巴丹吉林沙漠南缘地下水补给机制研究
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摘要
为研究巴丹吉林沙漠南缘水源地的地下水补给机制,分析了采自浅井、深井及湖泊的35个水样的Cl-浓度、TDS含量和氢氧同位素特征。根据巴丹吉林水源地及周边水化学水平分布特征,结合研究区气象和水文条件、水文地质结构、地下水流场发现,戈壁区地下水对沙漠区地下水无明显补给作用,但是沙漠区、戈壁区及山区地下水稳定同位素关系表明,沙漠区地下水来源于南部山区及戈壁区的地下水或降水。通过野外调查发现,沙漠边缘分布大量洪积黏土,认为沙漠外围山区、山前戈壁带降水在季节性河道形成的脉冲式洪流是沙漠区地下水的重要补给来源之一,这一认识不仅解释了采用水化学和同位素技术进行分析而获得不同结论的原因,而且有利于地下水资源评价。
Chloride,TDS,deuterium and oxygen-18 were analyzed for 35 samples from deep and shallow wells,lakes to research groundwater recharge mechanism in Badain Jaran well field which lies in the south of Badain Jaran desert.Based on the horizontal distribution features of hydrogeochemistry and combined with the meteorological and hydrological conditions,groundwater in the desert terrain do not originate in gobi area.While,the groundwater stable isotopic relationship between the mountainous area,gobi area and desert terrain indicates that the groundwater in desert terrain is derived from southern mountainous area and gobi region.On the basis of previous studies and a large amount of pluvial clay in the desert edge were found in the field investigation indicate that the impulse type flood from mountainous area and gobi belt is one of the important recharge source of groundwater in desert area,this understanding not only explains the reason of different conclusions which are based on hydrogeochemistry and isotope technology respectively,but also is helpful for evaluation of groundwater resources.
Chloride,TDS,deuterium and oxygen-18 were analyzed for 35 samples from deep and shallow wells,lakes to research groundwater recharge mechanism in Badain Jaran well field which lies in the south of Badain Jaran desert.Based on the horizontal distribution features of hydrogeochemistry and combined with the meteorological and hydrological conditions,groundwater in the desert terrain do not originate in gobi area.While,the groundwater stable isotopic relationship between the mountainous area,gobi area and desert terrain indicates that the groundwater in desert terrain is derived from southern mountainous area and gobi region.On the basis of previous studies and a large amount of pluvial clay in the desert edge were found in the field investigation indicate that the impulse type flood from mountainous area and gobi belt is one of the important recharge source of groundwater in desert area,this understanding not only explains the reason of different conclusions which are based on hydrogeochemistry and isotope technology respectively,but also is helpful for evaluation of groundwater resources.
引文
[1]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,2002,27(2):127-133.
[2]文冬光,沈照理,钟佐燊,等.地球化学模拟及其在水文地质中的应用[J].地质科技情报,1995,14(1):99-104.
[3]张人权,梁杏,靳孟贵,等.当代水文地质学发展趋势与对策[J].水文地质工程地质,2005,32(1):51-56.
[4]李云峰,李金荣,侯光才,等.从水文地球化学角度研究鄂尔多斯盆地南区白垩系地下水的排泄途径[J].西北地质,2004,37(3):91-95.
[5]HERCZEG A L,RGERSEN T,CHIVAS A R,et al.Geochemistry of Groundwater from the Great Artesian Basin,Australia[J].Journal of Hydrology,1991,126(3-4):225-245.
[6]DONG Z,QIAN G,LYU P,et al.Investigation of the Sand Sea with the Tallest Dunes on Earth:China's Badain Jaran Sand Sea[J].Earth-Science Reviews,2013,120:20-39.
[7]任伟,金胜.应用音频大地电磁法探测内蒙古巴丹吉林高大沙山结构及成因[J].现代地质,2011,25(6):1167-1173.
[8]高志发,谢瑞金,尚雪峰,等.中华人民共和国区域水文地质普查报告(1∶20万):努尔盖公社幅[R].北京:全国地质资料馆,1981:103-106.
