永定河对北京西山岩溶水和玉泉山泉的影响
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摘要
岩溶介质赋水各向异性使岩溶含水层具有不均一性和复杂性,增加了刻画地下水流场的难度和不确定性。为深入理解岩溶水系统不均一性,基于水化学和同位素数据研究了西山岩溶水系统补径排路径,为厘清岩溶水流场特征提供了新的依据。水化学和同位素证据表明西山岩溶区有3个补给源区:军庄、潭柘寺降水补给区和永定河渗漏补给区,每个补给区各自具有独立的径流通道。军庄补给区为降水和河水补给,降水补给向温泉—永丰屯方向径流;入渗河水补给沿永定河断裂向南东方向径流,在古城一带转向北东方向补给玉泉山泉。潭柘寺降水补给沿八宝山断裂北侧经回民公墓,八宝山朝四季青方向径流。自北而南可分为军庄—永丰屯径流带、永定河—香山径流带、潭柘寺—八宝山—四季青径流带。潭柘寺和永定河是西山岩溶水和重要补给源区,对玉泉山泉有直接影响。
The karst water mixed with infitrated river water shows high Na,Cl and O-18 values and can be used to indicate the distribution of the infiltrated river water in karst aquifers. Individual flow path for three recharge sources was identified in the Xishan karst aquifer in Beijing,China using hydrochemical and isotopic methods. The recharge of rainfall in the Junzhuang area had two flow routes: one flows eastwards to the Yongfengtun; another flows southeastwards along east of the Yongding fault. The recharge of rainfall in Tanzhesi area flows along north of the Babaoshan fault northeastwards Sijiqing. The Yongdingriver infiltrates in the Junzhuang area and flows along the Yongding fault in the direction of southeast and turns to the diction of northeast near Gucheng,along a buried fault which is revealed this time. River water plays an important role in recharge to the karst aquifer and can be used to restore depleted karst flow systems by increasing the flow and infiltration of river water.
The karst water mixed with infitrated river water shows high Na,Cl and O-18 values and can be used to indicate the distribution of the infiltrated river water in karst aquifers. Individual flow path for three recharge sources was identified in the Xishan karst aquifer in Beijing,China using hydrochemical and isotopic methods. The recharge of rainfall in the Junzhuang area had two flow routes: one flows eastwards to the Yongfengtun; another flows southeastwards along east of the Yongding fault. The recharge of rainfall in Tanzhesi area flows along north of the Babaoshan fault northeastwards Sijiqing. The Yongdingriver infiltrates in the Junzhuang area and flows along the Yongding fault in the direction of southeast and turns to the diction of northeast near Gucheng,along a buried fault which is revealed this time. River water plays an important role in recharge to the karst aquifer and can be used to restore depleted karst flow systems by increasing the flow and infiltration of river water.
引文
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AquilinaL,Ladouche B,Dorfliger N.2006.Water storage and transfer in the epikarst of karstic systems during high flow periods[J].Journal of Hydrology,327(3-4):472-485.
Bakalowicz M.2005.Karst groundwater:a challenge for new resources[J].Hydrogeology Journal,13(1):148-160.
Birk S,Liedl R,Sauter M.2004.Identification of localised recharge and conduit flow by combined analysis of hydraulic and physicochemical spring responses(Urenbrunnen,SW-Germany)[J].Journal of Hydrology,286(1-4):179-193.
Brown A L,Martin J B,Screaton E J,et al.2014.Bank storage in karst aquifers:The impact of temporary intrusion of river water on carbonate dissolution and trace metal mobility[J].Chemical Geology,385:56-69.
Chen Y S,Ma Y L.1981.On the recharge of ground-water in Beijing by the Yongding River through western hills[J].Shuili Xuebao,(3):10-18.
Corcho Alvarado J A,Paˇces T,Purtschert R.2013.Dating groundwater in the Bohemian Cretaceous Basin:Understanding tracer variations in the subsurface[J].Applied Geochemistry,29:189-198.
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Hameed A S,Resmi T R,Suraj S,et al.2015.Isotopic characterization and mass balance reveals groundwater recharge pattern in Chaliyar river basin,Kerala,India[J].Journal of Hydrology:Regional Studies,4:48-58.
Hartmann A,Weiler M,Wagener T,et al.2013.Process-based karst modelling to relate hydrodynamic and hydrochemical characteristics to system properties[J].Hydrology&Earth System Sciences,17(8):3305-3321.
Hartmann A,Goldscheider N,Wagener T,et al.2014.Karst water resources in a changing world:Review of hydrological modeling approaches[J].Reviews of Geophysics,52(3):218-242.
Hu C H,Wang Y G.2004.Study on water-sediment optimum allocation in upstream basin and comprehensive measures of sediment control in Guanting reservoir I:Reservoir sedimentation and general plan of water and sediment control[J].Journal of Sediment Research,(2):11-18.
