马瑞;董启明;孙自永;郑春苗;

• 1:中国地质大学环境学院
• 2:北京大学工学院水资源研究中心

摘要(Abstract)：

刻画地表水与地下水的相互作用过程及精确计算二者的交换量始终是个挑战,而新兴的温度示踪方法对于这方面的研究具有独特优势。重点介绍了地表水与地下水相互作用的温度示踪方法原理、应用及相关模拟的研究进展。温度示踪方法的数据获取成本低且温度适宜密集与连续监测,可对地表水与地下水相互作用过程进行精细刻画;在进行地表水与地下水相互作用的水-热耦合模拟时,温度数据可用于进一步校正模型,降低模型的不确定性,以提高交换量的计算精度。监测河水温度和河床沉积物内的水温,运用温度示踪方法研究河水与地下水的相互作用过程,并将水流及热运移数值模型相耦合,利用多源数据进行模型校正,可精细刻画地表水与地下水的交换量、相互作用带内的水流途径、流速及其变化趋势和控制因素,为地表水与地下水相互作用研究提供新的模型与方法。

关键词(KeyWords)： 地表水与地下水相互作用;温度示踪;水-热耦合模拟;模型校正

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金项目(41002081;91125009)

作者(Author): 马瑞;董启明;孙自永;郑春苗;

Email:

DOI:

