| Titre de série : |
Groundwater studies, 4 |
| Titre : |
Chapter 3 : Analytical and investigational techniques for non-indurated sediments |
| Type de document : |
texte imprimé |
| Auteurs : |
Brown, A. H. ; Konoplyantsev, A. A. ; Ineson, J. |
| Mention d'édition : |
UNESCO |
| Editeur : |
UNESCO |
| Année de publication : |
1983 |
| ISBN/ISSN/EAN : |
978-92-3-102087-2 |
| Note générale : |
Non indurated sediments, the bulk of tertiary to quaternary age, contain most of the world's large reservoirs of renewable ground-water supply. These sediments are preferred as sources of ground water, because they are soft, easy to drill, and make well construction rapid and inexpensive. Non-indurated sediments generally occur in valley or lowlands where the ground-water level is relatively near the land surface, and pumping lifts are consequently low. |
| Langues : |
Anglais (eng) |
| Mots-clés : |
Eau souterraine Hydrogéologie Bassin hydrologique Forage Qualité de l'eau |
| Index. décimale : |
622.2 Exploitation souterraine |
| Résumé : |
Non indurated sediments, the bulk of tertiary to quaternary age, contain most of the world's large reservoirs of renewable ground-water supply. These sediments are preferred as sources of ground water, because they are soft, easy to drill, and make well construction rapid and inexpensive. Non-indurated sediments generally occur in valley or lowlands where the ground-water level is relatively near the land surface, and pumping lifts are consequently low. |
| Note de contenu : |
Non indurated sediments, the bulk of tertiary to quaternary age, contain most of the world's large reservoirs of renewable ground-water supply. These sediments are preferred as sources of ground water, because they are soft, easy to drill, and make well construction rapid and inexpensive. Non-indurated sediments generally occur in valley or lowlands where the ground-water level is relatively near the land surface, and pumping lifts are consequently low. |
Groundwater studies, 4. Chapter 3 : Analytical and investigational techniques for non-indurated sediments [texte imprimé] / Brown, A. H. ; Konoplyantsev, A. A. ; Ineson, J. . - UNESCO . - UNESCO, 1983. ISBN : 978-92-3-102087-2 Non indurated sediments, the bulk of tertiary to quaternary age, contain most of the world's large reservoirs of renewable ground-water supply. These sediments are preferred as sources of ground water, because they are soft, easy to drill, and make well construction rapid and inexpensive. Non-indurated sediments generally occur in valley or lowlands where the ground-water level is relatively near the land surface, and pumping lifts are consequently low. Langues : Anglais ( eng)
| Mots-clés : |
Eau souterraine Hydrogéologie Bassin hydrologique Forage Qualité de l'eau |
| Index. décimale : |
622.2 Exploitation souterraine |
| Résumé : |
Non indurated sediments, the bulk of tertiary to quaternary age, contain most of the world's large reservoirs of renewable ground-water supply. These sediments are preferred as sources of ground water, because they are soft, easy to drill, and make well construction rapid and inexpensive. Non-indurated sediments generally occur in valley or lowlands where the ground-water level is relatively near the land surface, and pumping lifts are consequently low. |
| Note de contenu : |
Non indurated sediments, the bulk of tertiary to quaternary age, contain most of the world's large reservoirs of renewable ground-water supply. These sediments are preferred as sources of ground water, because they are soft, easy to drill, and make well construction rapid and inexpensive. Non-indurated sediments generally occur in valley or lowlands where the ground-water level is relatively near the land surface, and pumping lifts are consequently low. |
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