穆兴平原北部地下水年龄及更新性
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摘要
地下水年龄结构是了解一个地区地下水资源开采可持续性的重要基础。穆兴平原地下水开采量增加以及地下水环境恶化,对该地区可持续发展有一定制约,为此在2016年采集CFCs样品31组和3H样品60组,估算了研究区地下水年龄。结果表明,穆兴平原北部地下水年龄为21年到大于65年,由西北部和穆棱河向平原中部及乌苏里江逐渐变老,更新性变差,主要受到大气降水和地表河水补给,但是由于地表覆盖一层黏性土,地下水中缺失小于10年的水;不同井深样品中二者及NO_3~-浓度的变化,表明在60 m以上地下水的防污性能较差,而在100 m以下则较好,饮用水源井深需超过100 m。
The age structure of aquifer is an important basis for understanding the sustainability of groundwater exploitation.Increasing groundwater pumping with deteriorate groundwater environment in the Muling-Xingkai Plain(MXP) has restricted to some extent the sustainable development of the region. 31 groups of CFCs and 60 groups of 3H samples were collected to delineate groundwater flow systems. Estimated groundwater age ranges from 21 years to more than 70 years in the northern part of the MXP.Younger water occurs in northwest piedmont and hilly areas as well as Muling River, while older water occurs in the central part of the plain and the Wusuli River. This reflects long flow paths associated with regional flow. Although groundwater is mainly recharged by rain and surface water, ground water younger than 10 years was not found for the unsaturated zone consisting of silty clay. The variations of 3H and CFCs combined NO_3~- with wells depth indicate that the aquifer sensitivity of groundwater system above 60 m is low and it is high below 100 m. Wells for drinking water should exceed 100 m.
The age structure of aquifer is an important basis for understanding the sustainability of groundwater exploitation.Increasing groundwater pumping with deteriorate groundwater environment in the Muling-Xingkai Plain(MXP) has restricted to some extent the sustainable development of the region. 31 groups of CFCs and 60 groups of 3H samples were collected to delineate groundwater flow systems. Estimated groundwater age ranges from 21 years to more than 70 years in the northern part of the MXP.Younger water occurs in northwest piedmont and hilly areas as well as Muling River, while older water occurs in the central part of the plain and the Wusuli River. This reflects long flow paths associated with regional flow. Although groundwater is mainly recharged by rain and surface water, ground water younger than 10 years was not found for the unsaturated zone consisting of silty clay. The variations of 3H and CFCs combined NO_3~- with wells depth indicate that the aquifer sensitivity of groundwater system above 60 m is low and it is high below 100 m. Wells for drinking water should exceed 100 m.
引文
Chen Zhongyu,Qi Jixiang,Zhang Zhaoji.2010.Application of Isotope Hydrogeology Method in Typical Basins of North China[M].Beijing:Science Press(in Chinese).
Clark I D,Fritz P.1997.Environmental Isotopes in Hydrogeology[M].Boca Raton:Springer-Verlag,.
Cui Xiaoshun,Zheng Zhaoxian,Cheng Zhongshuang,Su Chen,Li Zhuang,Wu Yulong,Chen Zongyu.2018.Hydrochemical distribution characteristic and formation mechanism of shallow groundwater in the north of Muling-Xingkai Plain[J].South-toNorth Water Transfers and Water Science&Technology,16(4):146-153(in Chinese with English abstract).
Doney S C,Glover D M,Jenkins W J.1992.A model function of the global bomb tritium distribution in precipitation,1960-1986[J].Journal of Geophysical Research Oceans,97(C4):5481-5492.
Fouli Y,Cade-Menun B J,Cutforth H W.2013.Freeze-thaw cycles and soil water content effects on infiltration rate of three Saskatchewan soils[J].Canadian Journal of Soil Science,93(4):485-496.
International Atomic Energy Agency(IAEA).2006.Use of Chlorofluorocarbons in Hydrology:A Guidebook[M].Vienna:International Atomic Energy Agency.
Klaus H.2006.Environmental Tracers,Groundwater Age and Vulnerability.Groundwater Resources in Buried Valleys[M]//Reinhard Kirsch et al(ed.).Hannover:Leibniz Institute for Applied Geosciences,141-148.
Kendy,Eloise,Yongqiang Zhang,Changming Liu,Jinxia Wang,and Tammo Steenhuis.2004.Groundwater Recharge from Irrigated Cropland in the North China Plain:Case Study of Luancheng County,Hebei Province,1949-2000[J].Hydrological Processes,18,(12):2289-302.
Li Jing,Li Fadong,Song Shuai,Zhang,Yan,Cai Wenjing,Zhang Fang.2012.Worldwide application and prospective of CFCs groundwater age-dating method[J].Ecology&Environmental Sciences,21(8):1503-1508(in Chinese with Englishi abstract).
