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.
| Patrimonial right holder: Francisco José de Caldas District University. Copyrights © | Bogotá D. C. | Colombia |
Authors:
Edgar Orlando Ladino Moreno
Cesar Augusto Garcia Ubaque
Jorge Arturo Pineda Jaimes
__________________________
Clarification: The tool developed is pedagogical and educational. The use of this tool in real scenarios is the direct responsibility of the person who implements it. The authors are not responsible for the results generated by the application under real conditions.
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.
| Patrimonial right holder: Francisco José de Caldas District University. Copyrights © | Bogotá D. C. | Colombia |
Authors:
Edgar Orlando Ladino Moreno
Cesar Augusto Garcia Ubaque
Jorge Arturo Pineda Jaimes
__________________________
Clarification: The tool developed is pedagogical and educational. The use of this tool in real scenarios is the direct responsibility of the person who implements it. The authors are not responsible for the results generated by the application under real conditions.
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