关于南洞地下河系统南边界问题的讨论
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摘要
岩溶水系统的划分研究是水均衡分析、水资源评价的基础。南洞地下河是中国南方4个超大型地下河系统之一,其水文地质条件复杂,开发潜力巨大。由于南洞地下河系统蒙自盆地内有第三系阻水深槽存在,使得该区地下水位高于南北两侧,部分研究认为该阻水带是南洞地下河系统的南边界。本次通过进一步收集盆地内部和外围水文地质钻孔及地热钻孔资料、野外调查、洞穴探测及示踪试验,认为盆地内阻水深槽并不阻挡深部地下水,南洞地下河系统南边界应南移至南部地表分水岭一带。蒙自盆地及南部地下水流向应整体由南向北。
The study on the division of karst water system is the basis of water balance analysis and water resource evaluation.The Nandong underground river is one of the 4 super large underground river systems in southern China. Its hydrogeological conditions are complex and its exploitation potential are also tremendous. Due to the existence of deep grooves in Tertiary in the Mengzi basin of the Nandong underground river system, the groundwater level in this area is higher than that of the north and south sides, and some studies suggest that the water resistance zone is the southern boundary of the Nandong underground river.Through the further collection of hydrogeological and geothermal drilling data inside and outside of the basin, field investigation,cave detection and tracing test, this paper found that the deep grooves do not block deep groundwater, and the southern boundary of Nandong underground river system should be moved to the southern surface watershed area.The groundwater flow in the Mengzi basin and the South should be from south to north as a whole.
The study on the division of karst water system is the basis of water balance analysis and water resource evaluation.The Nandong underground river is one of the 4 super large underground river systems in southern China. Its hydrogeological conditions are complex and its exploitation potential are also tremendous. Due to the existence of deep grooves in Tertiary in the Mengzi basin of the Nandong underground river system, the groundwater level in this area is higher than that of the north and south sides, and some studies suggest that the water resistance zone is the southern boundary of the Nandong underground river.Through the further collection of hydrogeological and geothermal drilling data inside and outside of the basin, field investigation,cave detection and tracing test, this paper found that the deep grooves do not block deep groundwater, and the southern boundary of Nandong underground river system should be moved to the southern surface watershed area.The groundwater flow in the Mengzi basin and the South should be from south to north as a whole.
引文
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[7]段乔文,周翠琼,李焱.云南开远南洞暗河系统生态环境地质管理保护区划分[J].地质灾害与环境保护,2004,15(2):57-62.(DUAN Qiaowen, ZHOU Cuiqiong, LI Yan. Divide ecologic environment geologic administer protected area of Nandong underground river system,Yunnan Kaiyuan[J]. Journal of Geological Hazards and Environment Preservation, 2004,15(2):57-62.(in Chinese))
[8]夏日元,莫源富,唐健生.云南蒙自盆地岩溶石漠化动态演变特征研究[A].中国岩溶地下水与石漠化研究[C].中国地质调查局.南宁:广西科学技术出版社,2003:20-25.(XIA Riyuan, MO Yuanfu, TANG Jiansheng. Study on the dynamic evolution characteristics of Karst rocky desertification in Mengzi basin, Yunnan[A]. Study on Karst Groundwater and Rocky Desertification in China[C]. China Geological Survey. Nanning:Guangxi Science and Technology Press,2003:20-25.(in Chinese))
[9]王宇,张贵.滇东岩溶石山地区石淇化特征及成因[J].地球科学进展,2003,18(6):933-938.(WANG Yu, ZHANG Gui. On the desertification and genesis of karststone mountain area in east Yunnan[J]. Advance in Earth Sciences, 2003,18(6):933-938.(in Chinese))
[10]康彦仁,王挺,梁彬,等.云南南洞地下河系统的形成演化及水资源开发研究[R].地质矿产部岩溶地质研究所,1991.(KANG Yanren,WANG Ting, LIANG Bin, et al. Study on formation and evolution of Nandong underground river system and development of water resources in Yunnan province[R]. Institute of Karat Geology,Ministry of Geology and Mineral Resources, 1991.(in Chinese))
