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Wetlands in northern Salt Lake Valley, Salt Lake County, Utah

Wetlands in northern Salt Lake Valley, Salt Lake County, Utah

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4<strong>Utah</strong> Geological SurveyFigure 3. Annual water usages by category for <strong>Salt</strong> <strong>Lake</strong> <strong>Valley</strong> (based on data from <strong>Utah</strong> Division of Water Rights).Purpose and ScopeThe purpose of this study is to use exist<strong>in</strong>g data to estimate awater budget for the wetland areas, and to use exist<strong>in</strong>g steadystateand transient ground-water flow models developed by theU.S. Geological Survey (USGS) (Lambert, 1995a) to simulatethe hydrologic effects on wetlands from various recharge ratesand projected ground-water withdrawals at various projectedGreat <strong>Salt</strong> <strong>Lake</strong> levels; the estimated water budget and modelsimulations focus on wetlands around the marg<strong>in</strong>s of Great<strong>Salt</strong> <strong>Lake</strong>, although the study results may apply to all of thewetlands <strong>in</strong> <strong>Salt</strong> <strong>Lake</strong> <strong>Valley</strong>. These simulations can be usedto assess potential threats to wetlands from <strong>in</strong>creased groundwaterwithdrawals and drought, and provide a basis for (1)implement<strong>in</strong>g restrictions on domestic withdrawals, (2) assess<strong>in</strong>gwater needs for wetland preservation, and (3) encourag<strong>in</strong>gthe development of water conservation programs.Our study comb<strong>in</strong>es empirical and model<strong>in</strong>g analyses to understandthe effects of changes <strong>in</strong> land use and climate. Weused an estimated water budget to compare and <strong>in</strong>terpretnumerical ground-water flow models, which simulate fluxes<strong>in</strong>to and out of the <strong>Salt</strong> <strong>Lake</strong> <strong>Valley</strong> wetland areas. Numericalground-water flow models have been used to understandthe <strong>in</strong>teraction between wetlands and ground water <strong>in</strong> otherstudies (Burk and others, 2005; Bishop and others, 2009). Theaccuracy of the solutions obta<strong>in</strong>ed by numerical methods isgenerally sufficient; however, the accuracy depends on severalfactors, <strong>in</strong>clud<strong>in</strong>g our understand<strong>in</strong>g of the complexityof the system, boundary and <strong>in</strong>itial conditions, and numericalmethods used.A second objective is to document the hydraulic gradient andcurrent quality of ground water <strong>in</strong> the wetland areas near Great<strong>Salt</strong> <strong>Lake</strong>. We used water levels <strong>in</strong> shallow wells to documentthe hydraulic gradient <strong>in</strong> the shallow unconf<strong>in</strong>ed aquifer, anddata from water samples from two of the wells to provide <strong>in</strong>sight<strong>in</strong>to the current quality of ground water flow<strong>in</strong>g <strong>in</strong>to thewetland areas. Data from two wells are not sufficient to accuratelycharacterize the quality of ground water enter<strong>in</strong>g thewetland areas, but <strong>in</strong>formation from these two wells <strong>in</strong> additionto data from previous work provide a sense of the qualityof ground water recharg<strong>in</strong>g the wetland areas.This report provides the necessary <strong>in</strong>tegration of geologicand hydrologic wetland studies to more fully understand thehydrologic system of the <strong>Salt</strong> <strong>Lake</strong> <strong>Valley</strong> wetlands area <strong>in</strong>relation to wetland functionality, with emphasis on the wetlandsnear Great <strong>Salt</strong> <strong>Lake</strong>. The scope of this study <strong>in</strong>cludes athorough literature search; a compilation of published and unpublishedgeologic, hydrologic, and wetland <strong>in</strong>formation; andfield sampl<strong>in</strong>g and analysis of water data from shallow wells.Detailed USGS ground-water models, which are described<strong>in</strong> this report, were used by the USGS and other agencies toidentify historical changes <strong>in</strong> the ground-water flow system <strong>in</strong><strong>Salt</strong> <strong>Lake</strong> <strong>Valley</strong>.

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