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{"id":42,"date":"2007-12-06T11:27:42","date_gmt":"2007-12-06T16:27:42","guid":{"rendered":"http:\/\/hydrogeology.glg.msu.edu\/wordpress\/2007\/12\/06\/modeling-watershed-scale-groundwater-flow-and-geochemistry"},"modified":"2017-10-19T11:21:34","modified_gmt":"2017-10-19T16:21:34","slug":"modeling-watershed-scale-groundwater-flow-and-geochemistry","status":"publish","type":"post","link":"https:\/\/hydrogeology.msu.edu\/research\/completed\/modeling-watershed-scale-groundwater-flow-and-geochemistry","title":{"rendered":"Modeling Watershed Scale Groundwater Flow and Geochemistry"},"content":{"rendered":"

\"Cedar<\/a>Ground water chemistry is reflective of time-weighted averages of anthropogenic inputs originating from spatial and temporal patterns of land use. We developed an approach to examine potential relationships between land use-derived solutes and baseflow surface water quality using regional ground water and solute transport models linked to GIS. Our first test of this approach estimated chloride concentrations in surface water due to road salt transport through ground water in Michigan’s Grand Traverse Bay watershed.<\/p>\n

Further development of\u00a0 watershed-scale groundwater flow and transport models\u00a0 has been undertaken to examine the impacts of various land uses on nitrate concentrations.\u00a0 In Michigan, streams are predominantly groundwater-fed for much of the year.\u00a0 Therefore, understanding groundwater nitrate concentrations and fluxes is vital to understanding stream water quality.\u00a0 The figure on the left shows a preliminary simulation of total N concentrations in Cedar Creek, a small\u00a0 subwatershed of the Muskegon River in central lower Michigan.<\/p>\n

Related Publications:<\/strong><\/p>\n

Wood W.W. and Sanford W.E., 2007, Atmospheric bromine flux from the coastal Abu Dhabi sabkhat: A ground-water mass-balance investigation. Geophysical Research Letters, 34(14).<\/p>\n

Tyler S.W., Munoz J.F., and Wood W.W., 2006, The response of playa and sabkha hydraulics and mineralogy to climate forcing. Ground Water, 44(3), 329-338.<\/p>\n

Wood W.W., Sanford W.E., and Frape S., 2005, Chemical openness and potential for misinterpretation of the solute environment of coastal sabkhat. Chemical Geology, 215(1-4), 361-372.<\/p>\n

Wayland, KG, DW Hyndman, DF Boutt, BC Pijanowski, DT Long, (2002), Modeling The Impact Of Historical Land Uses On Surface Water Quality Using Ground Water Flow And Solute Transport Models, Lakes and Reservoirs, (7), 189-199<\/a><\/p>\n

Boutt, DF, DW Hyndman, BC Pijanowski, and DT Long, (2001), Modeling Impacts of Land Use on Groundwater and Surface Water Quality, Ground Water, 39 (1), 24-34<\/a><\/p>\n

Related Conference Abstracts:<\/strong><\/p>\n

Welty, NR, DW Hyndman, (2005), Exploring Linkages Between Land Use and Hydroecology Using Multivariate Analysis and Process-Based Models, Eos Trans AGU, 86(18)<\/a><\/p>\n

Kendall, AD, MC Spansky, and DW Hyndman, (2005), Using Dual-Region Calibration to Improve Recharge and Hydraulic Conductivity Estimates for Hydrologic Modeling, Eos Trans AGU, 86(18)<\/a><\/p>\n

Welty, NR, DW Hyndman, and LA Panayotoff , (2004), Eco-hydrologic modeling of nutrients, oxygen, and temperature across a range of Michigan streams, AGU Fall Meeting, San Francisco, EOS, H51D-1175<\/a><\/p>\n

Spansky, M, and DW Hyndman, (2004), Evaluating Nitrate Contributions from Different Land Use Types across a Regional Watershed Using Flow and Transport Models, AGU Spring Annual Meeting, EOS<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"

Ground water chemistry is reflective of time-weighted averages of anthropogenic inputs originating from spatial and temporal patterns of land use. We developed an approach to examine potential relationships between land use-derived solutes and baseflow surface water quality using regional ground water and solute transport models linked to GIS. Our first test of this approach estimated … <\/p>\n