、碳酸盐岩的水岩作用、硫化物矿物的氧化溶解及农业活动等因素控制.本研究对探究西南地区复杂岩溶金属矿区地下水组分的来源及形成机制具有重要参考意义.

English Abstract

    全文HTML

参考文献 (33)

返回顶部

目录

/

返回文章
返回

Copyright © 2019 中国科学院生态环境研究中心