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Groundwater chemical evolution and diagenetic processes in the Upper Floridan aquifer, southern South Carolina and northeastern Georgia.

机译：佛罗里达上层含水层，南卡罗来纳州南部和乔治亚州东北部的地下水化学演化和成岩过程。

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The Upper Floridan aquifer in southern South Carolina and northeastern Georgia is composed of 76 percent low-magnesium calcite with the remainder made up primarily by silicates. Based on ground-water chemistry, the aquifer can be subdivided into two zones: (1) a low-salinity zone (Cl ;In the mixing zone, concentrations of most ground-water constituents deviate from the values expected for conservative mixing of fresh water with seawater. Mineral saturation and mass balance calculations show that this can be explained by dissolution of carbonate minerals in response to CO;The ground-water composition changes along flow paths in the low-salinity zone with decreasing calcium and bicarbonate concentrations, and increasing magnesium, sodium, potassium, sulfate, silica, fluoride, pH, and

机译：南卡罗来纳州南部和佐治亚州东北部的上佛罗里达水层由76％的低镁方解石组成，其余部分主要由硅酸盐组成。根据地下水化学性质，可将含水层分为两个区域：（1）低盐度区域（Cl）；在混合区域中，大多数地下水成分的浓度偏离了保守混合淡水的预期值矿物饱和度和质量平衡计算表明，这可以用碳酸盐矿物对CO的溶解来解释；地下水组成沿低盐度带的流路变化，钙和碳酸氢盐浓度降低，镁含量增加，钠，钾，硫酸盐，二氧化硅，氟化物，pH和

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作者
Burt, Ronald Allen.;
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作者单位

University of South Carolina.;

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授予单位 University of South Carolina.;
学科 Geology.
学位 Ph.D.
年度 1988
页码 270 p.
总页数 270
原文格式 PDF
正文语种 eng
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机译：南佛罗里达南部和佐治亚州东北部上佛罗里达州的地下水化学演化和成岩过程

Groundwater chemical evolution and diagenetic processes in the Upper Floridan aquifer, southern South Carolina and northeastern Georgia.

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