[11]张贵,周翠琼,康晓波.云南开远南洞地下河水质演变特征[J].中国岩溶,2008,27(4):366-370.(ZHANG Gui, ZHOU Cuiqiong,KANG Xiaobo.Changing features of water quality in the Nandong underground river, Kaiyuan, Yunnan[J]. Carsologica Sinica, 2008,27(4):366-370.(in Chinese))
[12]覃星铭,蒋忠诚,何丙辉,等.南洞流域东部重点区的石漠化现状及治理对策分析[J].中国岩溶,2014,33(4):456-463.(QIN Xingming, JIANG Zhongcheng, HE Binghui, et al. Current status and treatment of rocky desertification in key eastern areas of the Nandong subterranean river system[J]. Carsologica Sinca,2014,33(4):456-463.(in Chinese))
[13]覃星铭,蒋忠诚,蓝芙宁,等.南洞地下河最枯径流的周期变化及趋势分析[J].广西师范大学学报(自然科学版),2015,(2):120-126.(QIN Xingming, JIANG Zhongcheng, LAN Funing, et al.Analysis of trend and annual lowest runoff periodic variation in the Nandong subterranean river system[J]. Journal of Guangxi Normal University(Natural Science Edition), 2015(2):120-126.(in Chinese))
[14]赵一,李衍青,覃星铭,等.南洞地下河岩溶管道展布及结构特征的示踪试验解析[J].中国岩溶,2017,36(2):226-233.(ZHAO Yi, LI Yuqing, QIN Xingming, et al. Tracer tests on distribution and structural characteristics of karst channels in Nandong underground river drainage[J]. Carsologica Sinica, 2017,36(2):226-233.(in Chinese))
[15]张人权,周宏,陈植华,等.山西郭庄泉岩溶水系统分析[J].地球科学, 1991,16(1):1-17.(ZHANG enquan,ZHOU Hong,CHEN Zhihua,et al.The systematic analysis of Guozhuang spring karstwater system in Shanxi[J]. Earth Science:Journal of China University of Geosciences, 1991,16(1):1-17.(in Chinese))
[16]陈植华.岩溶水系统泉流量系统分析——以山西郭庄泉为例[J].地球科学,1991,16(1):51-60.(CHEN Zhihua.The systematic analysis of spring discharge of karst groudwater system[J]. Earth Science, 1991,16(1):51-60.(in Chinese))
[17]劳文科,蓝芙宁,蒋忠诚,等.石期河流域岩溶水系统及其水资源构成分析[J].中国岩溶,2009,28(3):255-262.(LAO Wenke, LAN Funing, JIANG Zhongcheng, et al. Analysis on karst groundwater system and its water resources composition in Shiqihe basin[J].Carsologica Sinica, 2009,28(3):255-262.(in Chinese))
[18]党学亚,张茂省.晋西南峨嵋台塬的岩溶水系统及岩溶水资源潜力[J].水文地质工程地质,2007,32(4):70-73.(DANG Xueya,ZHANG Maosheng. Karst water system and water resources potential in the Emei loess platform in southwestern Shanxi[J]. Hydrogeology&Engineering Geology, 2007,32(4):70-73.(in Chinese))
[19]罗明明,肖天昀,陈植华,等.香溪河岩溶流域几种岩溶水系统的地质结构特征[J].水文地质工程地质,2014,41(6):13-19.(LUO Mingming, XIAO Tianyun, CHEN Zhihua, et al. Geological structure characteristics of several karst water systems in the Xiangxi River karst basin[J]. Hydrogeology&Engineering Geology, 2014,41(6):13-19.(in Chinese))
[2]张人权,梁杏,靳孟贵,等.水文地质学基础[M].北京:地质出版社,2011.(ZHANG Renquan, LIANG Xing, JIN Menggui, et al.Fundamentals of Hydrogeology[M]. Beijing:Geological Publishing House, 2011.(in Chinese))
[3]卢耀如,张凤娥,刘长礼,等.中国典型地区岩溶水资源及其生态水文特征[J].地球学报,2006,27(5):393-402.(LU Yaoru, ZHANG Fenge,LIU Changli, et al. Karst water resources in typical areas of China and their ecohydrological characteristics[J]. Acta Geoscienticasinica, 2006,27(5):393-402.(in Chinese))
[4]康彦仁,梁彬.云南南洞地下河系统的水文地质特征[J].水文地质工程地质,1996,(4):28-30.(KANG Yanren, LIANG Bin. Hydrogeological characteristics of the subterranean river system in the south cave of Yunnan[J]. Hydrogeology&Engineering Geology,1996,(4):28-30.(in Chinese))
[5]马祖陆.云南南洞地下河流域地貌特征及地下河发育演化的初步研究[J].中国岩溶,1993,(3):273-283.(MA Zulu. A preliminary study on the geomorphic features of the subterranean river basin and the development and evolution of the Nandong underground river in Yunnan[J]. Carsologiga Sinca, 1993,(3):273-283.(in Chinese))
[6]高明刚.云南南洞岩溶地下水温度场时空变化规律研究[J].中国岩溶,1995,(1):19-30.(GAO Ming gang.Study on the temporal and spatial variation of karst groundwater temperature field in Nandong of Yunnan[J].Carsologica Sinica, 1995,(1):19-30.(in Chinese))
