地表水和地下水相互作用及集成模型研究
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摘要
本文在总结国内外地表水和地下水相互作用研究的热点问题的基础上,归纳了定量计算的基本方法,评述了国内外主要的集成模型并对其进行了分类;认为集成模型应该解决时空尺度整合、参数的不确定性等关键问题,指出综合水循环各组成部分的复杂系统模型是模型发展的必然趋势。
Focusing on the key issues of interactions between surface water and groundwater,this paper generalized the main research methods of quantification,summarized and classified the existing integrated models,and pointed out the key problems to be addressed such as coupling of temporal/spatial scale and parameter uncertainty.The paper concluded that a complicated system model combining all the components in water cycle is the present trend of integrated models development.
Focusing on the key issues of interactions between surface water and groundwater,this paper generalized the main research methods of quantification,summarized and classified the existing integrated models,and pointed out the key problems to be addressed such as coupling of temporal/spatial scale and parameter uncertainty.The paper concluded that a complicated system model combining all the components in water cycle is the present trend of integrated models development.
引文
[1]Woessner W W.Stream and fluvial plain ground water interactions:Rescaling hydrogeologic thought[J].Ground Water,2000,38(3):423-429.
[2]Sophocleous M.Interactions between groundwater and surface water:The state of the science[J].Hydrogeology Journal,2002,10(1):52-67.
[3]Winter T C.Recent advances in understanding the interaction of groundwater and surface water[J].Review ofGeophysics,1995,33:985-994.
[4]籍传茂,侯景岩,王兆馨.世界各国地下水开发和国际合作指南[M].北京:地震出版社,1996.
[5]陈建生,汪集,赵霞,盛雪芬,等.用同位素方法研究额济纳盆地承压含水层地下水的补给[J].地质论评,2004,50(6):649-658.
[6]崔亚莉,邵景力,李慈君.玛纳斯河地表水、地下水转化关系研究[J].水文地质工程地质,2001,2:9-13.
[7]李如忠,汪家权,王超,等.不确定性信息下的河流纳污能力计算初探[J].水科学进展,2003,14(4):459-463.
[8]杨志峰,刘静玲,肖芳,等.海河流域河流生态基流量整合计算[J].环境科学学报,2005,25(4):442-448.
[9]Nobi N,DasGupta A.Simulation of regional flow and salinity intrusion in an integrated stream-aquifer system in coastalregion:southwest region of bangladesh[J].Ground water,1997,35(5):786-796.
[10]袁道先.岩溶作用对环境变化的敏感性及其记录[J].科学通报,1995,40(13):1210-1213.
[11]Lan Y C,Kang E S,Zhang J S,et al.Study on the mutual transformation between groundwater and surface waterresources in the Hexi inland arid regions[J].地球科学进展,2002,17(4):535-545.
[12]宫辉力,尹连旺,赵文吉,等.基于GIS技术的浅层地下水硝酸盐氮浓度场数值仿真[J].系统仿真学报,2004,16(6):1254-1256.
[13]成小英,李世杰.长江中下游典型湖泊营养化演变过程及其特征分析[J].科学通报,2006,51(7):848-855.
[14]Chen C X,Hu L T.Analytical solution of well fields disturbance in confined-unconfined steady groundwater pumping flow[A].In:Proceedings of the 2003 International Symposium on Water Resources and the Urban Environment[C].Wuhan,China,China Environmental Science Press,2003.41-45.
[15]Fleckmenstein J,Anderson M,Fogg G,et al.Managing surface water-groundwater to restore fall flows in the cosumnesriver[J].Journal of water resources planning and management,2004,130(4):301-310.
[16]谢新民,陈守煜,王本德.地表-地下水资源系统多目标管理模型与模型决策研究[J].大连理工大学学报,1994,34(2):240-248.
[17]Hamada H.Analysis of the interaction between surface water and groundwater using Radon-222[J].Jarq-Japanagricultural research quarterly,1999,33(4):261-265.
[18]顾正华,唐洪武,李云,等.水流模拟智能化问题的探讨[J].水科学进展,2004,15(1):129-133.
[19]高飞,张元禧.河西走廊内陆石羊河流域水资源转化模型及其时移转化关系[J].水利学报,1995,(11):77-83.
