Hydraulic routing and unsteady flow Flashcards
Open Channel Hydraulic - assumptions
prismatic channel - cross section does not change
longitudinal dimension longer than transverse dimensions
bed slope «_space;1
incompressible flow -> water density is constant
steady uniform flow
change in time = o
change in direction = 0
steady non-uniform flow
change in time = 0
change in direction does not equal 0
Unsteady non-uniform flow
change in time does not equal 0
change in direction does not equal 0
Finite Difference Method
not able to get analytical solution for most of the case of ODE and PDE’s
FDM needed to solve numerically
the method approximates its derivatives, PDE/ODE can be expressed by function itself and then solved numerically