Titre de série :	U.S . Geological survey water -supply paper, 2322
Titre :	Leachate migration from and in-situ oil - shale -retort near rock springs, wyoming
Type de document :	texte imprimé
Auteurs :	Glover, K. C.
Mention d'édition :	U.S. Geological survey
Editeur :	U.S. Geological Survey
Année de publication :	1988
ISBN/ISSN/EAN :	CI-04248
Note générale :	Hydrogeologic factors influencing leachate movement from an in-situ oil shale retord near rock springs wyoming, were investigated through models of groud-water flow and solute transport. Leachate, indicated by the conservative ion thiocyanate has been observed 1/2 mile down gradient from the report. The contamined aquifer is part of the creen river formation and consist of thin permeable layers of tuff and sandstone interbeded with oil shale.
Langues :	Anglais (eng)
Mots-clés :	Hydrogéologie  Stratigraphie  Eau souterraine
Index. décimale :	551.48 Hydrologie :
Résumé :	Hydrogeologic factors influencing leachate movement from an in-situ oil shale retord near rock springs wyoming, were investigated through models of groud-water flow and solute transport. Leachate, indicated by the conservative ion thiocyanate has been observed 1/2 mile down gradient from the report. The contamined aquifer is part of the creen river formation and consist of thin permeable layers of tuff and sandstone interbeded with oil shale.
Note de contenu :	Hydrogeologic factors influencing leachate movement from an in-situ oil shale retord near rock springs wyoming, were investigated through models of groud-water flow and solute transport. Leachate, indicated by the conservative ion thiocyanate has been observed 1/2 mile down gradient from the report. The contamined aquifer is part of the creen river formation and consist of thin permeable layers of tuff and sandstone interbeded with oil shale.

U.S . Geological survey water -supply paper, 2322. Leachate migration from and in-situ oil - shale -retort near rock springs, wyoming [texte imprimé] / Glover, K. C.  . -  U.S. Geological survey . - U.S. Geological Survey, 1988.
ISSN : CI-04248
Hydrogeologic factors influencing leachate movement from an in-situ oil shale retord near rock springs wyoming, were investigated through models of groud-water flow and solute transport. Leachate, indicated by the conservative ion thiocyanate has been observed 1/2 mile down gradient from the report. The contamined aquifer is part of the creen river formation and consist of thin permeable layers of tuff and sandstone interbeded with oil shale.
Langues : Anglais (eng)

Mots-clés :	Hydrogéologie  Stratigraphie  Eau souterraine
Index. décimale :	551.48 Hydrologie :
Résumé :	Hydrogeologic factors influencing leachate movement from an in-situ oil shale retord near rock springs wyoming, were investigated through models of groud-water flow and solute transport. Leachate, indicated by the conservative ion thiocyanate has been observed 1/2 mile down gradient from the report. The contamined aquifer is part of the creen river formation and consist of thin permeable layers of tuff and sandstone interbeded with oil shale.
Note de contenu :	Hydrogeologic factors influencing leachate movement from an in-situ oil shale retord near rock springs wyoming, were investigated through models of groud-water flow and solute transport. Leachate, indicated by the conservative ion thiocyanate has been observed 1/2 mile down gradient from the report. The contamined aquifer is part of the creen river formation and consist of thin permeable layers of tuff and sandstone interbeded with oil shale.