Title: HydroGeoSphere: A Fully Integrated, Physically Based Hydrological Model
Abstract: GroundwaterVolume 50, Issue 2 p. 170-176 HydroGeoSphere: A Fully Integrated, Physically Based Hydrological Model Philip Brunner, Corresponding Author Philip Brunner Centre d’Hydrogéologie et de Géothermie, University of Neuchâtel, Switzerland; [email protected]Search for more papers by this authorCraig T. Simmons, Craig T. Simmons National Centre for Groundwater Research and Training, Flinders University, GPO Box 2100, Adelaide, SA 5001, Australia. School of the Environment, Flinders University, GPO Box 2100, Adelaide, SA 5001, Australia.Search for more papers by this author Philip Brunner, Corresponding Author Philip Brunner Centre d’Hydrogéologie et de Géothermie, University of Neuchâtel, Switzerland; [email protected]Search for more papers by this authorCraig T. Simmons, Craig T. Simmons National Centre for Groundwater Research and Training, Flinders University, GPO Box 2100, Adelaide, SA 5001, Australia. School of the Environment, Flinders University, GPO Box 2100, Adelaide, SA 5001, Australia.Search for more papers by this author First published: 07 December 2011 https://doi.org/10.1111/j.1745-6584.2011.00882.xCitations: 319Read the full textAboutPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Share a linkShare onEmailFacebookTwitterLinkedInRedditWechat References AquaVeo. 2011. GMS, Provo, UT. Behie, G.A., and P.A. Forsyth. 1984. Incomplete factorization methods for fully implicit simulation of enhanced oil-recovery. SIAM Journal on Scientific and Statistical Computing 5, no. 3: 543–561. Beven, K. 2002. Towards an alternative blueprint for a physically based digitally simulated hydrologic response modelling system. Hydrological Processes 16, no. 2: 189–206. Brooks, R.J., and A.T. Corey. 1964. Hydraulic Properties of Porours Media. Hydrology Paper No. 3. Fort Collins: Colorado State University. Brookfield, A.E., E.A. Sudicky, Y.-J. Park, and B. Conant Jr. 2009. Simulation of thermal stream loadings using a fully-integrated surface/subsurface modeling framework. Hydrological Processes 23, no. 15: 15. DOI: 10.1002/hyp Brunner, P., C.T. Simmons, and P.G. Cook. 2009. Spatial and temporal aspects of the transition from connection to disconnection between rivers, lakes and groundwater. Journal of Hydrology 376, no. 1–2: 159–169. Carrera-Hernandez, J.J., C.A. Mendoza, K.J. Devito, R.M. Petrone, and B.D. Smerdon. 2011. Effects of aspen harvesting on groundwater recharge and water table dynamics in a subhumid climate. Water Resources Research 47:W05542. DOI: 10.1029/2010WR009684. Doble, R., P. Brunner, J. McCallum, and P.G. Cook. 2011. An analysis of river bank slope and unsaturated flow effects on bank storage. Ground Water. DOI: 10.1111/j.1745-6584.2011.00821.x. Doherty, J. 2010. PEST- Model-Independent Parameter Estimation. Watermark Numerical Computing. pesthomepage.org. Ebel, B.A., B.B. Mirus, C.S. Heppner, J.E. VanderKwaak, and K. Loague. 2009. First-order exchange coefficient coupling for simulating surface water-groundwater interactions: parameter sensitivity and consistency with a physics-based approach. Hydrological Processes 23, no. 13: 1949–1959. Forsyth, P.A. 1991. A control volume finite-element approach to napl groundwater contamination. SIAM Journal on Scientific and Statistical Computing 12, no. 5: 1029–1057. Forsyth, P.A. 1988. Comparison of the single-phase and two-phase numerical model formulation for saturated-unsaturated groundwater flow. Computer Methods in Applied Mechanics and Engineering 69, no. 2: 243–259. Forsyth, P.A., and P.H. Sammon. 1986. Practical considerations for adaptive implicit methods in reservoir simulation. Journal of Computational Physics 62, no. 2: 265–281. Forsyth, P.A., Y.S. Wu, and K. Pruess. 1995. Robust numerical-methods for saturated-unsaturated flow with dry initial conditions in heterogeneous media. Advances in Water Resources 18, no. 1: 25–38. Freeze, A.R., and R.L. Harlan. 1969. Blueprint for a physically-based, digitally-simulated hydrogeologic response model. Journal of Hydrology 9: 237–258. Gerke, H.H., and M.T. Van Genuchten. 