Muskingum

Muskingum路由單元可模擬自然水流

The Muskingum Routing calculates the discharge within a river or channel reach given the inflow hydrograph at the upstream end. The unit is based on the continuity equation and the Muskingum storage relationship (McCarthy G.T. (1938)).

Cross section details are not required and only the Muskingum parameters k and x are specified. Both parameters are fixed. A minimum of two Muskingum Routing sections are required for each end of the river or channel reach.

| Titular derecho patrimonial: Universidad Distrital Francisco José de Caldas. Copyrights © | Bogotá D. C. | Colombia |

Autores:

Edgar Orlando Ladino Moreno

Cesar Augusto Garcia Ubaque

Jorge Arturo Pineda Jaimes