长白山矿泉水补给径流与排泄关系
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摘要
为研究长白山地区广泛分布的偏硅酸型矿泉水的补给源,通过氢氧同位素与水化学分析,结合水文地质、地球物理等资料,确定长白山泉水接受来自于西藏羌塘盆地的外源水补给。长白山泉水TDS很低但富含偏硅酸的现象表明,地下水流经的含水层是由硅酸盐等火山岩组成,结合长白山地区火山玄武岩大量的喷发事实,推断地下水导水通道由孔洞玄武岩构成。指出应加强对西藏冰川、河流与湖泊的保护,从而确保长白山优质矿泉水能够持续地开发利用。
In order to study the supply source of widely distributed metasilicate type mineral water in the Changbai Mountain area,based on the information of hydrogeology and geophysics,the water supply of the Changbai Mountain springs from the Qiangtang Basin in Tibet was determined,through the hydrogen and oxygen isotope analysis as well as the water chemical analysis. TDS of the Changbai Mountain spring water is low,but with rich metasilicate,and this phenomenon indicates that the aquifer that water flows through is composed of silicate volcanic rock. Combined with the massive eruption of volcanic basalt in the area of Changbai Mountain,it can be concluded that the groundwater channel is composed of pore basalt. Therefore,the protection of Tibetan glaciers,rivers and lakes should be strengthened to ensure the sustainable development and utilization of high-quality mineral water in the area of Changbai Mountain.
In order to study the supply source of widely distributed metasilicate type mineral water in the Changbai Mountain area,based on the information of hydrogeology and geophysics,the water supply of the Changbai Mountain springs from the Qiangtang Basin in Tibet was determined,through the hydrogen and oxygen isotope analysis as well as the water chemical analysis. TDS of the Changbai Mountain spring water is low,but with rich metasilicate,and this phenomenon indicates that the aquifer that water flows through is composed of silicate volcanic rock. Combined with the massive eruption of volcanic basalt in the area of Changbai Mountain,it can be concluded that the groundwater channel is composed of pore basalt. Therefore,the protection of Tibetan glaciers,rivers and lakes should be strengthened to ensure the sustainable development and utilization of high-quality mineral water in the area of Changbai Mountain.
引文
[1]林琳.长白山区矿泉水资源成因与开发调控的研究[D].长春:吉林大学,2016.
[2]刘彦臣,张宇石.研析长白山天然矿泉水资源基本特征及其价值[J].通化师范学院学报,2009,30(2):52-54.(LIUYanchen,ZHANG Yushi.Basic features and value of natural mineral water resources in Changbai Mountain[J].Journal of Tonghua Teachers Collese,2009,30(2):52-54.(in Chinese))
[3]张勃夫.长白山靖宇矿泉水矿田形成分布特征及开发战略建议[J].吉林地质,2001,20(2):58-63.(ZHANG Bofu.The distributive characteristics of Jingyu mineral water field in the Changbaishan area,Jinlin Province and its suggestion for developmental strategy[J].Jilin Geology,2001,20(2):58-63.(in Chinese))
[4]江巧宁,陈建生.深循环地下水补给长白山天池的水量平衡分析[J].水资源保护,2015,31(5):7-13.(JIANG Qiaoning,CHEN Jiansheng.Analysis on water balance of deep cycle groundwater supplying Tianchi Lake of Changbai Mountain[J].Water Resources Protection,2015,31(5):7-13.(in Chinese))
[5]杨雪,杨东,安丽娜,等.1961-2013年吉林省气温与降水变化特征[J].中国农学通报,2016,32(29):139-146.(YANG Xue,YANG Dong,AN Lina,et al.Variation characteristics of temperature and precipitation in Jinlin:from 1961 to2013[J].Chinese Agricultural Science Bulletin,2016,32(29):139-146.(in Chinese))
[6]赵清华,谭文清,孙春.吉林长白山饮用天然矿泉水形成条件与资源保护[J].吉林地质,2005,24(4):64-70.(ZHAOQinghua,TAN Wenqing,SUN Chun.The forming condition and resource preservation of natural mineral drinking water in Changbai Mountain[J].Jilin Geology,2005,24(4):64-70.(in Chinese))
[7]吉林省长白山地区靖宇县和抚松县天然矿泉水调查评价报告[R].长春:吉林省地质工程勘察院,2003.
