Titre de série : |
US Geological Survey Water-Supply Paper, 2071 |
Titre : |
Sediment, trap efficiency of a multiple purpose impoundment, north branch rack creek basin, Montgomery country, Maryland, 1968-76 |
Type de document : |
texte imprimé |
Auteurs : |
Herb, W.J. |
Mention d'édition : |
US Government Printing Office |
Editeur : |
US Government Printing Office |
Année de publication : |
1988 |
ISBN/ISSN/EAN : |
CI-09427 |
Note générale : |
Lake Bernard Frank, a multiple-purpose reservoir in montgomery country MD, impounds runoff and sediment from 12-5 square miles of the upper north branch rach creek basin. Sediment trap efficiency was studied by the U.S Geological Survey between 1967 and 1976. Suspended sediment inflow to the impoundment for unmerasured storm period in 1968-76 was estimated from daily suspended sediment transport curves. Bedlood contribution was estimated by the Schoklitsch and Meyer-peter and Muller bedload, transport equation... |
Langues : |
Anglais (eng) |
Mots-clés : |
Géologie Topographie Hydrologie Ruissellement Débit solide |
Index. décimale : |
551.48 Hydrologie : |
Résumé : |
Lake Bernard Frank, a multiple-purpose reservoir in montgomery country MD, impounds runoff and sediment from 12-5 square miles of the upper north branch rach creek basin. Sediment trap efficiency was studied by the U.S Geological Survey between 1967 and 1976. Suspended sediment inflow to the impoundment for unmerasured storm period in 1968-76 was estimated from daily suspended sediment transport curves. Bedlood contribution was estimated by the Schoklitsch and Meyer-peter and Muller bedload, transport equation... |
Note de contenu : |
Lake Bernard Frank, a multiple-purpose reservoir in montgomery country MD, impounds runoff and sediment from 12-5 square miles of the upper north branch rach creek basin. Sediment trap efficiency was studied by the U.S Geological Survey between 1967 and 1976. Suspended sediment inflow to the impoundment for unmerasured storm period in 1968-76 was estimated from daily suspended sediment transport curves. Bedlood contribution was estimated by the Schoklitsch and Meyer-peter and Muller bedload, transport equation... |
US Geological Survey Water-Supply Paper, 2071. Sediment, trap efficiency of a multiple purpose impoundment, north branch rack creek basin, Montgomery country, Maryland, 1968-76 [texte imprimé] / Herb, W.J. . - US Government Printing Office . - US Government Printing Office, 1988. ISSN : CI-09427 Lake Bernard Frank, a multiple-purpose reservoir in montgomery country MD, impounds runoff and sediment from 12-5 square miles of the upper north branch rach creek basin. Sediment trap efficiency was studied by the U.S Geological Survey between 1967 and 1976. Suspended sediment inflow to the impoundment for unmerasured storm period in 1968-76 was estimated from daily suspended sediment transport curves. Bedlood contribution was estimated by the Schoklitsch and Meyer-peter and Muller bedload, transport equation... Langues : Anglais ( eng)
Mots-clés : |
Géologie Topographie Hydrologie Ruissellement Débit solide |
Index. décimale : |
551.48 Hydrologie : |
Résumé : |
Lake Bernard Frank, a multiple-purpose reservoir in montgomery country MD, impounds runoff and sediment from 12-5 square miles of the upper north branch rach creek basin. Sediment trap efficiency was studied by the U.S Geological Survey between 1967 and 1976. Suspended sediment inflow to the impoundment for unmerasured storm period in 1968-76 was estimated from daily suspended sediment transport curves. Bedlood contribution was estimated by the Schoklitsch and Meyer-peter and Muller bedload, transport equation... |
Note de contenu : |
Lake Bernard Frank, a multiple-purpose reservoir in montgomery country MD, impounds runoff and sediment from 12-5 square miles of the upper north branch rach creek basin. Sediment trap efficiency was studied by the U.S Geological Survey between 1967 and 1976. Suspended sediment inflow to the impoundment for unmerasured storm period in 1968-76 was estimated from daily suspended sediment transport curves. Bedlood contribution was estimated by the Schoklitsch and Meyer-peter and Muller bedload, transport equation... |
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