[9]CHEN J S,LI L,WANG J Y,et al.Groundwater Maintains Dune Landscape[J].Nature,2004,432:459-460.
[10]张竞.阿拉善西部关键水文地质问题研究[D].北京:中国地质大学,2015:54-56.
[11]张竞,王旭升,贾凤超,等.对内蒙古阿拉善西部地下水流向问题的新认识[J].现代地质,2015,29(1):213-219.
[12]黄天明,庞忠和.应用环境示踪剂探讨巴丹吉林沙漠及古日乃绿洲地下水补给[J].现代地质,2007,21(4):624-630.
[13]马妮娜,杨小平.巴丹吉林沙漠及其东南边缘地区水化学和环境同位素特征及其水文学意义[J].第四纪研究,2008,28(4):702-711.
[14]马金珠,黄天明,丁贞玉,等.同位素指示的巴丹吉林沙漠南缘地下水补给来源[J].地球科学进展,2007,22(9):922-930.
[15]Gates J B,Edmunds W M,Darling W G,et al.Conceptual Model of Recharge to Southeastern Badain Jaran Desert Groundwater and Lakes from Environmental Tracers[J].Applied Geochemistry,2008,23:3519-3534.
[16]欧阳波罗.巴丹吉林沙漠湖水和地下水氢氧同位素研究[D].北京:中国地质大学,2014:39.
[17]刘建刚.巴丹吉林沙漠湖泊和地下水补给机制[J].水资源保护,2010,26(2):18-23.
[18]李文鹏,郝爱兵,刘振英,等.塔里木盆地地下水开发远景区研究[M].北京:地质出版社,2000:59-61.
[19]RICHARD S J,RYAN M P,JUSTIN P D.Spatial and Temporal Constraints on Regional-Scale Groundwater Flow in the Pampa Del Tamarugal Basin,Atacama Desert,Chile[J].Hydrogeology Journal,2016,24(8):1921-1937.
[20]王秀云,张振宏,李发军,等.气象服务在阿拉善右旗旅游业中的作用与效益分析[J].自然科学,2016(10):208.
[21]朱家涛,贺连忠,何贵平,等.内蒙古阿拉善盟阿拉善右旗山洪灾害分析评价报告[R].阿拉善右旗:阿拉善右旗水务局,2015:14-17.
[22]陈建生,李发全.内蒙古阿拉善右旗巴丹吉林镇新水源地研究报告[R].南京:河海大学,2014:35-36.
[23]绳宝印,李嘉斌,张哲.中华人民共和国区域水文地质普查报告(1∶20万):雅布赖盐场幅[R].北京:全国地质资料馆,1981:17-18.
[24]HERCZEG A L,EDMUNDS W M.Inorganic Ions as Tracers[M]//COOK P G,HERCZEG A L.Environmental Tracers in Subsurface Hydrology.Boston:Kluwer,1999:31-77.
[25]Matthess G.The Properties of Groundwater[M].New Jersey:John Wiley and Sons,1982:255.
[26]殷秀兰,凤蔚,王瑞久,等.新疆乌鲁木齐河流域北部平原区水文地球化学[J].地球学报,2015,36(1):77-84.
[27]顾慰祖,庞忠和,王全九,等.同位素水文学[M].北京:科学出版社,2011:119-126.
[28]WU Y,WANG N A,ZHAO L Q,et al.Hydrochemical Characteristics and Recharge Sources of Lake Nuoertu in the Badain Jaran Desert[J].China Sci.Bull.,2014,59:886-895.
[2]文冬光,沈照理,钟佐燊,等.地球化学模拟及其在水文地质中的应用[J].地质科技情报,1995,14(1):99-104.
[3]张人权,梁杏,靳孟贵,等.当代水文地质学发展趋势与对策[J].水文地质工程地质,2005,32(1):51-56.
[4]李云峰,李金荣,侯光才,等.从水文地球化学角度研究鄂尔多斯盆地南区白垩系地下水的排泄途径[J].西北地质,2004,37(3):91-95.
[5]HERCZEG A L,RGERSEN T,CHIVAS A R,et al.Geochemistry of Groundwater from the Great Artesian Basin,Australia[J].Journal of Hydrology,1991,126(3-4):225-245.
