Titre de série : |
Geological survey water supply paper, 1798-L |
Titre : |
Sedimentation in small drainage basins : effect of land use and retention practices on sediment yields in the Stony Brook Basin, New Jersey |
Type de document : |
texte imprimé |
Auteurs : |
Mansue, L. J. ; Anderson, P. W. |
Mention d'édition : |
US Government printing office |
Editeur : |
US Government Printing Office |
Année de publication : |
1974 |
ISBN/ISSN/EAN : |
CI-08245 |
Note générale : |
The average annual rate of suspended sediment discharge of the Stony Brook at princeton, N. J. (44,5 square miles) is about 8,800 tons, or 200 tons per square mile. Annual yields within the basin, which is in the piedmont lowlands section of the piedmont physiographic province in west-central New Jersey, range from 25 to 400 tons per square mile. Storm runoff that transports suspended materials in excess of a ton carries 90 percent of the total suspended - sediments dischatge from the basin. |
Langues : |
Anglais (eng) |
Mots-clés : |
Sédimentation Qualité de l'eau Drainage Hydrologie Débit solide |
Index. décimale : |
551.48 Hydrologie : |
Résumé : |
The average annual rate of suspended sediment discharge of the Stony Brook at princeton, N. J. (44,5 square miles) is about 8,800 tons, or 200 tons per square mile. Annual yields within the basin, which is in the piedmont lowlands section of the piedmont physiographic province in west-central New Jersey, range from 25 to 400 tons per square mile. Storm runoff that transports suspended materials in excess of a ton carries 90 percent of the total suspended - sediments dischatge from the basin. |
Note de contenu : |
The average annual rate of suspended sediment discharge of the Stony Brook at princeton, N. J. (44,5 square miles) is about 8,800 tons, or 200 tons per square mile. Annual yields within the basin, which is in the piedmont lowlands section of the piedmont physiographic province in west-central New Jersey, range from 25 to 400 tons per square mile. Storm runoff that transports suspended materials in excess of a ton carries 90 percent of the total suspended - sediments dischatge from the basin. |
Geological survey water supply paper, 1798-L. Sedimentation in small drainage basins : effect of land use and retention practices on sediment yields in the Stony Brook Basin, New Jersey [texte imprimé] / Mansue, L. J. ; Anderson, P. W. . - US Government printing office . - US Government Printing Office, 1974. ISSN : CI-08245 The average annual rate of suspended sediment discharge of the Stony Brook at princeton, N. J. (44,5 square miles) is about 8,800 tons, or 200 tons per square mile. Annual yields within the basin, which is in the piedmont lowlands section of the piedmont physiographic province in west-central New Jersey, range from 25 to 400 tons per square mile. Storm runoff that transports suspended materials in excess of a ton carries 90 percent of the total suspended - sediments dischatge from the basin. Langues : Anglais ( eng)
Mots-clés : |
Sédimentation Qualité de l'eau Drainage Hydrologie Débit solide |
Index. décimale : |
551.48 Hydrologie : |
Résumé : |
The average annual rate of suspended sediment discharge of the Stony Brook at princeton, N. J. (44,5 square miles) is about 8,800 tons, or 200 tons per square mile. Annual yields within the basin, which is in the piedmont lowlands section of the piedmont physiographic province in west-central New Jersey, range from 25 to 400 tons per square mile. Storm runoff that transports suspended materials in excess of a ton carries 90 percent of the total suspended - sediments dischatge from the basin. |
Note de contenu : |
The average annual rate of suspended sediment discharge of the Stony Brook at princeton, N. J. (44,5 square miles) is about 8,800 tons, or 200 tons per square mile. Annual yields within the basin, which is in the piedmont lowlands section of the piedmont physiographic province in west-central New Jersey, range from 25 to 400 tons per square mile. Storm runoff that transports suspended materials in excess of a ton carries 90 percent of the total suspended - sediments dischatge from the basin. |
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