Bibliographic citations
Frías, E., Mogollón, A. (2017). Simulación hidráulica bidimensional de las zonas de inundación aguas abajo del sector Huabalito - Chicama - 2017 [Tesis, Universidad Privada Antenor Orrego - UPAO]. https://hdl.handle.net/20.500.12759/4523
Frías, E., Mogollón, A. Simulación hidráulica bidimensional de las zonas de inundación aguas abajo del sector Huabalito - Chicama - 2017 [Tesis]. : Universidad Privada Antenor Orrego - UPAO; 2017. https://hdl.handle.net/20.500.12759/4523
@misc{renati/378519,
title = "Simulación hidráulica bidimensional de las zonas de inundación aguas abajo del sector Huabalito - Chicama - 2017",
author = "Mogollón Borrero, Angello Gianfranco",
publisher = "Universidad Privada Antenor Orrego - UPAO",
year = "2017"
}
The present project was developed in the sector of Huabalito-Chicama, which was one of the zones most affected by the phenomenon of the Coastal Child, this type of climatological disasters, two-dimensional flood zones downstream of the Huabalito-Chicama sector. The methodology presented through the processing and post-processing of field and processed data by integrating the Hec-Ras Hydraulic model with Sig-Arcview respectively is a reliable, technically efficient and economically reasonable alternative to our national reality and regional level. According to the results obtained from the model can be deduced from the alternative proposed for the protection of the access road to the left margin. In addition, we must point out that according to the observed values, they can conclude that with the flow obtained the sandstones that already have velocities of 3 m / s greater, which are a being for the transport of suspended materials in the bed of river. With the approach given can guarantee the adequate protection of the road to Huabalito-Punta Moreno Bridge, the agricultural areas bordering the banks and also the same protection infrastructure used as we have adequate balance widths and temporary structures such as son the pier appropriate way in the specific points of the channel. For this reason, it is now necessary for local and regional authorities to apply this method in the different stretches of the Chicama River and in other coastal countries, to quantify damages in possible future floods and to plan the necessary corrective measures.
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