[8]危润初.靖宇国家级自然保护区天然矿泉水形成机理研究[D].长春:吉林大学,2014.
[9]金东淳,崔钟燮.长白山天池火山喷发历史文献记载的考究[J].地质论评,1999,45(增刊1):304-307.(JIN Dongchun,CUI Zhongxie.A study of eruptions in Tianchi Volcano,Changbai Mountain recorded in historical documents[J].Geological Review,1999,45(Sup1):304-307.(in Chinese))
[10]张兴库,朴观熙.长白山天池水文特性分析[J].水文,1991,11(2):49-51.(ZHANG Xingku,PIAO Guanxi.Analysis on hydrologic characteristics of Changbaishan Tianchi[J].Journal of China Hydrology,1991,11(2):49-51.(in Chinese))
[11]ZHOU Shiqiao,KANG Shichang,CHEN Feng,et al.Water balance observations reveal significant subsurface water seepage from Lake Nam Co,south-central Tibetan Plateau[J].Journal of Hydrology,2013,491:89-99.
[12]陈建生,江巧宁.地下水深循环研究进展[J].水资源保护,2015,31(6):8-17.(CHEN Jiansheng,JIANG Qiaoning.Research progress of ground water deep circulation[J].Water Resources Protection,2015,31(6):8-17.(in Chinese))
[13]高月.抚松县矿泉水补给条件与形成机理研究[D].长春:吉林大学,2016.
[14]张兵,宋献方,张应华,等.基于氚和CFCs的三江平原浅层地下水更新能力估算[J].自然资源学报,2014,29(11):1859-1868.(ZHANG Bing,SONG Xianfang,ZHANG Yinghua,et al.Estimation of groundwater renewal rate by tritium and chlorofluorocarbons in Sanjiang Plain[J].Journal of Natural Resources,2014,29(11):1859-1868.(in Chinese))
[15]洪昌红,邱静,黄本胜,等.补给带法在基岩裂隙水可开采量计算中的应用[J].水资源保护,2013,29(2):58-60.(HONGChanghong,QIU Jing,HUANG Bensheng,et al.Application of recharge zone method to calculation of allowable withdrawal of bedrock fissure water[J].Water Resources Protection,2013,29(2):58-60.(in Chinese))
[16]陈建生,杨光亮,王婷,等.内蒙古鄂尔多斯西北土壤水流动示踪实验及自流井群补给源讨论[J].地球学报,2014,39(3):365-374.(CHEN Jiansheng,YANG Guangliang,WANG Ting,et al.Soil water flow tracer test in northwest Ordos Basin,Inner Mongolia and discussion on recharge resources of artesian wells[J].Acta Geoscientica Sinica,2014,39(3):365-374.(in Chinese))
[17]陈建生,王婷,陈茜茜,等.鄂尔多斯自流盆地地下水来源争议问题讨论[J].地质论评,2013,59(5):900-908.(CHENJiansheng,WANG Ting,CHEN Xixi,et al.Discussion on the origin of groundwater in the Orods Basin[J].Geological Review,2013,59(5):900-908.(in Chinese))
[18]CHEN Jiansheng,LIU Xiaoyan,WANG Chiyuen,et al.Isotopic constraints on the origin of groundwater in the Ordos Basin of northern China[J].Environmental Earth Sciences,2012,66(2):505-517.
