Titre de série :	Journal of hydrology
Titre :	Géochemistry and natural ionic and isotopic tracing / two compementary ways to study the naturel salinity regime of the hydrological system of lake chad
Type de document :	texte imprimé
Auteurs :	Roche, M. A.
Année de publication :	1975
ISBN/ISSN/EAN :	CI-02254
Note générale :	As a consequence of intense evaporation and transit through a succession of sedimentary traps, the isotopic conposition of the water and the characteristics of the dissolved and suspended loads change downstream in a regular manner resembling chromatography... This study illustrates that these two avenues of research prove to be complementary, justifying the use of common models and, in the final analysis, are indispensable to each other.
Langues :	Anglais (eng)
Mots-clés :	Géochimie  Salinité  Hydrogéologie  Lac  Hydrologie  Tracé isotopique  Tracé ionique
Index. décimale :	551.48 Hydrologie :
Résumé :	As a consequence of intense evaporation and transit through a succession of sedimentary traps, the isotopic conposition of the water and the characteristics of the dissolved and suspended loads change downstream in a regular manner resembling chromatography... This study illustrates that these two avenues of research prove to be complementary, justifying the use of common models and, in the final analysis, are indispensable to each other.
Note de contenu :	As a consequence of intense evaporation and transit through a succession of sedimentary traps, the isotopic conposition of the water and the characteristics of the dissolved and suspended loads change downstream in a regular manner resembling chromatography... This study illustrates that these two avenues of research prove to be complementary, justifying the use of common models and, in the final analysis, are indispensable to each other.

Journal of hydrology. Géochemistry and natural ionic and isotopic tracing / two compementary ways to study the naturel salinity regime of the hydrological system of lake chad [texte imprimé] / Roche, M. A. . - 1975.
ISSN : CI-02254
As a consequence of intense evaporation and transit through a succession of sedimentary traps, the isotopic conposition of the water and the characteristics of the dissolved and suspended loads change downstream in a regular manner resembling chromatography... This study illustrates that these two avenues of research prove to be complementary, justifying the use of common models and, in the final analysis, are indispensable to each other.
Langues : Anglais (eng)

Mots-clés :	Géochimie  Salinité  Hydrogéologie  Lac  Hydrologie  Tracé isotopique  Tracé ionique
Index. décimale :	551.48 Hydrologie :
Résumé :	As a consequence of intense evaporation and transit through a succession of sedimentary traps, the isotopic conposition of the water and the characteristics of the dissolved and suspended loads change downstream in a regular manner resembling chromatography... This study illustrates that these two avenues of research prove to be complementary, justifying the use of common models and, in the final analysis, are indispensable to each other.
Note de contenu :	As a consequence of intense evaporation and transit through a succession of sedimentary traps, the isotopic conposition of the water and the characteristics of the dissolved and suspended loads change downstream in a regular manner resembling chromatography... This study illustrates that these two avenues of research prove to be complementary, justifying the use of common models and, in the final analysis, are indispensable to each other.