Liu Fangfang.Ecological Quality Evaluation of Xingkai Lake Wetland Nature Reserve[D].Haerbin:Northeast Forestry University(in Chinese with English abstract).
Liu Futian,Su Xiaosi,Hou Guangcai,Lin Xueyu,Yi Shuping,Dong Weihong.2007.Application of CFCs methods in dating shallow groundwater in the ordos cretaceous groundwater basin[J].Journal of Jilin University,37(2):298-302(in Chinese with English abstract).
Liu Jun,Chen Zongyu,Wei Wen,Zhang yilong,Li Zhenghong,Liu Fuliang,Guo Hualiang.2014.Using chlorofluorocarbons(CFCs)and tritium(3H)to estimate groundwater age and flow velocity in Hohhot Basin,China[J].Hydrological Processes,28(3):1372-1382.
Liu Jun.2016.Study of Age Structure and Patterns of Groundwater Recharge and Groundwater Flow in Hohhot Basin[D].Bejing:Chinese Academy of Geological Sciences(in Chinese with English abstract).
Jeong S,Kim J,Lee K.2008.Effect of clay content on well-graded sands due to infiltration[J].Engineering Geology,102(1-2):74-81.
Oster H,Sonntag C,Münnich K O.1996.Groundwater age dating with chlorofluorocarbons[J].Water Resources Research,32(32):2989-3002.
Qin Dajun.2005.CFC dating method and its application in groundwater[J].Groundwater,27(6):435-437(in Chinese).
Santoni S,Huneau F,Garel E,Vergnaud-Ayraud V,Labasque T,Aquilina L.2016.Residence time,mineralization processes and groundwater origin within a carbonate coastal aquifer with a thick unsaturated zone[J].Journal of Hydrology,540:50-63.
Su Chen,Cheng Zhongshuang,Wei Wen,Chen Zongyu.2018.Assessing groundwater availability and the response of the groundwater system to intensive exploitation in the North China Plain by analysis of long-term isotopic tracer data[J].Hydrogeology Journal,26(5):1401-1415.
Sun Fangqiang,Yin Lihe,Wang Xiaoyong,Ma Hongyun,Zhang Jun,Dong Jiaqiu,He Shuaijun.2017.Determination of vertical infiltration recharge of groundwater in the thick unsaturated zone of Sangong River Basin,Xinjiang[J].Geology in China,44(5):913-923(in Chinese with English abstract).
Tu Leyi.2015.Analysis of Krypton Gas Dissolved in Groundwater for Radiokrypton Dating[D].Hefei:University of Science and Technology of China(in Chinese with English abstract).
von Rohden,Christoph,Andreas Kreuzer,Chen Zongyu,Rolf Kipfer,Werner Aeschbach-Hertig.2010.Characterizing the Recharge Regime of the Strongly Exploited Aquifers of the North China Plain by Environmental Tracers[J].Water Resources Research,46(5):1-14.
Wang,Fengsheng.1998.The regional recovery model of tritium concentration for meteoric water in jilin Province[J].Jilin Geology,3:75-81(in Chinese with English abstract).
Wang Jiyang,Chen Jiansheng,Chen Baohong,Tong Haibin,Tan Zhongcheng,Sun Yingying.2015.Review and prospect of isotope hydrology[J].Journal of Hohai University,43(5):406-413(in Chinese with English abstract).
Wen Dongguang.2002.Groundwater resources attribute based on environmental isotopes[J].Earth Science,27(2):141-147(in Chinese with English abstract).
Yurtsever Y,Mook W G.2001.Environmental Isotopes in the Hydrological Cycle.Principles and Applications[M].Vienna,27-32.
Zhang Bing.,Song Xianfang,Zhang,Yinghua,Han Dongmei,Yang,Lihu,Tang,Changyuan.2014.Estimation of groundwater renewal rate by tritium and chlorofluorocarbons in Sanjiang plain[J].Journal of Natural Resources,29(11):1859-1868(in Chinese with English abstract).
Zuber A.1986.Mathematical models for the interpretation of environmental radioisotopes in groundwater systems[C]//Handbook of Environmental Isotope Geochemistry,2:1-59.
陈宗宇,齐继祥,张兆吉.2010.北方典型盆地同位素水文地质学方法应用[M].北京:科学出版社.
崔小顺,郑昭贤,程中双,苏晨,李壮,吴宇龙,陈宗宇.2018.穆兴平原北区浅层地下水水化学分布特征及其形成机理[J].南水北调与水利科技,16(4):146-153.
李静,李发东,宋帅,张妍,蔡文静,张芳.2012.CFCs地下水年龄示踪技术的原理、应用及展望[J].生态环境学报,21(8):1503-1508.
