乌蒙山区典型富水型背斜泉群成因机理研究——以绥江县新滩镇银厂村幸福泉为例
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摘要
乌蒙山区划跨云南、贵州、四川三省,是国家新一轮扶贫开发攻坚战主战场之一,五角堡背斜位于乌蒙山区中部,分布于绥江县五角堡至屏山县楼东一带,背斜周边共出露天然泉点45个,幸福泉位于五角堡背斜北西翼,距离核部2km,枯水季流量141L/s,丰水季流量822L/s,为新滩镇供水水源地。根据前人调查,此泉的成因机理研究主要有两种截然不同的理论,一种为"上升泉理论",一种为"下降泉理论",针对这两种理论,以现场调查、示踪试验及地球物理勘探为依据,对幸福泉成因机理进行深入分析并提出自己的观点,认为幸福泉为岩溶裂隙上升泉,为此后同类富水性背斜泉群的研究及该地区地下水资源的合理开发利用提供科学依据。
Wumeng Mountain stretch across Yunnan,Guizhou and Sichuan provinces.It is one of the battlegrounds for the new round of poverty alleviation in China.The Wujiaobao anticline is located in the middle of Wumeng Mountain,and distributed in the area from the Wujiaobao of Suijiang County to Loudong of Pingshan County.There are 45 natural.springs exposed in the periphery of the anticline.The Xingfu Spring is the water supply source of Xintan town that 2 km away from the core,which is located in the northwestern wing of the anticline of Wujiaobao,and the seasonal flow is 141 L/s and 822 L/s in the low water season and in the abundant water season respectively.According to the previous investigations,there are mainly.two different theories on the genesis mechanism of the spring,one is the theory of "rising springs" and the other is the theory of "falling springs".According to the above theories,this paper made an in-depth analysis of the genesis mechanism of the Xingfu Spring and put forward its own point of view based on field investigation,tracer test and geophysical prospecting.It will provide a scientific basis for the research on the same type of water-bearing anticline springs and the rational exploitation and utilization of groundwater resources in the area.
Wumeng Mountain stretch across Yunnan,Guizhou and Sichuan provinces.It is one of the battlegrounds for the new round of poverty alleviation in China.The Wujiaobao anticline is located in the middle of Wumeng Mountain,and distributed in the area from the Wujiaobao of Suijiang County to Loudong of Pingshan County.There are 45 natural.springs exposed in the periphery of the anticline.The Xingfu Spring is the water supply source of Xintan town that 2 km away from the core,which is located in the northwestern wing of the anticline of Wujiaobao,and the seasonal flow is 141 L/s and 822 L/s in the low water season and in the abundant water season respectively.According to the previous investigations,there are mainly.two different theories on the genesis mechanism of the spring,one is the theory of "rising springs" and the other is the theory of "falling springs".According to the above theories,this paper made an in-depth analysis of the genesis mechanism of the Xingfu Spring and put forward its own point of view based on field investigation,tracer test and geophysical prospecting.It will provide a scientific basis for the research on the same type of water-bearing anticline springs and the rational exploitation and utilization of groundwater resources in the area.
引文
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[6]#12
[7]屈伟,丁坚平,邹仕孝,等.褶皱构造对岩溶泉发育的控制作用一以贵州威宁地区为例[J].地下水,2009,(6):131-133.(QU Wei,DING Jianping,ZOU Shixiao,et al.Control effect of fold structure on the development of karst springs-a case study in Weining,Guizhou[J].Ground water,2009,(6):131-133.(in Chinese))
[8]袁汉林,王大瑞,蔡辉,等.区域水文地质普查报告[R].1980.(YUAN Hanlin,WANG Darui,CAI Hui,et al.Report on the regional hydrogeological survey[R].1980.(in Chinese))
[9]李晓.云南省绥江县新城供水工程水源论证报告[R].2007.(LI Xiao.Water resources demonstration report of Suijiang water supply project in Suijiang county,Yunnan province[R].2007.(in Chinese))
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[11]郑勇,孙忠伟,刘涛,等.浅谈新疆天然矿泉水的成因类型[J].西部探矿工程,2015,27(3):159-162+174.(ZHENG Yong,SUN Zhongwei,LIU Tao,et al.Discussion on the genetic types of natural mineral water in Xinjiang[J].West-China Exploration Engineering,2015,27(3):159-162+174.(in Chinese))
