To define or predict incipient motion in an alluvial channel, most of the investigators use a standard or modified form of Shields- diagram. Shields- diagram does give a process to determine the incipient motion parameters but an iterative one. To design properly (without iteration), one should have another equation for resistance. Absence of a universal resistance equation also magnifies the difficulties in defining the model. Neural network technique, which is particularly useful in modeling a complex processes, is presented as a tool complimentary to modeling incipient motion. Present work develops a neural network model employing the RBF network to predict the average velocity u and water depth y based on the experimental data on incipi...
An accurate prediction of roughness coefficient is of substantial importance for river management. T...
Abstract. Experimental and Neural network modeling investigation were completed to study the resista...
The flow resistance of an alluvial channel flow is not only affected by the Reynolds number and th...
The design of an alluvial channel for critical conditions requires information about four basic para...
Seepage through sand bed channels in a downward direction (suction) reduces the stability of particl...
The resistance to flow in an open channel is associated with the value of the Darcy-Weisbach frictio...
This study investigates the performance of artificial neural networks in predicting the incipient se...
[1] Incipient motion of particles on a river bed can, in principle, be understood and predicted from...
An artificial neural network (ANN) was developed to predict the depth-integrated alongshore suspende...
Regime width of alluvial channels is a vital problem in river morphology and channel design. Many eq...
The amount of sand moving parallel to a coastline forms a prerequisite for many harbor design projec...
Prediction of highly non linear behavior of suspended sediment flow in rivers has prime importance i...
A vital topic regarding the optimum and economical design of rigid boundary open channels such as se...
The current study aims to verify the existing equations for incipient motion for a rigid rectangular...
The main objective of the present work is to predict the longitudinal dispersion coefficient in natu...
An accurate prediction of roughness coefficient is of substantial importance for river management. T...
Abstract. Experimental and Neural network modeling investigation were completed to study the resista...
The flow resistance of an alluvial channel flow is not only affected by the Reynolds number and th...
The design of an alluvial channel for critical conditions requires information about four basic para...
Seepage through sand bed channels in a downward direction (suction) reduces the stability of particl...
The resistance to flow in an open channel is associated with the value of the Darcy-Weisbach frictio...
This study investigates the performance of artificial neural networks in predicting the incipient se...
[1] Incipient motion of particles on a river bed can, in principle, be understood and predicted from...
An artificial neural network (ANN) was developed to predict the depth-integrated alongshore suspende...
Regime width of alluvial channels is a vital problem in river morphology and channel design. Many eq...
The amount of sand moving parallel to a coastline forms a prerequisite for many harbor design projec...
Prediction of highly non linear behavior of suspended sediment flow in rivers has prime importance i...
A vital topic regarding the optimum and economical design of rigid boundary open channels such as se...
The current study aims to verify the existing equations for incipient motion for a rigid rectangular...
The main objective of the present work is to predict the longitudinal dispersion coefficient in natu...
An accurate prediction of roughness coefficient is of substantial importance for river management. T...
Abstract. Experimental and Neural network modeling investigation were completed to study the resista...
The flow resistance of an alluvial channel flow is not only affected by the Reynolds number and th...