[20]武强,孔庆友,张自忠,等.地表河网-地下水系统耦合模拟Ⅰ:模型[J].水利学报,2005,36(5):588-592,597.
[21]武强,徐军祥,张自忠,等.地表河网-地下水系统耦合模拟Ⅱ:应用实例[J].水利学报,2005,36(6):754-758.
[22]McDonald M G,Harbaugh A W.A modular three-dimensional finite difference ground-water flow model,U.S.GeologicalSurvey[M].Techniques of water resources Investigations,USA:USGS,1988.
[23]Jobson H E,Harbaugh A W.Modifications to the diffusion analogy surface-water flow model(DAFLOW)for coupling tothe modular finite-difference ground-water flow model(MODFLOW)[R].U.S.Geological Survey Open-File Report,1999.
[24]Swain E D.Implementation and use of direct-flow connections in a coupled ground-water and surface-water model[J].Ground Water,1994,32(1):139-144.
[25]Swain E D,Wexler E J.A coupled surface-water and ground-water flow model(MODBRANCH)for simulation of stream-aquifer interaction[M].Techniques of Water-Resources Investigations of the U.S.Geological Survey,1999.
[26]Sophocleous M A,Koelliker J K,Govindaraju R S,et al.Integrated numerical modeling for basin-wide watermanagement:The case of the Rattlesnake Creek basin in south-central Kansas[J].Journal of Hydrology,1999,214(1-4):179-196.
[27]Sophocleous M A,Perkins S P.Methodology and application of combined watershed and groundwater models in Kansas[J].Journal of Hydrology,2000,236(3-4):185-201.
[28]Labolle E M,Ahmed A A,Fogg G E.Review of the integrated groundwater and surface-water model(IGSM)[J].Groundwater,2003,41(2):238-246.
[29]Panday S,Huyakorn P S.A fully coupled physically-based spatially-distributed model for evaluating surface/subsurfaceflow[J].Advances in Water Resources,2004,27(4):361-382.
[30]Al-Thani A A,Beaven R P.White J.K.,Modelling flow to leachate wells in landfills[J].Waste Management,2004,24(3):271-276.
[31]贾仰文,王浩,倪广恒,等.分布式流域水文模型原理与实践[M].北京:中国水利水电出版社,2005.
[32]Quemer E P.Description and application of the combined surface and groundwater flow model MOGROW[J].Journal ofHydrology,1997,192(1-4):158-188.
[33]Refsgarrd J C.Parameterisation,calibration and validation of distributed hydrological models[J].Journal of Hydrology,1997,198(1-4):69-97.
[34]Andersen J,Refsgaard J C,Jensen K H.Distributed hydrological modelling of the Senegal River Basin:modelconstruction and validation[J].Journal of Hydrology,2001,247(3-4):200-214.
[2]Sophocleous M.Interactions between groundwater and surface water:The state of the science[J].Hydrogeology Journal,2002,10(1):52-67.
[3]Winter T C.Recent advances in understanding the interaction of groundwater and surface water[J].Review ofGeophysics,1995,33:985-994.
[4]籍传茂,侯景岩,王兆馨.世界各国地下水开发和国际合作指南[M].北京:地震出版社,1996.
[5]陈建生,汪集,赵霞,盛雪芬,等.用同位素方法研究额济纳盆地承压含水层地下水的补给[J].地质论评,2004,50(6):649-658.
[6]崔亚莉,邵景力,李慈君.玛纳斯河地表水、地下水转化关系研究[J].水文地质工程地质,2001,2:9-13.
[7]李如忠,汪家权,王超,等.不确定性信息下的河流纳污能力计算初探[J].水科学进展,2003,14(4):459-463.
[8]杨志峰,刘静玲,肖芳,等.海河流域河流生态基流量整合计算[J].环境科学学报,2005,25(4):442-448.
[9]Nobi N,DasGupta A.Simulation of regional flow and salinity intrusion in an integrated stream-aquifer system in coastalregion:southwest region of bangladesh[J].Ground water,1997,35(5):786-796.
[10]袁道先.岩溶作用对环境变化的敏感性及其记录[J].科学通报,1995,40(13):1210-1213.
[11]Lan Y C,Kang E S,Zhang J S,et al.Study on the mutual transformation between groundwater and surface waterresources in the Hexi inland arid regions[J].地球科学进展,2002,17(4):535-545.