[12]王宇.云南泸西皮家寨岩溶大泉束流调压壅水开发示范[J].中国岩溶,2008,(1):1-5+18.(WANG Yu.Demonstration of the development of turbulent pressure and muddy water in the karst springs in the Pijiazhai,Yunnan,China[J].Carsologica Sinica,2008,(1):1-5+18.(in Chinese))
[13]王永,张鹏川.六盘山区臭水泉群的水文地质特征与成因[J].中国煤田地质,2005,(3):23-26.(WANG Yong,ZHANG Pengchuan.Hydrogeological characteristics and genesis of the Choushui spring group in Liupan montains[J].Coal Geology of china,2005,(3):23-26.(in Chinese))
[14]田级生.太行山东麓岩溶大泉成因及其开发利用[J].水文地质工程地质,1983,(6):41-44.(TIAN Jisheng.Causes of formation and exploitation of karst springs in the eastern Taihang mountains[J].Hydrogeology&Engineering Geology,1983,(6):41-44.(in Chinese))
[15]施佳会,王锦国,陈舟.其宗岩溶泉成因简析[J].水电能源科学,2014,32(11):58-62.(SHI Jiahui,WANG Jinguo,CHEN Zhou.A brief analysis on the causes of the formation of the karst springs in Tibet[J].Water Resources and Power,2014,32(11):58-62.(in Chinese))
[2]胡国华,肖翔群.黄河多泥沙河段扩散系数的示踪实验研究[J].水动力学研究与进展(A辑),2005,(6):773-779.(HU Guohua, XIAO Xiangqun.Experimental study by tracing on diffusion coefficient at heavy sediment-carrying reach of Yellow River[J].Journal of Hydrodynamics(Series A),2005,(6):773-779.(in Chinese))
[3]周克钊,余常昭,张永良.天然河流纵向离散系数示踪实验计算方法研究[J].环境科学学报,1986,(3):314-326.(ZHOU Kezhao,YU Changzhao,ZHANG Yongliang.Study on calculation of vertical discrete coefficient tracer for natural rivers[J].Acta Scientiae Circumstantiae,1986,(3):314-326.(in Chinese))
[4]张永良,周克钊,王和平,等.三种不同投放方式的示踪实验[J].水利学报,1987,(2):60-65.(ZHANG Yongliang,ZHOU Kezhao,WANG Heping,el al.Tracer experiments with three different delivery methods[J].Journal of Hydraulic Engineering,1987,(2):60-65.(in Chinese))
[5]郑晓明,周建伟,柴波.广西桂平市西山乳泉的成因探讨[J].安全与环境工程,2013,(2):4-9.(ZHENG Xiaoming&ZHOU Jianwei,CHAI Bo.Study on the cause of Xishan milk spring in Guiping,Guangxi[J].Safety and Environmental Engineering,2013,(2):4-9.(in Chinese))
[6]#12
[7]屈伟,丁坚平,邹仕孝,等.褶皱构造对岩溶泉发育的控制作用一以贵州威宁地区为例[J].地下水,2009,(6):131-133.(QU Wei,DING Jianping,ZOU Shixiao,et al.Control effect of fold structure on the development of karst springs-a case study in Weining,Guizhou[J].Ground water,2009,(6):131-133.(in Chinese))
[8]袁汉林,王大瑞,蔡辉,等.区域水文地质普查报告[R].1980.(YUAN Hanlin,WANG Darui,CAI Hui,et al.Report on the regional hydrogeological survey[R].1980.(in Chinese))
[9]李晓.云南省绥江县新城供水工程水源论证报告[R].2007.(LI Xiao.Water resources demonstration report of Suijiang water supply project in Suijiang county,Yunnan province[R].2007.(in Chinese))
[10]孙峰根,罗绍河,王心义.关于地下水排泄的若干理论问题[J].焦作矿业学院学报,1994,(4):1-6.(SUN Fenggen,LUO Shaohe,WANG Xinyi.Some theoretical issues on groundwater excretion[J].Journal of Jiaozuo Mining Institute,1994,(4):1-6.(in Chinese))
[11]郑勇,孙忠伟,刘涛,等.浅谈新疆天然矿泉水的成因类型[J].西部探矿工程,2015,27(3):159-162+174.(ZHENG Yong,SUN Zhongwei,LIU Tao,et al.Discussion on the genetic types of natural mineral water in Xinjiang[J].West-China Exploration Engineering,2015,27(3):159-162+174.(in Chinese))
[12]王宇.云南泸西皮家寨岩溶大泉束流调压壅水开发示范[J].中国岩溶,2008,(1):1-5+18.(WANG Yu.Demonstration of the development of turbulent pressure and muddy water in the karst springs in the Pijiazhai,Yunnan,China[J].Carsologica Sinica,2008,(1):1-5+18.(in Chinese))
[13]王永,张鹏川.六盘山区臭水泉群的水文地质特征与成因[J].中国煤田地质,2005,(3):23-26.(WANG Yong,ZHANG Pengchuan.Hydrogeological characteristics and genesis of the Choushui spring group in Liupan montains[J].Coal Geology of china,2005,(3):23-26.(in Chinese))
[14]田级生.太行山东麓岩溶大泉成因及其开发利用[J].水文地质工程地质,1983,(6):41-44.(TIAN Jisheng.Causes of formation and exploitation of karst springs in the eastern Taihang mountains[J].Hydrogeology&Engineering Geology,1983,(6):41-44.(in Chinese))
[15]施佳会,王锦国,陈舟.其宗岩溶泉成因简析[J].水电能源科学,2014,32(11):58-62.(SHI Jiahui,WANG Jinguo,CHEN Zhou.A brief analysis on the causes of the formation of the karst springs in Tibet[J].Water Resources and Power,2014,32(11):58-62.(in Chinese))
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