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dc.contributor.author Griggs, John E en_US
dc.contributor.author Peterson, Frank L en_US
dc.date.accessioned 2008-07-17T22:28:24Z en_US
dc.date.available 2008-07-17T22:28:24Z en_US
dc.date.issued 1989-06 en_US
dc.identifier.citation Griggs JE, Peterson FL. 1989. Groundwater flow and development alternatives: a numerical simulation of Laura, Majuro Atoll, Marshall Islands. Honolulu (HI): Water Resources Research Center, University of Hawaii at Manoa. WRRC technical report, 183. en_US
dc.identifier.uri http://hdl.handle.net/10125/1972 en_US
dc.description U.S. Geological Survey University of Guam Grant/Contract No. RCUH 3162, RCUH 3292 en_US
dc.description.abstract The numerical simulation of groundwater flow with solute transport is described for Laura on Majuro Atoll, Marshall Islands. The primary objective was to investigate strategies for developing and managing the freshwater resource in Laura. Secondary objectives included performing a sensitivity analysis of the parameters used to calibrate the model and illustrating the effect of density-dependent fluid flow. The two-dimensional mathematical model SUTRA was selected for the simulations because it is based on density-dependent fluid flow and solute transport equations. Cartesian coordinates were used to approximate a vertical cross section through the Laura area in which three boreholes and three nests of piezometers were emplaced during another 1987 study. The wells are along a line perpendicular to the ocean and lagoon shorelines running through the central portion of Laura. The model was calibrated in a transient mode with constant sea-level boundary conditions by using observed salinity data. Permeabilities and dispersivities were adjusted during calibration. In a preliminary attempt, tidal boundary conditions were also used to calibrate the model. Model calibration showed that the 50% isochlor depth depends primarily on permeability and that the transition zone thickness is most sensitive to transverse dispersivities. Simulated pumping results indicated that gallery-type wells constructed in the center of the islet could supply 1.4 to 2.1 million l/day of fresh water. Also, a comparison between flow regimes generated by single-phase fluid flow and density-dependent fluid flow demonstrated that the latter greatly affects the groundwater flow regime and must be included in flow dynamics modeling studies of atolls and small oceanic islands. en_US
dc.format.extent x + 91 pages en_US
dc.language.iso en-US en_US
dc.publisher Water Resources Research Center, University of Hawaii at Manoa en_US
dc.relation.ispartofseries WRRC Technical Report en_US
dc.relation.ispartofseries 183 en_US
dc.subject groundwater movement en_US
dc.subject groundwater potential en_US
dc.subject solute transport en_US
dc.subject simulation analysis en_US
dc.subject geohydrology en_US
dc.subject groundwater flow en_US
dc.subject SUTRA en_US
dc.subject Laura en_US
dc.subject Majuro Atoll en_US
dc.subject Marshall Islands en_US
dc.subject.lcsh Groundwater flow -- Marshall Islands -- Majuro Atoll -- Mathematical models. en_US
dc.subject.lcsh Water resources development -- Marshall Islands -- Majuro Atoll. en_US
dc.subject.lcsh Water-supply -- Marshall Islands -- Majuro Atoll. en_US
dc.title WRRCTR No.183 Groundwater flow and development alternatives: A numerical simulation of Laura, Majuro Atoll, Marshall Islands en_US
dc.type Report en_US
dc.type.dcmi Text en_US

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