1993. A dual-porosity model for simulating the preferential movement of water and solutes in structured porous-media. Water Resources Research 29, no. 2: 305–319. Graf, T. 2005. Modeling coupled thermohaline flow and reactive solute transport in discretely-fractured porous media. http://www.theses.ulaval.ca/2005/23197/23197.pdf. Graf, T., and M.C. Boufadel. 2011. Effect of viscosity, capillarity and grid spacing on thermal variable-density flow. Journal of Hydrology 400, no. 1–2: 41–57. Graf, T., and R. Therrien. 2008. A test case for the simulation of three-dimensional variable-density flow and solute transport in discretely-fractured porous media. Advances in Water Resources 31, no. 10: 1352–1363. Graf, T., and R. Therrien. 2007. Coupled thermohaline groundwater flow and single-species reactive solute transport in fractured porous media. Advances in Water Resources 30, no. 4: 742–771. Huyakorn, P.S., and G.F. Pinder. 1983. Computational Methods in Subsurface Flow, vol. xiii, 473. New York: Academic Press. Tecplot Inc. 2011. TECPLOT. Washington: Bellevue. Kristensen, K.J., and S.E. Jensen. 1975. A model for estimating actual evapotranspiration from potential evapotranspiration. Nordic Hydrology 6: 170–188. Lemieux, J.M., E.A. Sudicky, W.R. Peltier, and L. Tarasov. 2008. Simulating the impact of glaciations on continental groundwater flow systems: 1. Relevant processes and model formulation. Journal of Geophysical Research. Earth Surface 113:F03017. DOI: 10.1029/2007JF000928. McCallum, J.L., P.G. Cook, P. Brunner, and D. Berhane. 2010. Solute dynamics during bank storage flows and implications for chemical base flow separation. Water Resources Research 46: W07541. Park, Y.-J., E.A. Sudicky, S. Panday, and G. Matanga. 2009. Implicit sub-time stepping for solving nonlinear equations of flow in an integrated surface-subsurface system. Vadose Zone Journal 8, no. 4: 825–836. DOI: 10.2136/vzj2009.0013 Park, Y.J., E.A. Sudicky, R.G. McLaren, and J.F. Sykes. 2004. Analysis of hydraulic and tracer response tests within moderately fractured rock based on a transition probability geostatistical approach. Water Resources Research 40:W12404. DOI: 10.1029/2004WR003188. Partington, D., P. Brunner, C.T. Simmons, R. Therrien, A.D. Werner, G.C. Dandy, and H.R. Maier. 2011. A hydraulic mixing-cell method to quantify the groundwater component of streamflow within spatially distributed fully integrated surface water-groundwater flow models. Environmental Modelling and Software 26, no. 7: 886–898. Rausch, R., Schäfer, W., Therrien, R., and Wagner, C. 2005. Solute Transport Modelling: An Introduction to Models and Solution Strategies, v, 205 p. Berlin: Gebrüder Borntraeger. Raymond, J., and R. Therrien. 2008. Low-temperature geothermal potential of the flooded Gaspé Mines, Québec, Canada. Geothermics 37, no. 2: 189–210. Schwartz, F.W., E.A. Sudicky, R.G. McLaren, Y.-J. Park, M. Huber, and M. Apted. 2010. Ambiguous hydraulic heads and 14C activities in transient regional flow. Ground Water 48, no. 3: 366–379. Therrien, R. 1992. Three-dimensional analysis of variably-saturated flow and solute transport in discretely-fractured porous media. Ph.D. thesis, University of Waterloo, Waterloo, Ont. Therrien, R., and E.A. Sudicky. 2000. Well bore boundary conditions for variably saturated flow modeling. Advances in Water Resources 24, no. 2: 195–201. Therrien, R., and E.A. Sudicky. 1996. Three-dimensional analysis of variably-saturated flow and solute transport in discretely-fractured porous media. Journal of Contaminant Hydrology 23, no. 1–2: 1–44. Unger, A.J.A., Q. Li, E.A. Sudicky, D. Kassenaar, E.J. Wexler, and S. Shikaze. 2008. Simulating the multi-seasonal response of a large-scale watershed with a 3D physically-based hydrologic model. Journal of Hydrology 357, no. 3–4: 317–336. van Genuchten, M.T. 1980. A closed-form equation for predicting the hydraulic conductivity of unsaturated soils. Soil Science Society of America Journal 44, no. 5: 892–898. Verseghy, D.L. 1991. Class—A Canadian land surface scheme for GCMS. I. Soil model. International Journal of Climatology 11, no. 2: 111–133. Citing Literature Volume50, Issue2March/April 2012Pages 170-176 ReferencesRelatedInformation