Differences using measured and calculated solar radiation in order to estimate the temperature of the conductor in overhead lines
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Domingo Fernández, Rodrigo; González Diego, Antonio; Mañana Canteli, Mario; Arroyo Gutiérrez, Alberto; Cavia Soto, María de los Ángeles; Olmo de Celis, Cesar Juan delFecha
2016-05Derechos
© The European Association for the Development of Renewable Energies, Environment and Power Quality (EA4EPQ)
Publicado en
Renewable Energy & Power Quality Journal (RE&PQJ), 2016, 1(14), 780-784
International Conference on Renewable Energies and Power Quality (ICREPQ'16), Madrid
Editorial
The European Association for the Development of Renewable Energies, Environment and Power Quality (EA4EPQ)
Palabras clave
Conductor temperature
Ampacity
Solar radiation
Pyranometer
Resumen/Abstract
In the last 20 years, installed wind power capacity in North of Spain has grown from 24 to more than 1,650 MW. In this geographical region, wind energy farms are located in places that are far away from the transmission networks so they have to be integrated into distribution networks. Build new overhead lines dedicated for a distribution energy is not the best way to increase the evacuation energy of the wind farms because the cost is quite strong. So, the aim to solve these issues, is by means of an increase in the capacity of existing lines using the dynamic management of the network. This paper is devoted to show the difference of the conductor temperature between the parameter of solar radiation measured by a pyranometer and the use of the theoretical solar radiation which is explained in CIGRE TB601 [1] and IEEE Std. 738-2012 [2] algorithms.
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