刘芳芳.2009.兴凯湖湿地自然保护区生态质量评价[D].哈尔滨:东北林业大学.
刘君.2016.呼和浩特盆地地下水年龄结构与补给流动模式研究[D].北京:中国地质科学院.
柳富田,苏小四,侯光才,林学钰,易树平,董维红.2007.CFCs法在鄂尔多斯白垩系地下水盆地浅层地下水年龄研究中的应用[J].吉林大学学报(地球科学版),37(2):298-302.
秦大军.2005.地下水CFC定年方法及应用[J].地下水,27(6):435-437.
孙芳强,尹立河,王晓勇,马洪云,张俊,董佳秋,贺帅军.2017.新疆三工河流域厚层包气带区地下水垂向补给量的厘定[J].中国地质,44(5):913-923.
涂乐义.2015.地下水溶解氪气分析用于放射性氪同位素测年[D].合肥:中国科学技术大学.
汪集旸,陈建生,陆宝宏,童海滨,谭忠成,孙营营.2015.同位素水文学的若干回顾与展望[J].河海大学学报(自然科学版),43(5):406-413.
王凤生.1998.吉林省大气降水氚浓度恢复的区域模型探讨[J].吉林地质,3:75-81.
文冬光.2002.用环境同位素论区域地下水资源属性[J].地球科学,27(2):141-147.
张兵,宋献方,张应华,韩冬梅,杨丽虎,唐常源.2014.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,29(11):1859-1868.
Clark I D,Fritz P.1997.Environmental Isotopes in Hydrogeology[M].Boca Raton:Springer-Verlag,.
Cui Xiaoshun,Zheng Zhaoxian,Cheng Zhongshuang,Su Chen,Li Zhuang,Wu Yulong,Chen Zongyu.2018.Hydrochemical distribution characteristic and formation mechanism of shallow groundwater in the north of Muling-Xingkai Plain[J].South-toNorth Water Transfers and Water Science&Technology,16(4):146-153(in Chinese with English abstract).
Doney S C,Glover D M,Jenkins W J.1992.A model function of the global bomb tritium distribution in precipitation,1960-1986[J].Journal of Geophysical Research Oceans,97(C4):5481-5492.
Fouli Y,Cade-Menun B J,Cutforth H W.2013.Freeze-thaw cycles and soil water content effects on infiltration rate of three Saskatchewan soils[J].Canadian Journal of Soil Science,93(4):485-496.
International Atomic Energy Agency(IAEA).2006.Use of Chlorofluorocarbons in Hydrology:A Guidebook[M].Vienna:International Atomic Energy Agency.
Klaus H.2006.Environmental Tracers,Groundwater Age and Vulnerability.Groundwater Resources in Buried Valleys[M]//Reinhard Kirsch et al(ed.).Hannover:Leibniz Institute for Applied Geosciences,141-148.
Kendy,Eloise,Yongqiang Zhang,Changming Liu,Jinxia Wang,and Tammo Steenhuis.2004.Groundwater Recharge from Irrigated Cropland in the North China Plain:Case Study of Luancheng County,Hebei Province,1949-2000[J].Hydrological Processes,18,(12):2289-302.
Li Jing,Li Fadong,Song Shuai,Zhang,Yan,Cai Wenjing,Zhang Fang.2012.Worldwide application and prospective of CFCs groundwater age-dating method[J].Ecology&Environmental Sciences,21(8):1503-1508(in Chinese with Englishi abstract).
Liu Fangfang.Ecological Quality Evaluation of Xingkai Lake Wetland Nature Reserve[D].Haerbin:Northeast Forestry University(in Chinese with English abstract).
Liu Futian,Su Xiaosi,Hou Guangcai,Lin Xueyu,Yi Shuping,Dong Weihong.2007.Application of CFCs methods in dating shallow groundwater in the ordos cretaceous groundwater basin[J].Journal of Jilin University,37(2):298-302(in Chinese with English abstract).
Liu Jun,Chen Zongyu,Wei Wen,Zhang yilong,Li Zhenghong,Liu Fuliang,Guo Hualiang.2014.Using chlorofluorocarbons(CFCs)and tritium(3H)to estimate groundwater age and flow velocity in Hohhot Basin,China[J].Hydrological Processes,28(3):1372-1382.
Liu Jun.2016.Study of Age Structure and Patterns of Groundwater Recharge and Groundwater Flow in Hohhot Basin[D].Bejing:Chinese Academy of Geological Sciences(in Chinese with English abstract).
Jeong S,Kim J,Lee K.2008.Effect of clay content on well-graded sands due to infiltration[J].Engineering Geology,102(1-2):74-81.
Oster H,Sonntag C,Münnich K O.1996.Groundwater age dating with chlorofluorocarbons[J].Water Resources Research,32(32):2989-3002.
