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Devonshire groundwater

Figure 7.26. Hydrogeologic cross-section of the Devonshire groundwater lens. The X s denote a calculated fit to the 50% isoline of relative salinity (e) using the Ghyben-Herzberg-Dupuit model. (After Vacher, 1974, 1978.)... Figure 7.26. Hydrogeologic cross-section of the Devonshire groundwater lens. The X s denote a calculated fit to the 50% isoline of relative salinity (e) using the Ghyben-Herzberg-Dupuit model. (After Vacher, 1974, 1978.)...
Based on these observations of the chemistry of the Devonshire groundwater lens, and on calculations whose results are portrayed in Figure 7.34, Plummer et al. (1976) concluded the following ... [Pg.348]

Figure 7.32. Geochemistry of the Devonshire, Bermuda groundwater lens. (A) Well samples and location of freshwater, (B) percentage of seawater in the groundwater, (C) saturation with respect to aragonite, (D) saturation with respect to calcite. SI (= Q) is the saturation index. (After Plummer et al., 1976.)... Figure 7.32. Geochemistry of the Devonshire, Bermuda groundwater lens. (A) Well samples and location of freshwater, (B) percentage of seawater in the groundwater, (C) saturation with respect to aragonite, (D) saturation with respect to calcite. SI (= Q) is the saturation index. (After Plummer et al., 1976.)...
See other pages where Devonshire groundwater is mentioned: [Pg.339]    [Pg.340]    [Pg.347]    [Pg.350]    [Pg.350]   


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