[7]段乔文,周翠琼,李焱.云南开远南洞暗河系统生态环境地质管理保护区划分[J].地质灾害与环境保护,2004,15(2):57-62.(DUAN Qiaowen, ZHOU Cuiqiong, LI Yan. Divide ecologic environment geologic administer protected area of Nandong underground river system,Yunnan Kaiyuan[J]. Journal of Geological Hazards and Environment Preservation, 2004,15(2):57-62.(in Chinese))
[8]夏日元,莫源富,唐健生.云南蒙自盆地岩溶石漠化动态演变特征研究[A].中国岩溶地下水与石漠化研究[C].中国地质调查局.南宁:广西科学技术出版社,2003:20-25.(XIA Riyuan, MO Yuanfu, TANG Jiansheng. Study on the dynamic evolution characteristics of Karst rocky desertification in Mengzi basin, Yunnan[A]. Study on Karst Groundwater and Rocky Desertification in China[C]. China Geological Survey. Nanning:Guangxi Science and Technology Press,2003:20-25.(in Chinese))
[9]王宇,张贵.滇东岩溶石山地区石淇化特征及成因[J].地球科学进展,2003,18(6):933-938.(WANG Yu, ZHANG Gui. On the desertification and genesis of karststone mountain area in east Yunnan[J]. Advance in Earth Sciences, 2003,18(6):933-938.(in Chinese))
[10]康彦仁,王挺,梁彬,等.云南南洞地下河系统的形成演化及水资源开发研究[R].地质矿产部岩溶地质研究所,1991.(KANG Yanren,WANG Ting, LIANG Bin, et al. Study on formation and evolution of Nandong underground river system and development of water resources in Yunnan province[R]. Institute of Karat Geology,Ministry of Geology and Mineral Resources, 1991.(in Chinese))
[11]张贵,周翠琼,康晓波.云南开远南洞地下河水质演变特征[J].中国岩溶,2008,27(4):366-370.(ZHANG Gui, ZHOU Cuiqiong,KANG Xiaobo.Changing features of water quality in the Nandong underground river, Kaiyuan, Yunnan[J]. Carsologica Sinica, 2008,27(4):366-370.(in Chinese))
[12]覃星铭,蒋忠诚,何丙辉,等.南洞流域东部重点区的石漠化现状及治理对策分析[J].中国岩溶,2014,33(4):456-463.(QIN Xingming, JIANG Zhongcheng, HE Binghui, et al. Current status and treatment of rocky desertification in key eastern areas of the Nandong subterranean river system[J]. Carsologica Sinca,2014,33(4):456-463.(in Chinese))
[13]覃星铭,蒋忠诚,蓝芙宁,等.南洞地下河最枯径流的周期变化及趋势分析[J].广西师范大学学报(自然科学版),2015,(2):120-126.(QIN Xingming, JIANG Zhongcheng, LAN Funing, et al.Analysis of trend and annual lowest runoff periodic variation in the Nandong subterranean river system[J]. Journal of Guangxi Normal University(Natural Science Edition), 2015(2):120-126.(in Chinese))
[14]赵一,李衍青,覃星铭,等.南洞地下河岩溶管道展布及结构特征的示踪试验解析[J].中国岩溶,2017,36(2):226-233.(ZHAO Yi, LI Yuqing, QIN Xingming, et al. Tracer tests on distribution and structural characteristics of karst channels in Nandong underground river drainage[J]. Carsologica Sinica, 2017,36(2):226-233.(in Chinese))
[15]张人权,周宏,陈植华,等.山西郭庄泉岩溶水系统分析[J].地球科学, 1991,16(1):1-17.(ZHANG enquan,ZHOU Hong,CHEN Zhihua,et al.The systematic analysis of Guozhuang spring karstwater system in Shanxi[J]. Earth Science:Journal of China University of Geosciences, 1991,16(1):1-17.(in Chinese))
[16]陈植华.岩溶水系统泉流量系统分析——以山西郭庄泉为例[J].地球科学,1991,16(1):51-60.(CHEN Zhihua.The systematic analysis of spring discharge of karst groudwater system[J]. Earth Science, 1991,16(1):51-60.(in Chinese))
[17]劳文科,蓝芙宁,蒋忠诚,等.石期河流域岩溶水系统及其水资源构成分析[J].中国岩溶,2009,28(3):255-262.(LAO Wenke, LAN Funing, JIANG Zhongcheng, et al. Analysis on karst groundwater system and its water resources composition in Shiqihe basin[J].Carsologica Sinica, 2009,28(3):255-262.(in Chinese))
[18]党学亚,张茂省.晋西南峨嵋台塬的岩溶水系统及岩溶水资源潜力[J].水文地质工程地质,2007,32(4):70-73.(DANG Xueya,ZHANG Maosheng. Karst water system and water resources potential in the Emei loess platform in southwestern Shanxi[J]. Hydrogeology&Engineering Geology, 2007,32(4):70-73.(in Chinese))
[19]罗明明,肖天昀,陈植华,等.香溪河岩溶流域几种岩溶水系统的地质结构特征[J].水文地质工程地质,2014,41(6):13-19.(LUO Mingming, XIAO Tianyun, CHEN Zhihua, et al. Geological structure characteristics of several karst water systems in the Xiangxi River karst basin[J]. Hydrogeology&Engineering Geology, 2014,41(6):13-19.(in Chinese))
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