[12]宫辉力,尹连旺,赵文吉,等.基于GIS技术的浅层地下水硝酸盐氮浓度场数值仿真[J].系统仿真学报,2004,16(6):1254-1256.
[13]成小英,李世杰.长江中下游典型湖泊营养化演变过程及其特征分析[J].科学通报,2006,51(7):848-855.
[14]Chen C X,Hu L T.Analytical solution of well fields disturbance in confined-unconfined steady groundwater pumping flow[A].In:Proceedings of the 2003 International Symposium on Water Resources and the Urban Environment[C].Wuhan,China,China Environmental Science Press,2003.41-45.
[15]Fleckmenstein J,Anderson M,Fogg G,et al.Managing surface water-groundwater to restore fall flows in the cosumnesriver[J].Journal of water resources planning and management,2004,130(4):301-310.
[16]谢新民,陈守煜,王本德.地表-地下水资源系统多目标管理模型与模型决策研究[J].大连理工大学学报,1994,34(2):240-248.
[17]Hamada H.Analysis of the interaction between surface water and groundwater using Radon-222[J].Jarq-Japanagricultural research quarterly,1999,33(4):261-265.
[18]顾正华,唐洪武,李云,等.水流模拟智能化问题的探讨[J].水科学进展,2004,15(1):129-133.
[19]高飞,张元禧.河西走廊内陆石羊河流域水资源转化模型及其时移转化关系[J].水利学报,1995,(11):77-83.
[20]武强,孔庆友,张自忠,等.地表河网-地下水系统耦合模拟Ⅰ:模型[J].水利学报,2005,36(5):588-592,597.
[21]武强,徐军祥,张自忠,等.地表河网-地下水系统耦合模拟Ⅱ:应用实例[J].水利学报,2005,36(6):754-758.
[22]McDonald M G,Harbaugh A W.A modular three-dimensional finite difference ground-water flow model,U.S.GeologicalSurvey[M].Techniques of water resources Investigations,USA:USGS,1988.
[23]Jobson H E,Harbaugh A W.Modifications to the diffusion analogy surface-water flow model(DAFLOW)for coupling tothe modular finite-difference ground-water flow model(MODFLOW)[R].U.S.Geological Survey Open-File Report,1999.
[24]Swain E D.Implementation and use of direct-flow connections in a coupled ground-water and surface-water model[J].Ground Water,1994,32(1):139-144.
[25]Swain E D,Wexler E J.A coupled surface-water and ground-water flow model(MODBRANCH)for simulation of stream-aquifer interaction[M].Techniques of Water-Resources Investigations of the U.S.Geological Survey,1999.
[26]Sophocleous M A,Koelliker J K,Govindaraju R S,et al.Integrated numerical modeling for basin-wide watermanagement:The case of the Rattlesnake Creek basin in south-central Kansas[J].Journal of Hydrology,1999,214(1-4):179-196.
[27]Sophocleous M A,Perkins S P.Methodology and application of combined watershed and groundwater models in Kansas[J].Journal of Hydrology,2000,236(3-4):185-201.
[28]Labolle E M,Ahmed A A,Fogg G E.Review of the integrated groundwater and surface-water model(IGSM)[J].Groundwater,2003,41(2):238-246.
[29]Panday S,Huyakorn P S.A fully coupled physically-based spatially-distributed model for evaluating surface/subsurfaceflow[J].Advances in Water Resources,2004,27(4):361-382.
[30]Al-Thani A A,Beaven R P.White J.K.,Modelling flow to leachate wells in landfills[J].Waste Management,2004,24(3):271-276.
[31]贾仰文,王浩,倪广恒,等.分布式流域水文模型原理与实践[M].北京:中国水利水电出版社,2005.
[32]Quemer E P.Description and application of the combined surface and groundwater flow model MOGROW[J].Journal ofHydrology,1997,192(1-4):158-188.
[33]Refsgarrd J C.Parameterisation,calibration and validation of distributed hydrological models[J].Journal of Hydrology,1997,198(1-4):69-97.
[34]Andersen J,Refsgaard J C,Jensen K H.Distributed hydrological modelling of the Senegal River Basin:modelconstruction and validation[J].Journal of Hydrology,2001,247(3-4):200-214.
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