Koeniger P,Margane A,Abi-Rizk J,et al.2017.Stable isotope based mean catchment altitudes of springs in the Lebanon Mountains[J].Hydrological Processes,31(21):3708-3718.
Lakey B,Krothe N C.1996.Stable Isotopic Variation of Storm Discharge from a Perennial Karst Spring,Indiana[J].Water Resources Research,32(32):721-732.
Lang Y C,Liu C Q,Zhao Z Q,et al.2006.Geochemistry of surface and ground water in Guiyang,China:Water/rock interaction and pollution in a karst hydrological system[J].Applied Geochemistry,21(6):887-903.
Li K P,Ma F S,Zhang H X,et al.2017.Recharge sourch identification and evolution of inflowing water in a seabed gold mine[J].Journal of Engineering Geology,25(1):180-189.
Li S L,Liu C Q,Lang Y C,et al.2010.Tracing the sources of nitrate in karstic groundwater in Zunyi,Southwest China:a combined nitrogen isotope and water chemistry approach[J].Environmental Earth Sciences,60(7):1415-1423.
Li X B,Qin D J,Guo Y,et al.2017.Effect of Yufu river on chemical process of karst groundwater in Ji'nan,Shandong province[J].Journal of Engineering Geooogy,25(1):190-198.
Ma R,Wang Y X,Sun Z Y,et al.2011.Geochemical evolution of groundwater in carbonate aquifers in Taiyuan,northern China[J].Applied Geochemistry,26(5):884-897.
Moral F,Cruz-Sanjulin J J,Olías M.2008.Geochemical evolution of groundwater in the carbonate aquifers of Sierra de Segura(Betic Cordillera,southern Spain)[J].Journal of Hydrology,360(1-4):281-296.
Ne'grel Ph,Petelet-Giraud E.2005.Strontium isotopes as tracers of groundwaterinduced floods:The Somme case study(France)[J].Journal of Hydrology,305(1-4):99-119.
Plummer L N,Busenberg E,Mcconnell J B,et al.1998.Flow of river water into a Karstic limestone aquifer.1.Tracing the young fraction in groundwater mixtures in the Upper Floridan Aquifer near Valdosta,Georgia[J].Applied Geochemistry,13(8):995-1015.
Qiao X J,Li G M,Li Y P,et al.2015.Influences of heterogeneity on three-dimensional groundwater flow simulation and wellhead protection area delineation in karst groundwater system,Taiyuan City,Northern China[J].Environmental Earth Sciences,73(10):6705-6717.
Qin D J,Zhao Z F,Guo Y,et al.2017.Using hydrochemical,stable isotope,and river water recharge data to identify groundwater flow paths in a deeply buried karst system[J].Hydrological Processes,31(24):4297-4314.
Qin D J,Zhao Z F,Han L F,et al.2012.Determination of groundwater recharge regime and flowpath in the Lower Heihe River Basin in an arid area of Northwest China by using environmental tracers:Implications for vegetation degradation in the EjinaOasis[J].Applied Geochemistry,27(6):1133-1145.
Qiu S H.1957.The relationship between Yongding River and recharge of ground-water in Beijing[J].Hydrogeology and Engineering Geology,(2):16-18,35.
Rooij R D,Graham W.2017.Generation of complex karstic conduit networks with a hydrochemicalmodel[J].Water Resources Research,53(8):6993-7011.
Scanlon B R.1989.Physical Controls on Hydrochemical Variability in the Inner Bluegrass Karst Region of Central Kentucky a[J].Groundwater,27(5):639-646.
Tang C L,Liang Y P,Han K,et al.2015.Hydrogeological significance of the Jiulongshan-Xiangyu syncline at Yuquanshan sping[J].Carsologica Sinica,31(5):431-437.
Wang X H,Liu W C,Shen Y Y,et al.2011.Analysis on the hydrogeology characteristics and exploitation potential of the emergency karst water source field in Xishan region,Beijing[J].Carsologica Sinica,30(2):216-221.
Wong C I,Mahler B J,MusgroveM,et al.2012.Changes in sources and storage in a karst aquifer during a transition from drought to wet conditions[J].Journal of Hydrology,468-469:159-172.
Zhao C H,Liang Y P,Wang W T,et al.2017.Discussion on the characteristics of karst water systems in the Xishan area of Beijing[J].Carsologica Sinica,36(5):641-647.
陈雨孙,马英林.1981.论永定河水通过西山对北京市地下水的补给[J].水利学报,(3):10-18.
程大珍,陈民,史世平,等.2001.永定河上游人类活动对降雨径流关系的影响[J].水利水电工程设计,20(2):19-21.