[19]陈建生,陈亚飞,谢飞,等.鄂尔多斯乌海地下水水位上升原因分析[J].水资源保护,2016,32(3):1-9.(CHEN Jiansheng,CHEN Yafei,XIE Fei,et al.Analysis of causes of groundwater level rise in Wuhai area of Ordos Basin[J].Water Resources Protection,2016,32(3):1-9.(in Chinese))
[20]陈建生,刘震,刘晓艳.深循环地下水维系黄土高原风尘颗粒连续沉积[J].地质学报,2013,87(2):278-287.(CHENJiansheng,LIU Zhen,LIU Xiaoyan.Deep-circulation groundwater maintains continuous deposition of dusty particles in loess plateau[J].Acta Geologica Sinica,2013,87(2):278-287.(in Chinese))
[21]陈建生,王文凤.深循环地下水作用下红土与黄土成因研究[J].水资源保护,2017,33(3):1-7.(CHEN Jiansheng,WANG Wenfeng.Study on the formation mechanism of aeolian soil of laterite and loess under the action of deep groundwater circulation[J].Water Resources Protection,2017,33(3):1-7.(in Chinese))
[22]韩子夜.我国新生代玄武岩地下水资源及其开发利用[J].勘察科学技术,1989(3):26-29.(HAN Ziye.Cenozoic basalt and its exploitation and utilization of groundwater resources in our country[J].Site Investigation Science and Technology,1989(3):26-29.(in Chinese))
[2]刘彦臣,张宇石.研析长白山天然矿泉水资源基本特征及其价值[J].通化师范学院学报,2009,30(2):52-54.(LIUYanchen,ZHANG Yushi.Basic features and value of natural mineral water resources in Changbai Mountain[J].Journal of Tonghua Teachers Collese,2009,30(2):52-54.(in Chinese))
[3]张勃夫.长白山靖宇矿泉水矿田形成分布特征及开发战略建议[J].吉林地质,2001,20(2):58-63.(ZHANG Bofu.The distributive characteristics of Jingyu mineral water field in the Changbaishan area,Jinlin Province and its suggestion for developmental strategy[J].Jilin Geology,2001,20(2):58-63.(in Chinese))
[4]江巧宁,陈建生.深循环地下水补给长白山天池的水量平衡分析[J].水资源保护,2015,31(5):7-13.(JIANG Qiaoning,CHEN Jiansheng.Analysis on water balance of deep cycle groundwater supplying Tianchi Lake of Changbai Mountain[J].Water Resources Protection,2015,31(5):7-13.(in Chinese))
[5]杨雪,杨东,安丽娜,等.1961-2013年吉林省气温与降水变化特征[J].中国农学通报,2016,32(29):139-146.(YANG Xue,YANG Dong,AN Lina,et al.Variation characteristics of temperature and precipitation in Jinlin:from 1961 to2013[J].Chinese Agricultural Science Bulletin,2016,32(29):139-146.(in Chinese))
[6]赵清华,谭文清,孙春.吉林长白山饮用天然矿泉水形成条件与资源保护[J].吉林地质,2005,24(4):64-70.(ZHAOQinghua,TAN Wenqing,SUN Chun.The forming condition and resource preservation of natural mineral drinking water in Changbai Mountain[J].Jilin Geology,2005,24(4):64-70.(in Chinese))
[7]吉林省长白山地区靖宇县和抚松县天然矿泉水调查评价报告[R].长春:吉林省地质工程勘察院,2003.
[8]危润初.靖宇国家级自然保护区天然矿泉水形成机理研究[D].长春:吉林大学,2014.
[9]金东淳,崔钟燮.长白山天池火山喷发历史文献记载的考究[J].地质论评,1999,45(增刊1):304-307.(JIN Dongchun,CUI Zhongxie.A study of eruptions in Tianchi Volcano,Changbai Mountain recorded in historical documents[J].Geological Review,1999,45(Sup1):304-307.(in Chinese))
[10]张兴库,朴观熙.长白山天池水文特性分析[J].水文,1991,11(2):49-51.(ZHANG Xingku,PIAO Guanxi.Analysis on hydrologic characteristics of Changbaishan Tianchi[J].Journal of China Hydrology,1991,11(2):49-51.(in Chinese))
[11]ZHOU Shiqiao,KANG Shichang,CHEN Feng,et al.Water balance observations reveal significant subsurface water seepage from Lake Nam Co,south-central Tibetan Plateau[J].Journal of Hydrology,2013,491:89-99.
