A numerical model for estimating groundwater flux from subsurface temperature profiles

Hydrological Processes

Volumn 21, Issue 25, 2007, Pages 3440-3448

  Keshari, Ashok K ^a   Koo, Min Ho ^b  

^a INDIAN INSTITUTE OF TECHNOLOGY DELHI   (India)

^b Kongju National University   (South Korea)

Author keywords

Groundwater modelling; Groundwater recharge; Heat transport; Numerical model; Subsurface temperature

Indexed keywords

CORRELATION METHODS; FINITE DIFFERENCE METHOD; MATHEMATICAL MODELS; PARTIAL DIFFERENTIAL EQUATIONS; RECHARGING (UNDERGROUND WATERS); SENSITIVITY ANALYSIS; TEMPERATURE DISTRIBUTION;

CORRELATION COEFFICIENT; GROUNDWATER FLUX; SUBSURFACE TEMPERATURE;

GROUNDWATER FLOW;

CORRELATION METHODS; FINITE DIFFERENCE METHOD; GROUNDWATER FLOW; MATHEMATICAL MODELS; PARTIAL DIFFERENTIAL EQUATIONS; RECHARGING (UNDERGROUND WATERS); SENSITIVITY ANALYSIS; TEMPERATURE DISTRIBUTION;

BOUNDARY CONDITION; CLIMATE CHANGE; CONVECTION; CORRELATION; DIFFUSION; FINITE DIFFERENCE METHOD; GROUNDWATER FLOW; HEAT TRANSFER; HYDROLOGICAL MODELING; NUMERICAL MODEL; SENSITIVITY ANALYSIS; SUBSURFACE FLOW; TEMPERATURE PROFILE; WATER TEMPERATURE;

ASIA; EURASIA; FAR EAST; JAPAN;

EID: 34548107383     PISSN: 08856087     EISSN: 10991085     Source Type: Journal    
DOI: 10.1002/hyp.6577     Document Type: Article

References (30)