郭高轩,刘文臣,辛宝东,等.2011.北京岩溶水勘查开发的现状与思考[J].南水北调与水利科技,9(2):33-36,45.
胡春宏,王延贵.2004.官厅水库流域水沙优化配置与综合治理措施研究Ⅰ---水库泥沙淤积与流域水沙综合治理方略[J].泥沙研究,(2):11-18.
李宝学,秦大军,郭艺,等.2017.玉符河对济南岩溶水化学过程的影响研究[J].工程地质学报,25(1):190-198.
李克蓬,马凤山,张洪训,等.2017.海底金矿矿坑涌水水源判识及演化研究[J].工程地质学报,25(1):180-189.
邱树杭.1957.试论永定河与北京市地下水的补给关系[J].水文地质工程地质,(2):16-18,35.
唐春雷,梁永平,韩凯,等.2015.玉泉山泉九龙山-香峪向斜的水文地质意义[J].中国岩溶,(5):431-437.
王晓红,刘文臣,沈媛媛,等.2011.北京西山岩溶水应急水源地水文地质特征及开采潜力分析[J].中国岩溶,30(2):216-221.
赵春红,梁永平,王维泰,等.2017.北京西山泉域岩溶水系统特征探讨[J].中国岩溶,36(5):641-647.
AquilinaL,Ladouche B,Dorfliger N.2006.Water storage and transfer in the epikarst of karstic systems during high flow periods[J].Journal of Hydrology,327(3-4):472-485.
Bakalowicz M.2005.Karst groundwater:a challenge for new resources[J].Hydrogeology Journal,13(1):148-160.
Birk S,Liedl R,Sauter M.2004.Identification of localised recharge and conduit flow by combined analysis of hydraulic and physicochemical spring responses(Urenbrunnen,SW-Germany)[J].Journal of Hydrology,286(1-4):179-193.
Brown A L,Martin J B,Screaton E J,et al.2014.Bank storage in karst aquifers:The impact of temporary intrusion of river water on carbonate dissolution and trace metal mobility[J].Chemical Geology,385:56-69.
Chen Y S,Ma Y L.1981.On the recharge of ground-water in Beijing by the Yongding River through western hills[J].Shuili Xuebao,(3):10-18.
Corcho Alvarado J A,Paˇces T,Purtschert R.2013.Dating groundwater in the Bohemian Cretaceous Basin:Understanding tracer variations in the subsurface[J].Applied Geochemistry,29:189-198.
Ford D,Williams P D.2007.Karst hydrogeology and geomorphology[M].John Wiley&Sons Ltd.
Guo G X,Liu W C,Xin B D,et al.2011.Current situations and discussions on karst groundwater resources exploration in Beijing[J].South-to-North Water Diversion and Water Science&Technology,9(2):33-36,45.
Hameed A S,Resmi T R,Suraj S,et al.2015.Isotopic characterization and mass balance reveals groundwater recharge pattern in Chaliyar river basin,Kerala,India[J].Journal of Hydrology:Regional Studies,4:48-58.
Hartmann A,Weiler M,Wagener T,et al.2013.Process-based karst modelling to relate hydrodynamic and hydrochemical characteristics to system properties[J].Hydrology&Earth System Sciences,17(8):3305-3321.
Hartmann A,Goldscheider N,Wagener T,et al.2014.Karst water resources in a changing world:Review of hydrological modeling approaches[J].Reviews of Geophysics,52(3):218-242.
Hu C H,Wang Y G.2004.Study on water-sediment optimum allocation in upstream basin and comprehensive measures of sediment control in Guanting reservoir I:Reservoir sedimentation and general plan of water and sediment control[J].Journal of Sediment Research,(2):11-18.
Koeniger P,Margane A,Abi-Rizk J,et al.2017.Stable isotope based mean catchment altitudes of springs in the Lebanon Mountains[J].Hydrological Processes,31(21):3708-3718.
Lakey B,Krothe N C.1996.Stable Isotopic Variation of Storm Discharge from a Perennial Karst Spring,Indiana[J].Water Resources Research,32(32):721-732.
Lang Y C,Liu C Q,Zhao Z Q,et al.2006.Geochemistry of surface and ground water in Guiyang,China:Water/rock interaction and pollution in a karst hydrological system[J].Applied Geochemistry,21(6):887-903.
Li K P,Ma F S,Zhang H X,et al.2017.Recharge sourch identification and evolution of inflowing water in a seabed gold mine[J].Journal of Engineering Geology,25(1):180-189.
Li S L,Liu C Q,Lang Y C,et al.2010.Tracing the sources of nitrate in karstic groundwater in Zunyi,Southwest China:a combined nitrogen isotope and water chemistry approach[J].Environmental Earth Sciences,60(7):1415-1423.
