Titre de série :	U.S. Geological Survey Watter Supply paper, 2324
Titre :	The geochemical evolution of aqueous sodium in the black creek aquifer, Horry anf Georgetown countries, South Carolina
Type de document :	texte imprimé
Auteurs :	Zack, A. ; Roberts, I.
Mention d'édition :	United States Gouvernment Printing Office
Editeur :	United States Gouvernment Printing Office
Année de publication :	1988
ISBN/ISSN/EAN :	CI-05087
Note générale :	The Black Creek aquifer contains dilute seawater near the north Carolina State line, probably the result of incomplete flushing of ancient seawater. Data do not indicate that the dilute seawater has migrated toward areas of fresh ground-water withdrawals. The concentration of chloride in ground-water samples rangs from 5 to 720 milligrams per liter and that of sodium from 160 to 690 milligrams per liter. Ion-exchange reactions occur with the calcium carbonate dissolution reaction wich produces calcium/ bicarbonate, and hydroxylions. The reaction sequence and stoichiometry result in an aqueous solution in which the sum of bicarbonate and chloride equivalents per liter is equal to the equivalents per liter of sodium.
Langues :	Anglais (eng)
Mots-clés :	Eau souterraine  Hydrogéologie  Géochimie  Calcium  Sodium  Bicarbonate
Index. décimale :	551.48 Hydrologie :
Résumé :	The Black Creek aquifer contains dilute seawater near the north Carolina State line, probably the result of incomplete flushing of ancient seawater. Data do not indicate that the dilute seawater has migrated toward areas of fresh ground-water withdrawals. The concentration of chloride in ground-water samples rangs from 5 to 720 milligrams per liter and that of sodium from 160 to 690 milligrams per liter. Ion-exchange reactions occur with the calcium carbonate dissolution reaction wich produces calcium/ bicarbonate, and hydroxylions. The reaction sequence and stoichiometry result in an aqueous solution in which the sum of bicarbonate and chloride equivalents per liter is equal to the equivalents per liter of sodium.
Note de contenu :	The Black Creek aquifer contains dilute seawater near the north Carolina State line, probably the result of incomplete flushing of ancient seawater. Data do not indicate that the dilute seawater has migrated toward areas of fresh ground-water withdrawals. The concentration of chloride in ground-water samples rangs from 5 to 720 milligrams per liter and that of sodium from 160 to 690 milligrams per liter. Ion-exchange reactions occur with the calcium carbonate dissolution reaction wich produces calcium/ bicarbonate, and hydroxylions. The reaction sequence and stoichiometry result in an aqueous solution in which the sum of bicarbonate and chloride equivalents per liter is equal to the equivalents per liter of sodium.

U.S. Geological Survey Watter Supply paper, 2324. The geochemical evolution of aqueous sodium in the black creek aquifer, Horry anf Georgetown countries, South Carolina [texte imprimé] / Zack, A. ; Roberts, I.  . -  United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1988.
ISSN : CI-05087
The Black Creek aquifer contains dilute seawater near the north Carolina State line, probably the result of incomplete flushing of ancient seawater. Data do not indicate that the dilute seawater has migrated toward areas of fresh ground-water withdrawals. The concentration of chloride in ground-water samples rangs from 5 to 720 milligrams per liter and that of sodium from 160 to 690 milligrams per liter. Ion-exchange reactions occur with the calcium carbonate dissolution reaction wich produces calcium/ bicarbonate, and hydroxylions. The reaction sequence and stoichiometry result in an aqueous solution in which the sum of bicarbonate and chloride equivalents per liter is equal to the equivalents per liter of sodium.
Langues : Anglais (eng)

Mots-clés :	Eau souterraine  Hydrogéologie  Géochimie  Calcium  Sodium  Bicarbonate
Index. décimale :	551.48 Hydrologie :
Résumé :	The Black Creek aquifer contains dilute seawater near the north Carolina State line, probably the result of incomplete flushing of ancient seawater. Data do not indicate that the dilute seawater has migrated toward areas of fresh ground-water withdrawals. The concentration of chloride in ground-water samples rangs from 5 to 720 milligrams per liter and that of sodium from 160 to 690 milligrams per liter. Ion-exchange reactions occur with the calcium carbonate dissolution reaction wich produces calcium/ bicarbonate, and hydroxylions. The reaction sequence and stoichiometry result in an aqueous solution in which the sum of bicarbonate and chloride equivalents per liter is equal to the equivalents per liter of sodium.
Note de contenu :	The Black Creek aquifer contains dilute seawater near the north Carolina State line, probably the result of incomplete flushing of ancient seawater. Data do not indicate that the dilute seawater has migrated toward areas of fresh ground-water withdrawals. The concentration of chloride in ground-water samples rangs from 5 to 720 milligrams per liter and that of sodium from 160 to 690 milligrams per liter. Ion-exchange reactions occur with the calcium carbonate dissolution reaction wich produces calcium/ bicarbonate, and hydroxylions. The reaction sequence and stoichiometry result in an aqueous solution in which the sum of bicarbonate and chloride equivalents per liter is equal to the equivalents per liter of sodium.