Qin Dajun.2005.CFC dating method and its application in groundwater[J].Groundwater,27(6):435-437(in Chinese).
Santoni S,Huneau F,Garel E,Vergnaud-Ayraud V,Labasque T,Aquilina L.2016.Residence time,mineralization processes and groundwater origin within a carbonate coastal aquifer with a thick unsaturated zone[J].Journal of Hydrology,540:50-63.
Su Chen,Cheng Zhongshuang,Wei Wen,Chen Zongyu.2018.Assessing groundwater availability and the response of the groundwater system to intensive exploitation in the North China Plain by analysis of long-term isotopic tracer data[J].Hydrogeology Journal,26(5):1401-1415.
Sun Fangqiang,Yin Lihe,Wang Xiaoyong,Ma Hongyun,Zhang Jun,Dong Jiaqiu,He Shuaijun.2017.Determination of vertical infiltration recharge of groundwater in the thick unsaturated zone of Sangong River Basin,Xinjiang[J].Geology in China,44(5):913-923(in Chinese with English abstract).
Tu Leyi.2015.Analysis of Krypton Gas Dissolved in Groundwater for Radiokrypton Dating[D].Hefei:University of Science and Technology of China(in Chinese with English abstract).
von Rohden,Christoph,Andreas Kreuzer,Chen Zongyu,Rolf Kipfer,Werner Aeschbach-Hertig.2010.Characterizing the Recharge Regime of the Strongly Exploited Aquifers of the North China Plain by Environmental Tracers[J].Water Resources Research,46(5):1-14.
Wang,Fengsheng.1998.The regional recovery model of tritium concentration for meteoric water in jilin Province[J].Jilin Geology,3:75-81(in Chinese with English abstract).
Wang Jiyang,Chen Jiansheng,Chen Baohong,Tong Haibin,Tan Zhongcheng,Sun Yingying.2015.Review and prospect of isotope hydrology[J].Journal of Hohai University,43(5):406-413(in Chinese with English abstract).
Wen Dongguang.2002.Groundwater resources attribute based on environmental isotopes[J].Earth Science,27(2):141-147(in Chinese with English abstract).
Yurtsever Y,Mook W G.2001.Environmental Isotopes in the Hydrological Cycle.Principles and Applications[M].Vienna,27-32.
Zhang Bing.,Song Xianfang,Zhang,Yinghua,Han Dongmei,Yang,Lihu,Tang,Changyuan.2014.Estimation of groundwater renewal rate by tritium and chlorofluorocarbons in Sanjiang plain[J].Journal of Natural Resources,29(11):1859-1868(in Chinese with English abstract).
Zuber A.1986.Mathematical models for the interpretation of environmental radioisotopes in groundwater systems[C]//Handbook of Environmental Isotope Geochemistry,2:1-59.
陈宗宇,齐继祥,张兆吉.2010.北方典型盆地同位素水文地质学方法应用[M].北京:科学出版社.
崔小顺,郑昭贤,程中双,苏晨,李壮,吴宇龙,陈宗宇.2018.穆兴平原北区浅层地下水水化学分布特征及其形成机理[J].南水北调与水利科技,16(4):146-153.
李静,李发东,宋帅,张妍,蔡文静,张芳.2012.CFCs地下水年龄示踪技术的原理、应用及展望[J].生态环境学报,21(8):1503-1508.
刘芳芳.2009.兴凯湖湿地自然保护区生态质量评价[D].哈尔滨:东北林业大学.
刘君.2016.呼和浩特盆地地下水年龄结构与补给流动模式研究[D].北京:中国地质科学院.
柳富田,苏小四,侯光才,林学钰,易树平,董维红.2007.CFCs法在鄂尔多斯白垩系地下水盆地浅层地下水年龄研究中的应用[J].吉林大学学报(地球科学版),37(2):298-302.
秦大军.2005.地下水CFC定年方法及应用[J].地下水,27(6):435-437.
孙芳强,尹立河,王晓勇,马洪云,张俊,董佳秋,贺帅军.2017.新疆三工河流域厚层包气带区地下水垂向补给量的厘定[J].中国地质,44(5):913-923.
涂乐义.2015.地下水溶解氪气分析用于放射性氪同位素测年[D].合肥:中国科学技术大学.
汪集旸,陈建生,陆宝宏,童海滨,谭忠成,孙营营.2015.同位素水文学的若干回顾与展望[J].河海大学学报(自然科学版),43(5):406-413.
王凤生.1998.吉林省大气降水氚浓度恢复的区域模型探讨[J].吉林地质,3:75-81.
文冬光.2002.用环境同位素论区域地下水资源属性[J].地球科学,27(2):141-147.
张兵,宋献方,张应华,韩冬梅,杨丽虎,唐常源.2014.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,29(11):1859-1868.