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Auteur Schumm, S. A. |
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Titre : A geomorphic approach to erosion control in semiarid regions Type de document : texte imprimé Auteurs : Schumm, S. A. Mention d'édition : Washington (US) Editeur : Washington (US) Année de publication : 1969 ISBN/ISSN/EAN : CI-03829 Note générale : "In this paper, which is a review of roughly ten years of research concerning semi-arid land forms, an attempt has been made view erosional and depositional phenomena from a geomorphic perspective. The question that has been asked in each case was: ""How does the system function ?"". This emphasis on the processes of landscape modification a quantitative description of landforms has provided information on the origin of certain features, and a means of delineating critical areas of the landscape where conservation techniques should be able to provide further assistance to the conservation engineer when newly developed techniques of landform study re employed. The emphasis in this paper, has been on the relations existing between erosion and deposition and landform characteristics." Langues : Anglais (eng) Mots-clés : Géomorphologie Erosion Télédetection Vallée Alluvion Hydrologie Géologie Végétation PRECIPITATIONS Agriculture Drainage Index. décimale : 631.45 Erosion et lutte anti-érosion 631.46 Résumé : "In this paper, which is a review of roughly ten years of research concerning semi-arid land forms, an attempt has been made view erosional and depositional phenomena from a geomorphic perspective. The question that has been asked in each case was: ""How does the system function ?"". This emphasis on the processes of landscape modification a quantitative description of landforms has provided information on the origin of certain features, and a means of delineating critical areas of the landscape where conservation techniques should be able to provide further assistance to the conservation engineer when newly developed techniques of landform study re employed. The emphasis in this paper, has been on the relations existing between erosion and deposition and landform characteristics." Note de contenu : "In this paper, which is a review of roughly ten years of research concerning semi-arid land forms, an attempt has been made view erosional and depositional phenomena from a geomorphic perspective. The question that has been asked in each case was: ""How does the system function ?"". This emphasis on the processes of landscape modification a quantitative description of landforms has provided information on the origin of certain features, and a means of delineating critical areas of the landscape where conservation techniques should be able to provide further assistance to the conservation engineer when newly developed techniques of landform study re employed. The emphasis in this paper, has been on the relations existing between erosion and deposition and landform characteristics." A geomorphic approach to erosion control in semiarid regions [texte imprimé] / Schumm, S. A. . - Washington (US) . - Washington (US), 1969.
ISSN : CI-03829
"In this paper, which is a review of roughly ten years of research concerning semi-arid land forms, an attempt has been made view erosional and depositional phenomena from a geomorphic perspective. The question that has been asked in each case was: ""How does the system function ?"". This emphasis on the processes of landscape modification a quantitative description of landforms has provided information on the origin of certain features, and a means of delineating critical areas of the landscape where conservation techniques should be able to provide further assistance to the conservation engineer when newly developed techniques of landform study re employed. The emphasis in this paper, has been on the relations existing between erosion and deposition and landform characteristics."
Langues : Anglais (eng)
Mots-clés : Géomorphologie Erosion Télédetection Vallée Alluvion Hydrologie Géologie Végétation PRECIPITATIONS Agriculture Drainage Index. décimale : 631.45 Erosion et lutte anti-érosion 631.46 Résumé : "In this paper, which is a review of roughly ten years of research concerning semi-arid land forms, an attempt has been made view erosional and depositional phenomena from a geomorphic perspective. The question that has been asked in each case was: ""How does the system function ?"". This emphasis on the processes of landscape modification a quantitative description of landforms has provided information on the origin of certain features, and a means of delineating critical areas of the landscape where conservation techniques should be able to provide further assistance to the conservation engineer when newly developed techniques of landform study re employed. The emphasis in this paper, has been on the relations existing between erosion and deposition and landform characteristics." Note de contenu : "In this paper, which is a review of roughly ten years of research concerning semi-arid land forms, an attempt has been made view erosional and depositional phenomena from a geomorphic perspective. The question that has been asked in each case was: ""How does the system function ?"". This emphasis on the processes of landscape modification a quantitative description of landforms has provided information on the origin of certain features, and a means of delineating critical areas of the landscape where conservation techniques should be able to provide further assistance to the conservation engineer when newly developed techniques of landform study re employed. The emphasis in this paper, has been on the relations existing between erosion and deposition and landform characteristics." Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03829.158674 CI-03829 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03829.158673 CI-03829 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03829.158672 CI-03829 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03829.158671 CI-03829 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03829.158670 CI-03829 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03829.158669 CI-03829 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03829.158668 CI-03829 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03829.158667 CI-03829 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible
Titre : The fluvial system Type de document : texte imprimé Auteurs : Schumm, S. A. Mention d'édition : John Villey & Sons Editeur : John Villey & Sons Année de publication : 1977 ISBN/ISSN/EAN : 0-47-01901-1 Note générale : This book is an attempt to consider the fluvial system and its component in such a way that the interaction of the component and the resluting degree of inherent instability of the system can be comprehended and related to some concerns of the economics geologist, geomorphologist, stratigrapher, sedimentologist, land manager, conservationist, and civil engineer. A new way of viewing thr fluvial system is presented that can aid in the explanatsion of complexity of landscape evolution. Langues : Anglais (eng) Mots-clés : Versant Hydrologie Ruissellement Climatologie Erosion hydrique Vallée Réseau hydrographique Morphologie Océanographie Index. décimale : 551.48 Hydrologie : Résumé : This book is an attempt to consider the fluvial system and its component in such a way that the interaction of the component and the resluting degree of inherent instability of the system can be comprehended and related to some concerns of the economics geologist, geomorphologist, stratigrapher, sedimentologist, land manager, conservationist, and civil engineer. A new way of viewing thr fluvial system is presented that can aid in the explanatsion of complexity of landscape evolution. Note de contenu : This book is an attempt to consider the fluvial system and its component in such a way that the interaction of the component and the resluting degree of inherent instability of the system can be comprehended and related to some concerns of the economics geologist, geomorphologist, stratigrapher, sedimentologist, land manager, conservationist, and civil engineer. A new way of viewing thr fluvial system is presented that can aid in the explanatsion of complexity of landscape evolution. The fluvial system [texte imprimé] / Schumm, S. A. . - John Villey & Sons . - John Villey & Sons, 1977.
ISSN : 0-47-01901-1
This book is an attempt to consider the fluvial system and its component in such a way that the interaction of the component and the resluting degree of inherent instability of the system can be comprehended and related to some concerns of the economics geologist, geomorphologist, stratigrapher, sedimentologist, land manager, conservationist, and civil engineer. A new way of viewing thr fluvial system is presented that can aid in the explanatsion of complexity of landscape evolution.
Langues : Anglais (eng)
Mots-clés : Versant Hydrologie Ruissellement Climatologie Erosion hydrique Vallée Réseau hydrographique Morphologie Océanographie Index. décimale : 551.48 Hydrologie : Résumé : This book is an attempt to consider the fluvial system and its component in such a way that the interaction of the component and the resluting degree of inherent instability of the system can be comprehended and related to some concerns of the economics geologist, geomorphologist, stratigrapher, sedimentologist, land manager, conservationist, and civil engineer. A new way of viewing thr fluvial system is presented that can aid in the explanatsion of complexity of landscape evolution. Note de contenu : This book is an attempt to consider the fluvial system and its component in such a way that the interaction of the component and the resluting degree of inherent instability of the system can be comprehended and related to some concerns of the economics geologist, geomorphologist, stratigrapher, sedimentologist, land manager, conservationist, and civil engineer. A new way of viewing thr fluvial system is presented that can aid in the explanatsion of complexity of landscape evolution. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B929.114939 CI-07929 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B929.114940 CI-07929 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B929.114941 CI-07929 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B929.114942 CI-07929 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B929.114943 CI-07929 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B929.114944 CI-07929 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B929.114945 CI-07929 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B929.114946 CI-07929 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible
Titre de série : Transaction, 6 Titre : Yield of sediment in relation to mean annual precipitation Type de document : texte imprimé Auteurs : Langbein, W. B. ; Schumm, S. A. Année de publication : 1958 ISBN/ISSN/EAN : CI-03560 Note générale : Effective man annual precipation is related to sediment yiel from drainage basins throughout the climatic regions of the united states. Sediment yield is a maximum at about 10 to 14 inches of precipitation, decreasing sharply on both sides of this maximum, in on case owing to a deficiency of runoff and in the other to increased density of vegetation. Data are presented illustrating the increase in bulk density of vegatative density. It is suggested that the effect of a vlimatic change of sediment yield depends not only upon direction of climate change, but also on the climate before the change sediment concentration in runoff is shown to increase with decreased annual precipitation, suggesting further that a decrease in precipitation will cause stream channel degradation Langues : Anglais (eng) Mots-clés : PRECIPITATIONS Evapotranspiration Climat Drainage Végétation Erosion Géologie Sédimentation Index. décimale : 631.45 Erosion et lutte anti-érosion 631.46 Résumé : Effective man annual precipation is related to sediment yiel from drainage basins throughout the climatic regions of the united states. Sediment yield is a maximum at about 10 to 14 inches of precipitation, decreasing sharply on both sides of this maximum, in on case owing to a deficiency of runoff and in the other to increased density of vegetation. Data are presented illustrating the increase in bulk density of vegatative density. It is suggested that the effect of a vlimatic change of sediment yield depends not only upon direction of climate change, but also on the climate before the change sediment concentration in runoff is shown to increase with decreased annual precipitation, suggesting further that a decrease in precipitation will cause stream channel degradation Note de contenu : Effective man annual precipation is related to sediment yiel from drainage basins throughout the climatic regions of the united states. Sediment yield is a maximum at about 10 to 14 inches of precipitation, decreasing sharply on both sides of this maximum, in on case owing to a deficiency of runoff and in the other to increased density of vegetation. Data are presented illustrating the increase in bulk density of vegatative density. It is suggested that the effect of a vlimatic change of sediment yield depends not only upon direction of climate change, but also on the climate before the change sediment concentration in runoff is shown to increase with decreased annual precipitation, suggesting further that a decrease in precipitation will cause stream channel degradation Transaction, 6. Yield of sediment in relation to mean annual precipitation [texte imprimé] / Langbein, W. B. ; Schumm, S. A. . - 1958.
ISSN : CI-03560
Effective man annual precipation is related to sediment yiel from drainage basins throughout the climatic regions of the united states. Sediment yield is a maximum at about 10 to 14 inches of precipitation, decreasing sharply on both sides of this maximum, in on case owing to a deficiency of runoff and in the other to increased density of vegetation. Data are presented illustrating the increase in bulk density of vegatative density. It is suggested that the effect of a vlimatic change of sediment yield depends not only upon direction of climate change, but also on the climate before the change sediment concentration in runoff is shown to increase with decreased annual precipitation, suggesting further that a decrease in precipitation will cause stream channel degradation
Langues : Anglais (eng)
Mots-clés : PRECIPITATIONS Evapotranspiration Climat Drainage Végétation Erosion Géologie Sédimentation Index. décimale : 631.45 Erosion et lutte anti-érosion 631.46 Résumé : Effective man annual precipation is related to sediment yiel from drainage basins throughout the climatic regions of the united states. Sediment yield is a maximum at about 10 to 14 inches of precipitation, decreasing sharply on both sides of this maximum, in on case owing to a deficiency of runoff and in the other to increased density of vegetation. Data are presented illustrating the increase in bulk density of vegatative density. It is suggested that the effect of a vlimatic change of sediment yield depends not only upon direction of climate change, but also on the climate before the change sediment concentration in runoff is shown to increase with decreased annual precipitation, suggesting further that a decrease in precipitation will cause stream channel degradation Note de contenu : Effective man annual precipation is related to sediment yiel from drainage basins throughout the climatic regions of the united states. Sediment yield is a maximum at about 10 to 14 inches of precipitation, decreasing sharply on both sides of this maximum, in on case owing to a deficiency of runoff and in the other to increased density of vegetation. Data are presented illustrating the increase in bulk density of vegatative density. It is suggested that the effect of a vlimatic change of sediment yield depends not only upon direction of climate change, but also on the climate before the change sediment concentration in runoff is shown to increase with decreased annual precipitation, suggesting further that a decrease in precipitation will cause stream channel degradation Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B560.180842 CI-03560 Rapport Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B560.180841 CI-03560 Rapport Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B560.180839 CI-03560 Rapport Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B560.180840 CI-03560 Rapport Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B560.180837 CI-03560 Rapport Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B560.180838 CI-03560 Rapport Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B560.180836 CI-03560 Rapport Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B560.180835 CI-03560 Rapport Bibliothèque CDI-Ouaga Fond documentaire Disponible
