1970
DOI: 10.1016/0022-1694(70)90222-2
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Comparison of chemical hydrogeology of the carbonate peninsulas of Florida and Yucatan

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Cited by 250 publications
(132 citation statements)
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“…An example is the northern Yucatan Peninsula today, which, despite having high rainfall and large areal extent, possesses a freshwater lens less than 100 m deep (Back and Hanshaw, 1970). Although the petrography of Unit III is most easily explained by invoking freshwater alteration, the hydrology required by this model is not easily demonstrated.…”
Section: Freshwater Alterationmentioning
confidence: 99%
“…An example is the northern Yucatan Peninsula today, which, despite having high rainfall and large areal extent, possesses a freshwater lens less than 100 m deep (Back and Hanshaw, 1970). Although the petrography of Unit III is most easily explained by invoking freshwater alteration, the hydrology required by this model is not easily demonstrated.…”
Section: Freshwater Alterationmentioning
confidence: 99%
“…The chemical trends seen in Figures 33 are similar to major-ion evolution sequences (Chevotarev, 1955;Freeze and Cherry, 1979) and to dedolomitization, which is dissolution of dolomite and precipitation of calcite caused by the dissolution of anhydrite (Back and Hanshaw, 1970;Hanshaw and Back, 1979;Back et al, 1983;Busby et al, 1990;Plummer et al, 1990). Therefore, we also chose dissolved sulfate as a reaction-progress variable to examine water chemistry.…”
Section: Future Plansmentioning
confidence: 66%
“…Supersaturation with respect to calcite causes precipitation of the mineral, resulting in a decrease of alkalinity and further dissolution of dolomite and anhydrite. This is a typical mechanism of dedolomitization in carbonate rocks (Back and Hanshaw, 1970;Hanshaw and Back, 1979;Back et al, 1983;Busby et al, 1990;Plummer et al, 1990). (Dickey, 1969).…”
Section: Future Plansmentioning
confidence: 95%
“…The almost complete absence of confining beds above limestone in the Yucatan Peninsula determines a high hydraulic conductivity in the karstic substrate (Back and Hanshaw, 1970). This geohydrological trait leads to high infiltration of the rainfall through subsurface layers, and eventually, full recharging of the aquifer during rainy seasons.…”
Section: Methodsmentioning
confidence: 99%