Advances in Geosciences 2010
DOI: 10.1142/9789812838124_0007
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Numerical Simulation of Electric Conductivity Fluctuations Due to Groundwater Pumping in a Coastal Aquifer

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“…For the transport simulation in the aquifer (MT3DMS/SEAWAT software), the longitudinal and transverse dispersivity ( αL , αT ) were set to 3.6 m and 0.36 m lengths, respectively (Perera, Jinno, Hiroshiro, & Tsutsumi, ; Shoemaker, ), and the molecular diffusion to 1.0 10 −10 m 2 /d. Fresh water density was set to 1,000 g/L and salt water density to 1,024.5 g/L.…”
Section: Methodsmentioning
confidence: 99%
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“…For the transport simulation in the aquifer (MT3DMS/SEAWAT software), the longitudinal and transverse dispersivity ( αL , αT ) were set to 3.6 m and 0.36 m lengths, respectively (Perera, Jinno, Hiroshiro, & Tsutsumi, ; Shoemaker, ), and the molecular diffusion to 1.0 10 −10 m 2 /d. Fresh water density was set to 1,000 g/L and salt water density to 1,024.5 g/L.…”
Section: Methodsmentioning
confidence: 99%
“…The model results were compare with the TDS observation data from the wells located outside the urban area and close to the boundaries, selected as representatives for the regional unmodified salinity condition. For the transport simulation in the aquifer (MT3DMS/SEAWAT software), the longitudinal and transverse dispersivity (αL, αT) were set to 3.6 m and 0.36 m lengths, respectively (Perera, Jinno, Hiroshiro, & Tsutsumi, 2008;Shoemaker, 2004), and the molecular diffusion to 1.0 10 −10 m 2 /d. Fresh water density was set to 1,000 g/L and salt water density to 1,024.5 g/L.…”
Section: Methodsmentioning
confidence: 99%