[12]陈建生,江巧宁.地下水深循环研究进展[J].水资源保护,2015,31(6):8-17.(CHEN Jiansheng,JIANG Qiaoning.Research progress of ground water deep circulation[J].Water Resources Protection,2015,31(6):8-17.(in Chinese))
[13]高月.抚松县矿泉水补给条件与形成机理研究[D].长春:吉林大学,2016.
[14]张兵,宋献方,张应华,等.基于氚和CFCs的三江平原浅层地下水更新能力估算[J].自然资源学报,2014,29(11):1859-1868.(ZHANG Bing,SONG Xianfang,ZHANG Yinghua,et al.Estimation of groundwater renewal rate by tritium and chlorofluorocarbons in Sanjiang Plain[J].Journal of Natural Resources,2014,29(11):1859-1868.(in Chinese))
[15]洪昌红,邱静,黄本胜,等.补给带法在基岩裂隙水可开采量计算中的应用[J].水资源保护,2013,29(2):58-60.(HONGChanghong,QIU Jing,HUANG Bensheng,et al.Application of recharge zone method to calculation of allowable withdrawal of bedrock fissure water[J].Water Resources Protection,2013,29(2):58-60.(in Chinese))
[16]陈建生,杨光亮,王婷,等.内蒙古鄂尔多斯西北土壤水流动示踪实验及自流井群补给源讨论[J].地球学报,2014,39(3):365-374.(CHEN Jiansheng,YANG Guangliang,WANG Ting,et al.Soil water flow tracer test in northwest Ordos Basin,Inner Mongolia and discussion on recharge resources of artesian wells[J].Acta Geoscientica Sinica,2014,39(3):365-374.(in Chinese))
[17]陈建生,王婷,陈茜茜,等.鄂尔多斯自流盆地地下水来源争议问题讨论[J].地质论评,2013,59(5):900-908.(CHENJiansheng,WANG Ting,CHEN Xixi,et al.Discussion on the origin of groundwater in the Orods Basin[J].Geological Review,2013,59(5):900-908.(in Chinese))
[18]CHEN Jiansheng,LIU Xiaoyan,WANG Chiyuen,et al.Isotopic constraints on the origin of groundwater in the Ordos Basin of northern China[J].Environmental Earth Sciences,2012,66(2):505-517.
[19]陈建生,陈亚飞,谢飞,等.鄂尔多斯乌海地下水水位上升原因分析[J].水资源保护,2016,32(3):1-9.(CHEN Jiansheng,CHEN Yafei,XIE Fei,et al.Analysis of causes of groundwater level rise in Wuhai area of Ordos Basin[J].Water Resources Protection,2016,32(3):1-9.(in Chinese))
[20]陈建生,刘震,刘晓艳.深循环地下水维系黄土高原风尘颗粒连续沉积[J].地质学报,2013,87(2):278-287.(CHENJiansheng,LIU Zhen,LIU Xiaoyan.Deep-circulation groundwater maintains continuous deposition of dusty particles in loess plateau[J].Acta Geologica Sinica,2013,87(2):278-287.(in Chinese))
[21]陈建生,王文凤.深循环地下水作用下红土与黄土成因研究[J].水资源保护,2017,33(3):1-7.(CHEN Jiansheng,WANG Wenfeng.Study on the formation mechanism of aeolian soil of laterite and loess under the action of deep groundwater circulation[J].Water Resources Protection,2017,33(3):1-7.(in Chinese))
[22]韩子夜.我国新生代玄武岩地下水资源及其开发利用[J].勘察科学技术,1989(3):26-29.(HAN Ziye.Cenozoic basalt and its exploitation and utilization of groundwater resources in our country[J].Site Investigation Science and Technology,1989(3):26-29.(in Chinese))