Li X B,Qin D J,Guo Y,et al.2017.Effect of Yufu river on chemical process of karst groundwater in Ji'nan,Shandong province[J].Journal of Engineering Geooogy,25(1):190-198.
Ma R,Wang Y X,Sun Z Y,et al.2011.Geochemical evolution of groundwater in carbonate aquifers in Taiyuan,northern China[J].Applied Geochemistry,26(5):884-897.
Moral F,Cruz-Sanjulin J J,Olías M.2008.Geochemical evolution of groundwater in the carbonate aquifers of Sierra de Segura(Betic Cordillera,southern Spain)[J].Journal of Hydrology,360(1-4):281-296.
Ne'grel Ph,Petelet-Giraud E.2005.Strontium isotopes as tracers of groundwaterinduced floods:The Somme case study(France)[J].Journal of Hydrology,305(1-4):99-119.
Plummer L N,Busenberg E,Mcconnell J B,et al.1998.Flow of river water into a Karstic limestone aquifer.1.Tracing the young fraction in groundwater mixtures in the Upper Floridan Aquifer near Valdosta,Georgia[J].Applied Geochemistry,13(8):995-1015.
Qiao X J,Li G M,Li Y P,et al.2015.Influences of heterogeneity on three-dimensional groundwater flow simulation and wellhead protection area delineation in karst groundwater system,Taiyuan City,Northern China[J].Environmental Earth Sciences,73(10):6705-6717.
Qin D J,Zhao Z F,Guo Y,et al.2017.Using hydrochemical,stable isotope,and river water recharge data to identify groundwater flow paths in a deeply buried karst system[J].Hydrological Processes,31(24):4297-4314.
Qin D J,Zhao Z F,Han L F,et al.2012.Determination of groundwater recharge regime and flowpath in the Lower Heihe River Basin in an arid area of Northwest China by using environmental tracers:Implications for vegetation degradation in the EjinaOasis[J].Applied Geochemistry,27(6):1133-1145.
Qiu S H.1957.The relationship between Yongding River and recharge of ground-water in Beijing[J].Hydrogeology and Engineering Geology,(2):16-18,35.
Rooij R D,Graham W.2017.Generation of complex karstic conduit networks with a hydrochemicalmodel[J].Water Resources Research,53(8):6993-7011.
Scanlon B R.1989.Physical Controls on Hydrochemical Variability in the Inner Bluegrass Karst Region of Central Kentucky a[J].Groundwater,27(5):639-646.
Tang C L,Liang Y P,Han K,et al.2015.Hydrogeological significance of the Jiulongshan-Xiangyu syncline at Yuquanshan sping[J].Carsologica Sinica,31(5):431-437.
Wang X H,Liu W C,Shen Y Y,et al.2011.Analysis on the hydrogeology characteristics and exploitation potential of the emergency karst water source field in Xishan region,Beijing[J].Carsologica Sinica,30(2):216-221.
Wong C I,Mahler B J,MusgroveM,et al.2012.Changes in sources and storage in a karst aquifer during a transition from drought to wet conditions[J].Journal of Hydrology,468-469:159-172.
Zhao C H,Liang Y P,Wang W T,et al.2017.Discussion on the characteristics of karst water systems in the Xishan area of Beijing[J].Carsologica Sinica,36(5):641-647.
陈雨孙,马英林.1981.论永定河水通过西山对北京市地下水的补给[J].水利学报,(3):10-18.
程大珍,陈民,史世平,等.2001.永定河上游人类活动对降雨径流关系的影响[J].水利水电工程设计,20(2):19-21.
郭高轩,刘文臣,辛宝东,等.2011.北京岩溶水勘查开发的现状与思考[J].南水北调与水利科技,9(2):33-36,45.
胡春宏,王延贵.2004.官厅水库流域水沙优化配置与综合治理措施研究Ⅰ---水库泥沙淤积与流域水沙综合治理方略[J].泥沙研究,(2):11-18.
李宝学,秦大军,郭艺,等.2017.玉符河对济南岩溶水化学过程的影响研究[J].工程地质学报,25(1):190-198.
李克蓬,马凤山,张洪训,等.2017.海底金矿矿坑涌水水源判识及演化研究[J].工程地质学报,25(1):180-189.
邱树杭.1957.试论永定河与北京市地下水的补给关系[J].水文地质工程地质,(2):16-18,35.
唐春雷,梁永平,韩凯,等.2015.玉泉山泉九龙山-香峪向斜的水文地质意义[J].中国岩溶,(5):431-437.
王晓红,刘文臣,沈媛媛,等.2011.北京西山岩溶水应急水源地水文地质特征及开采潜力分析[J].中国岩溶,30(2):216-221.
赵春红,梁永平,王维泰,等.2017.北京西山泉域岩溶水系统特征探讨[J].中国岩溶,36(5):641-647.