参考文献(References)：

• [1]Edwardson K J,Bowden W B,Dahm C,et al.The hydrauliccharacteristics and geochemistry of hyporheic and parafluvialzones in Arctic tundra streams,north slope,Alaska[J].Ad-vances in Water Resources,2003,26:907-923.
• [2]Salehin M,Packman A I,Paradis M.Hyporheic exchangewith heterogeneous streambeds:Laboratory experiments andmodeling[J/OL].Water Resources Research,2004,40:W11504,doi:10.1029/2003WR002567.
• [3]滕彦国,左锐,王金生.地表水—地下水的交错带及其生态功能[J].地球与环境,2007,35(1):1-8.
• [4]Sophocleous M.Interactions between groundwater and surfacewater:The state of the science[J].Hydrogeology Journal,2002,10:52-67.
• [5]Kalbus E,Reinstorf F,Schirmer M.Measuring methods forgroundwater,surface water and their interactions:A review[J].Hydrology and Earth Systems Sciences,2006,3:1809-1850.
• [6]Paulsen R J,Smith C F,O’Rourke D,et al.Development andevaluation of an ultrasonic ground water seepage meter[J].Ground Water,2001,39(6):904-911.
• [7]Landon M K,Rus D L,Harvey F E.Comparison of instreammethods for measuring hydraulic conductivity in sandy stre-ambeds[J].Ground Water,2001,39(6):870-885.
• [8]Rutledge A T.Methods of using streamflowrecords for esti-mating total and effective recharge in the Appalachian Valleyand Ridge,Piedmont,and Blue Ridge physiographic provinces[J].Water Resources,1992,17:59-73.
• [9]Christensen S,Rasmussen K R,Moller K.Prediction of re-gional ground water flow to streams[J].Ground Water,1998,36(2):351-360.
• [10]Otz M H,Otz H K,Otz I,et al.Surface water/groundwaterinteraction in the Piora Aquifer,Switzerland:Evidence fromdye tracing tests[J].Hydrogeology Journal,2003,11:228-239.
• [11]Négrel Ph,Petelet-Giraud E.Strontium isotopes as tracers ofgroundwater-induced floods:The Somme case study(France)[J].Journal of Hydrology,2005,305:99-119.
• [12]Constantz J,Cox M H,Su G W.Comparison of heat andbromide as ground water tracers near streams[J].GroundWater,2003,41(5):647-656.
• [13]陈崇希,裴顺平,王逊.非完整河的数值模拟方法及建模中的若干问题[J].勘察科学技术,1999(4):3-6.
• [14]Parkin G,Birkinshaw S J,Younger P L,et al.A numericalmodelling and neural network approach to estimate the impactof groundwater abstractions on river flows[J].Journal of Hy-drology,2007,339:15-28.
• [15]Constantz J.Heat as a tracer to determine streambed waterexchanges[J/OL].Water Resources Research,2008,44:W00D10,doi:10.1029/2008WR006996.
• [16]Anderson M P.Heat as a ground water tracer[J].GroundWater,2005,43(6):951-968.
• [17]Constantz J E.Interaction between stream temperature,stre-amflow,and groundwater exchanges in alpine streams[J].Water Resources Research,1998,34(7):1609-1615.
• [18]Stonestrom D A,Constantz J.Heat as a tool for studying themovement of ground water near streams[R].[S.l.]:U.S.Geological Survey Circular 1260,U.S.Geological Survey,Re-ston,Virginia,2003.
• [19]Bartolino J R.The Rio Grande-Competing demands for a des-ert river[R]∥Stonestrom D A,Constantz J.Heat as a tool forstudying the movement of ground water near streams.USGSCircular 1260.Reston,Virginia:USGS,2003:8-16.
• [20]Bartolino J R,Niswonger R G.Numerical simulation of verti-cal ground-water flux of the Rio Grande from ground-watertemperature profiles,central New Mexico.Water ResourcesInvestigation Report 99-4212,1999[R].Albuquerque,NewMexico:USGS,1999.
• [21]Constantz J,Stewart A E,Niswonger R,et al.Analysis oftemperature profiles for investigating stream losses beneath e-phemeral channels[J/OL].Water Resources Research,2002,38(12):1316,doi:10.1029/2001WR001221.
• [22]Rorabaugh M I.Streambed percolation in development of wa-ter supplies[R].Washington,DC.U.S.Geological SurveyGroundwater Notes on Hydraulics,1954,25:13.
• [23]Winslow J D.Effect of stream infiltration on ground watertemperatures near Schenectady.N.Y.USGS Professional Pa-per,450-C[R].Washington,DC:USGS.1962.
• [24]Schneider R.Distortion of the geothermal field in aquifers bypumping.Professional Paper,800-C[R].Washington,DC:USGS.1972.
• [25]Andrews C B,Anderson M P.Thermal alteration of groundw-ater caused by seepage from a cooling lake[J].Water Re-sources Research,1979,15(3):595-602.
• [26]Lee D R.Method for locating sediment anomalies in lake bedsthat can be caused by groundwater inflow[J].Journal of Hy-drology,1985,79(1/2):187-193.
• [27]Silliman S E,Booth D F.Analysis of time-series measure-ments of sediment temperature for identification of gaining vs.losing portions of Juday Creek,Indiana[J].Journal of Hy-drology,1993,146:131-148.
• [28]Allander K K.Trout creek-evaluating ground-water and sur-face water exchange along an alpine stream,Lake Tahoe,Cali-fornia[R]∥Stonestrom D A,Constantz J.Heat as a tool forstudying the movement of ground water near streams.USGSCircular 1260.Reston,Virginia:USGS,2003:35-45.
• [29]Cox M H,Su G W,Constantz J.Heat,chloride,and specificconductance as ground water tracers near streams[J].GroundWater,2007,45(2):187-195.
