Abstract
A mixture of heat-conducting viscous inert fluids is given the structure of material with hidden variables. As a consequence, a model for sediment transport is elaborated within the approximation of sediments as a dilute suspension. Such a model turns out to be hyperbolic and allows for exceptional transverse waves.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
