Stony debris flow transits to sediment sheet when the river bed gradient becomes gentle. The consists of a water layer and moving layer. Fine sediments are expected behave as part fluid rather than solid phase in Further, it can be thought that fine suspended However, was not possible physically express whether behaves or numerical simulation model. Here we modeled behavior flow. We confirmed a...

In this work, an inverse finite element formulation was modified for considering material anisotropy in obtaining blank shape and forming severity of deep drawn orthotropic parts. In this procedure, geometry of final part and thickness of initial blank sheet were known. After applying ideal forming formulations between material points of initial blank and final shape, an equation system was obt...