CER59RJG9.Includes bibliographical references (page 17).The characteristics of the bed and the water surface in an alluvial channel are changed by changing the characteristics of the flow, the fluid, and/or the sediment. This paper first reviews the existing literature on the characteristics of bed forms and regimes of flow over an alluvial bed and then it reports the studies made by the writers about the scale of ripples and dunes and about the criteria for the prediction of different regimes of flow in an alluvial channel
Data compiled from standardized procedures for width measurement at established streamflow gaging st...
Alluvial rivers, insofar as they transport the material of which their channels are composed, posses...
Bank full discharge is generally considered to be the dominant steady flow which would generate the ...
CER61DBS79.Includes bibliographical references.From: Transactions of the American Society of Civil E...
CER59DBS34.Includes bibliographical references (page 42).Alluvial channel stage-discharge and depth-...
CER64DBS-CRM34.Includes bibliographical references.Offered for presentation at Sixth Congress of ICI...
CER83-84PYJ-DBS45.Includes bibliographical references (pages 29-40).April, 1984.April, 1984. Revised...
The reliability of predictors for friction factors and rates of sediment transport in alluvial chann...
The present study intended to review the historical development of the regime geometry equations pro...
Sediment transport and associated morphological changes in alluvial rivers occur primarily underunst...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary S...
The development of sand bed morphology in response to steady uniform flow is well described by phase...
In this study, experiments were performed in a curvilinear cross-sectional threshold alluvial channe...
Alluvial river channels are self-formed by the sediment-laden flow that is supplied to them from ups...
Meander flow takes place in one single channel which oscillates more orless regularly with amplitude...
Data compiled from standardized procedures for width measurement at established streamflow gaging st...
Alluvial rivers, insofar as they transport the material of which their channels are composed, posses...
Bank full discharge is generally considered to be the dominant steady flow which would generate the ...
CER61DBS79.Includes bibliographical references.From: Transactions of the American Society of Civil E...
CER59DBS34.Includes bibliographical references (page 42).Alluvial channel stage-discharge and depth-...
CER64DBS-CRM34.Includes bibliographical references.Offered for presentation at Sixth Congress of ICI...
CER83-84PYJ-DBS45.Includes bibliographical references (pages 29-40).April, 1984.April, 1984. Revised...
The reliability of predictors for friction factors and rates of sediment transport in alluvial chann...
The present study intended to review the historical development of the regime geometry equations pro...
Sediment transport and associated morphological changes in alluvial rivers occur primarily underunst...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary S...
The development of sand bed morphology in response to steady uniform flow is well described by phase...
In this study, experiments were performed in a curvilinear cross-sectional threshold alluvial channe...
Alluvial river channels are self-formed by the sediment-laden flow that is supplied to them from ups...
Meander flow takes place in one single channel which oscillates more orless regularly with amplitude...
Data compiled from standardized procedures for width measurement at established streamflow gaging st...
Alluvial rivers, insofar as they transport the material of which their channels are composed, posses...
Bank full discharge is generally considered to be the dominant steady flow which would generate the ...