• [30]Storey R G,Howard K W F,Williams D D.Factors control-ling riffle-scale hyporheic exchange flows and their seasonalchanges in a gaining stream:A three-dimensional groundwaterflow model[J].Water Resources Research,2003,39(2):1034.
• [31]Conant B.Delineating and quantifying groundwater dischargezones using streambed temperatures[J].Ground Water,2004,42(2):243-257.
• [32]Salem Z E,Taniguchi M,Sakura Y.Use of temperature pro-files and stable isotopes to trace flow lines:Nagaoka Area,Ja-pan[J].Ground Water,2004,42(1):83-91.
• [33]李端有,陈鹏霄,王志旺.温度示踪法渗流监测技术在长江堤防渗流监测中的应用初探[J].长江科学院院报,2000,17(4):48-51.
• [34]陈建生,余波,陈亮.利用地下水温度场研究江都高水河船厂堤防的渗漏[J].岩土工程界,2002,5(12):37-39.
• [35]董海洲,陈建生.利用温度示踪方法探测基坑渗漏[J].岩土力学与工程学报,2004,23(12):2085-2090.
• [36]王新建,曾长女,许保田,等.基于温度场反分析的堤坝多个集中渗漏通道探测方法[J].水利学报,2009,40(4):486-491.
• [37]葛建.分布式光纤测温系统在探测堤坝渗漏中的应用[J].中国水利,2008,12:62-63.
• [38]黄丽,郑春苗,刘杰,等.分布式光纤测温技术在黑河中游地表水与地下水转换研究中的应用[J].水文地质工程地质,2012,39(2):1-6.
• [39]Suzuki S.Percolation measurements based on heat flowthrough soil with special reference to paddy fields[J].Journalof Geophysical Research,1960,65:2883-2885.
• [40]Stallman R W.Steady one-dimensional fluid flow in a semi-in-finite porous medium with sinusoidal surface temperature[J].Journal of Geophysical Research,1965,70(12):2821-2827.
• [41]Bredehoeft J D,Papadopulos I S.Rates of vertical groundwa-ter movement estimated from the Earth’s thermal profile[J].Water Resources Research,1965,1(2):325-328.
• [42]Silliman S E,Ramirez J,McCabe R L.Quantifying downflowthrough creek sediments using temperature time series:One-dimensional solution incorporating measured surface tempera-ture[J].Journal of Hydrology,1995,167(1/4):99-119.
• [43]Becker M W,Georgian T,Ambrose H,et al.Estimating flowand flux of ground water discharge using water temperatureand velocity[J].Journal of Hydrology,2004,296:221-233.
• [44]Hatch C E,Fisher A T,Revenaugh J S,et al.Quantifyingsurface water-groundwater interactions using time series analy-sis of streambed thermal records:Method development[J/OL].Water Resources Research,2006,42:W10410,doi:10.1029/2005WR004787.
• [45]Keery J,Binley A,Crook N,et al.Temporal and spatial vari-ability of groundwater-surface water fluxes:Development andapplication of an analytical method using temperature time se-ries[J].Journal of Hydrology,2007,336:1-16.
• [46]Vogt T,Schneider P,Hahn-Woernle L,et al.Estimation ofseepage rates in a losing stream by means of fiber-optic high-resolution vertical temperature profiling[J].Journal of Hy-drology,2010,380:154-164.
• [47]Lautz L K,Ribaudo R E.Scaling up point-in-space heat trac-ing of seepage flux using bed temperatures as a quantitativeproxy[J].Hydrogeology Journal,2012,doi 10.1007/s10040-012-0870-2.
• [48]Thomas C L,Stewart A E S,Constantz J.Comparison ofmethods to determine infiltration rates along a reach of theSanta Fe River near La Bajada,New Mexico[R].NewMexico:U.S.Geol.Surv.Water Resour.,2000,Invest.Rep.,00-4141:1-65.
• [49]Burow K R,Constantz J,Fujii R.Heat as a tracer to examinedissolved organic carbon flux from an restored wetland[J].Ground Water,2005,43(4):545-556.
• [50]Su G W,Jasperse J,Seymour D,et al.Analysis of pumping-induced unsaturated regions beneath a perennial river[J/OL].Water Resources Research,2007,43:W08421,doi:10.1029/2006WR005389.
• [51]Briggs M A,Lautz L K,McKenzie J M,et al.Using high-reso-lution distributed temperature sensing to quantify spatial andtemporal variability in vertical hyporheic flux[J].Water Re-sources Research,2012,48:W02527,doi:10.1029/2011WR011227.
• [52]van Duin R H A.The influence of management on the temper-ature wave near the surface[R].Wageningen,Netherlands:Wageningen Institute of Land and Water Management,Tech-nical Bulletin No.29,1963:21.
• [53]Freeze R A,Cherry J A.Ground water[M].[S.l.]:Pren-tice-Hall,Upper Saddle River,N.J.,1979:604.
• [54]Constantz J.Temperature dependence of unsaturated hydraulicconductivity of two soils[J].Soil Sci.Soc.Am.J.,1982,26:466-470.
• [55]Ma R,Zheng C,Zachara J M,et al.Utility of bromide andheat tracers for aquifer characterization affected by highly tran-sient flow conditions[J/OL].Water Resources Research,2012,48:W08523,doi:10.1029/2011WR011281.
• [56]Bravo H R,Feng J,Hunt R J.Using groundwater tempera-ture data to constrain parameter estimation in a groundwaterflow model of a wetland system[J/OL].Water Resources Re-search,2002,38(8):doi:10.1029/2000WR000172.
• [57]Jiang Y,Woodbury A D.A full-Bayesian approach to the in-verse problem for steady-state groundwater flow and heattransport[J].Geophys.J.Int,2006,167:1501-1512.
• [58]Gerecht K E,Cardenas M B,Guswa A J,et al.Dynamics ofhyporheic flow and heat transport across a bed-to-bank contin-uum in a large regulated river[J/OL].Water Resources Re-search,2011,47,W03524,doi:10.1029/2010WR009794.