1. Boyle JM, Saleem ZA. 1979. Determination of recharge rates using temperature depth profiles in wells. Water Resources Research 15(6): 1616-1622.
2. Bredehoeft JD, Papadopulos IS. 1965. Rates of vertical groundwater movement estimated from earth's thermal profile. Water Resources Research 1(2): 325-328.
3. Cartwright K. 1970. Groundwater discharge in the Illinois basin as suggested by temperature anomalies. Water Resources Research 6: 912-918.
4. Cartwright K. 1979. Measurement of fluid velocity using temperature profiles: experimental verification. Journal of Hydrology 43: 185-194.
5. Constantz J, Tyler SW, Kwicklis E. 2003. Temperature-profile methods for estimating percolation rates in arid environments. Vadose Zone Hydrology 2: 12-24.
6. Healy RW, Ronan AD. 1996. Documentation of the Computer Program VS2DH for Simulation of Energy Transport in Variably Saturated Porous Media-Modification of the US Geol Survey's Computer Program VS2DT. Water Resources Investigation Report 96-4230, US Geological Survey.
7. Hoffman JD. 1992. Numerical Methods for Engineers and Scientists. McGraw-Hill: New York.
8. Jessop AM, Vigrass IW. 1989. Geothermal measurements in a deep well at Regina, Saskatchewan. Journal of Volcanology and Geothermal Research 37: 151-166.
9. Keshari AK. 1997. Review of groundwater assessment methodology. In Hydrologic Analysis of UP Sodic Land Reclamation Project-Part II. Technical Report by Mott McDonald in association with Eco Tech Services, New Delhi for a World Bank Funded Project for UP Bhumi Sudhar Nigam.
10. Kesbari AK, Koo MH. 2002. Estimation of groundwater recharge from ground temperature measurements along vertical profiles. In Technologiesfor Analyzing the Groundwater Flow System, Jeju Islands, Korea, June 21; 77-99.
11. Keshari AK, Koo MH. 2007. Simulation of subsurface temperature under variable recharge. Joumal of Porous Media 10(8): (in press).
12. Leaney FW, Herczeg AL. 1995. Regional recharge to a Karst aquifer estimated from chemical and isotopic composition of dilute and localized recharge. Journal of Hydrology 164: 363-387.
13. Liu B, Phillips F, Hoines S, Campbell AR, Sharma P. 1995. Water movement in desert soil traced by hydrogen and oxygen isotopes, chloride and chlorine-36, southern Arizona. Journal of Hydrology 168: 91-110.
14. Rawls WJ, Ahuja LR, Brakensiek DL, Shirmohammadi A. 1992. Infiltration and soil water movement. In Handbook of Hydrology, Maidment DR (ed.). McGraw-Hill: New York; 5.1-5-51.
15. Reiter M. 2001. Using precision temperature logs to estimate horizontal and vertical groundwater flow components. Water Resources Research 37(3): 663-674.
16. Ronan AD, Prudic DE, Thodal CE, Constantz J. 1998. Field study and simulation of diurnal temperature effects on infiltration and variably saturated flow beneath an ephemeral stream. Water Resources Research 34(9): 2137-2153.
17. Sakura Y. 1977. The method for the estimations of the groundwater velocities from temperature distributions: On the groundwater around Sapporo, Japan. Studies in Water Temperature 21: 2-14.
18. Silliman SE, Ramirez J, McCabe RL. 1995. Quantifying downflow through creek sediments using temperature time series: one-dimensional solution incorporating measured surface temperature. Journal of Hydrology 167: 99-119.
19. Sorey ML. 1971. Measurement of vertical groundwater velocity from temperature profiles in wells. Water Resources Research 7(4): 963-970.
20. Stallman RW. 1965. Steady one-dimensional fluid flow in a semi-infinite porous medium with sinusoidal surface temperature. Journal of Geophysical Research 70(12): 2821-2827.
21. Stonestrom DA, Constantz J. 2003. Heat as a Tool for Studying the Movement of Ground Water near Streams. US Geological Survey Circular 1260: 96.
22. Suzuki S. 1960. Percolation measurements based on heat flow through soil with special reference to paddy fields. J Geophys Res 65: 2883-2885.
23. Tabbagh A, Bendjoudi H, Benderitter Y. 1999. Determination of recharge in unsaturated soils using temperature monitoring. Water Resources Research 35(8): 2439-2446.
24. Taniguchi M. 1993. Evaluation of vertical groundwater fluxes and thermal properties of aquifers based on transient temperature-depth profiles. Water Resources Research 29(7): 2021-2026.
25. Taniguchi M, Sbarma ML. 1993. Determination of groundwater recharge using the change in soil temperature. Journal of Hydrology 148: 219-229.
26. Taniguchi M, Shimada J, Tanaka T, et al. 1999a. Disturbances of temperature-depth profiles due to surface climate change and subsurface water flow: 1. An effect of linear increase in surface temperature caused by global warming and urbanization in the Tokyo metropolitan area, Japan. Water Resources Research 35(5): 1507-1517.
27. Taniguchi M, Williamson DR, Peck AJ. 1999b. Disturbances of temperature-depth profiles due to surface climate change and subsurface water flow: 2. An effect of step increase in surface temperature caused by forest clearing in southwest Western Australia. Water Resources Research 35(5): 1519-1529.
28. Walker GR, Jolly ID, Cook PG. 1991. A new chloride leaching approach to the estimation of diffuse recharge following a change in land use. Journal of Hydrology 128: 49-67.
29. Walker WW, Sanford WE. 1995. Chemical and isotopic methods for quantifying groundwater recharge in a regional, semiarid environment. Ground Water 33(3): 458-468.
30. Woodside W, Messmer J. 1961. Thermal conductivity of porous media: 1. Unconsolidated sand. Journal of Applied Physics 32: 1688-1699.