[6]DONG Z,QIAN G,LYU P,et al.Investigation of the Sand Sea with the Tallest Dunes on Earth:China's Badain Jaran Sand Sea[J].Earth-Science Reviews,2013,120:20-39.
[7]任伟,金胜.应用音频大地电磁法探测内蒙古巴丹吉林高大沙山结构及成因[J].现代地质,2011,25(6):1167-1173.
[8]高志发,谢瑞金,尚雪峰,等.中华人民共和国区域水文地质普查报告(1∶20万):努尔盖公社幅[R].北京:全国地质资料馆,1981:103-106.
[9]CHEN J S,LI L,WANG J Y,et al.Groundwater Maintains Dune Landscape[J].Nature,2004,432:459-460.
[10]张竞.阿拉善西部关键水文地质问题研究[D].北京:中国地质大学,2015:54-56.
[11]张竞,王旭升,贾凤超,等.对内蒙古阿拉善西部地下水流向问题的新认识[J].现代地质,2015,29(1):213-219.
[12]黄天明,庞忠和.应用环境示踪剂探讨巴丹吉林沙漠及古日乃绿洲地下水补给[J].现代地质,2007,21(4):624-630.
[13]马妮娜,杨小平.巴丹吉林沙漠及其东南边缘地区水化学和环境同位素特征及其水文学意义[J].第四纪研究,2008,28(4):702-711.
[14]马金珠,黄天明,丁贞玉,等.同位素指示的巴丹吉林沙漠南缘地下水补给来源[J].地球科学进展,2007,22(9):922-930.
[15]Gates J B,Edmunds W M,Darling W G,et al.Conceptual Model of Recharge to Southeastern Badain Jaran Desert Groundwater and Lakes from Environmental Tracers[J].Applied Geochemistry,2008,23:3519-3534.
[16]欧阳波罗.巴丹吉林沙漠湖水和地下水氢氧同位素研究[D].北京:中国地质大学,2014:39.
[17]刘建刚.巴丹吉林沙漠湖泊和地下水补给机制[J].水资源保护,2010,26(2):18-23.
[18]李文鹏,郝爱兵,刘振英,等.塔里木盆地地下水开发远景区研究[M].北京:地质出版社,2000:59-61.
[19]RICHARD S J,RYAN M P,JUSTIN P D.Spatial and Temporal Constraints on Regional-Scale Groundwater Flow in the Pampa Del Tamarugal Basin,Atacama Desert,Chile[J].Hydrogeology Journal,2016,24(8):1921-1937.
[20]王秀云,张振宏,李发军,等.气象服务在阿拉善右旗旅游业中的作用与效益分析[J].自然科学,2016(10):208.
[21]朱家涛,贺连忠,何贵平,等.内蒙古阿拉善盟阿拉善右旗山洪灾害分析评价报告[R].阿拉善右旗:阿拉善右旗水务局,2015:14-17.
[22]陈建生,李发全.内蒙古阿拉善右旗巴丹吉林镇新水源地研究报告[R].南京:河海大学,2014:35-36.
[23]绳宝印,李嘉斌,张哲.中华人民共和国区域水文地质普查报告(1∶20万):雅布赖盐场幅[R].北京:全国地质资料馆,1981:17-18.
[24]HERCZEG A L,EDMUNDS W M.Inorganic Ions as Tracers[M]//COOK P G,HERCZEG A L.Environmental Tracers in Subsurface Hydrology.Boston:Kluwer,1999:31-77.
[25]Matthess G.The Properties of Groundwater[M].New Jersey:John Wiley and Sons,1982:255.
[26]殷秀兰,凤蔚,王瑞久,等.新疆乌鲁木齐河流域北部平原区水文地球化学[J].地球学报,2015,36(1):77-84.
[27]顾慰祖,庞忠和,王全九,等.同位素水文学[M].北京:科学出版社,2011:119-126.
[28]WU Y,WANG N A,ZHAO L Q,et al.Hydrochemical Characteristics and Recharge Sources of Lake Nuoertu in the Badain Jaran Desert[J].China Sci.Bull.,2014,59:886-895.
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