| Titre de série : |
research report - A water resources technical publication, 13 |
| Titre : |
Removal of saline water from aquifers |
| Type de document : |
texte imprimé |
| Auteurs : |
Carlson, E.J. |
| Mention d'édition : |
Unite State Departement of the interior |
| Editeur : |
Unite State Departement of the interior |
| Année de publication : |
1968 |
| ISBN/ISSN/EAN : |
CI-08638 |
| Note générale : |
Aquifer swetening is studied in the laboratory using a rectangular, glass - Walled, sand - fielled tank. Two types of aquifer are studies (1) a 1:40 scale/ two - part aquifer (coarse and fine sand) representing a vertical cross section through and idéalizeportion of an irrieated valley, and (2)a fine sand, sigle part aquifer used to evaluate a formula derived from the ghyben - Herzberg principle for computing depth to a saline - fresh water interface . Salt water is flushed from the aquifer into subsurface drains by applying fresh water to the surface . Tests results for both aquifer types showed that tile drains placed near the ground surface will not intercept and discharge surface applied fresh water if all or part of the aquifer contains salt water... |
| Langues : |
Anglais (eng) |
| Mots-clés : |
Eau salée Eau souterraine Drainage Débit fluvial Ressource en eau Hydrogéologie Modèle hydraulique Aquifère |
| Index. décimale : |
621.2 Hydraulique : turbines, pompes, accumulateurs, transmission hydraulique |
| Résumé : |
Aquifer swetening is studied in the laboratory using a rectangular, glass - Walled, sand - fielled tank. Two types of aquifer are studies (1) a 1:40 scale/ two - part aquifer (coarse and fine sand) representing a vertical cross section through and idéalizeportion of an irrieated valley, and (2)a fine sand, sigle part aquifer used to evaluate a formula derived from the ghyben - Herzberg principle for computing depth to a saline - fresh water interface . Salt water is flushed from the aquifer into subsurface drains by applying fresh water to the surface . Tests results for both aquifer types showed that tile drains placed near the ground surface will not intercept and discharge surface applied fresh water if all or part of the aquifer contains salt water... |
| Note de contenu : |
Aquifer swetening is studied in the laboratory using a rectangular, glass - Walled, sand - fielled tank. Two types of aquifer are studies (1) a 1:40 scale/ two - part aquifer (coarse and fine sand) representing a vertical cross section through and idéalizeportion of an irrieated valley, and (2)a fine sand, sigle part aquifer used to evaluate a formula derived from the ghyben - Herzberg principle for computing depth to a saline - fresh water interface . Salt water is flushed from the aquifer into subsurface drains by applying fresh water to the surface . Tests results for both aquifer types showed that tile drains placed near the ground surface will not intercept and discharge surface applied fresh water if all or part of the aquifer contains salt water... |
research report - A water resources technical publication, 13. Removal of saline water from aquifers [texte imprimé] / Carlson, E.J. . - Unite State Departement of the interior . - Unite State Departement of the interior, 1968. ISSN : CI-08638 Aquifer swetening is studied in the laboratory using a rectangular, glass - Walled, sand - fielled tank. Two types of aquifer are studies (1) a 1:40 scale/ two - part aquifer (coarse and fine sand) representing a vertical cross section through and idéalizeportion of an irrieated valley, and (2)a fine sand, sigle part aquifer used to evaluate a formula derived from the ghyben - Herzberg principle for computing depth to a saline - fresh water interface . Salt water is flushed from the aquifer into subsurface drains by applying fresh water to the surface . Tests results for both aquifer types showed that tile drains placed near the ground surface will not intercept and discharge surface applied fresh water if all or part of the aquifer contains salt water... Langues : Anglais ( eng)
| Mots-clés : |
Eau salée Eau souterraine Drainage Débit fluvial Ressource en eau Hydrogéologie Modèle hydraulique Aquifère |
| Index. décimale : |
621.2 Hydraulique : turbines, pompes, accumulateurs, transmission hydraulique |
| Résumé : |
Aquifer swetening is studied in the laboratory using a rectangular, glass - Walled, sand - fielled tank. Two types of aquifer are studies (1) a 1:40 scale/ two - part aquifer (coarse and fine sand) representing a vertical cross section through and idéalizeportion of an irrieated valley, and (2)a fine sand, sigle part aquifer used to evaluate a formula derived from the ghyben - Herzberg principle for computing depth to a saline - fresh water interface . Salt water is flushed from the aquifer into subsurface drains by applying fresh water to the surface . Tests results for both aquifer types showed that tile drains placed near the ground surface will not intercept and discharge surface applied fresh water if all or part of the aquifer contains salt water... |
| Note de contenu : |
Aquifer swetening is studied in the laboratory using a rectangular, glass - Walled, sand - fielled tank. Two types of aquifer are studies (1) a 1:40 scale/ two - part aquifer (coarse and fine sand) representing a vertical cross section through and idéalizeportion of an irrieated valley, and (2)a fine sand, sigle part aquifer used to evaluate a formula derived from the ghyben - Herzberg principle for computing depth to a saline - fresh water interface . Salt water is flushed from the aquifer into subsurface drains by applying fresh water to the surface . Tests results for both aquifer types showed that tile drains placed near the ground surface will not intercept and discharge surface applied fresh water if all or part of the aquifer contains salt water... |
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