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Hassan Jafari

غلام حسن جعفری فاطمه بختیاری
بررسي هيدرو- ژئونروتيك حوضه آبي قز لاوزن
Analyze of Hydro-Geoneurons of Ghezelozan Basin
Abstract


Analyze of geo-neurons of Ghezel Ozan basin, is done as a hydro-geo-neurotic by estimate, climatic information, soft wares like of Arc GIS, Surfer and excel. In this article to analyze of the drainage network neurotic system, is used the relationship between hydrology and climate data. Ghezel Ozan basin is divided into 56 sub basins, due to the attention to the place of the main shoots. Topo-geo- neuron, immemorial geo-neuron and virtual geo-neurons, were identified in accordance with the structures of basin pattern and attrition surfaces. The results showed that about 3792 square kilometers, the solid precipitation in Quaternary glaciers blocked and in some other way have played a role in the transformation of heights. The dominant landforms such a situation has been to form of glacier circus. In the downstream such landforms, despite of appropriate slope, linear probing surface water become glacier surface process and are created U-shaped glacial valleys and sometimes glacial acted to form of ice sheet and a total of landforms have shaped that will be remembered such as virtual geo-neuron. The neurons of Yanki Kand and Qalah Chay has acted as isolated topo-geo-neuron by the climate change of the region in Quaternary and melting of ice surfaces in middle of Ghezel Ozan basin. Zanjan Rood downstream, middle and along the Ghazal Ozan, of Bijar until Miyaneh is degenerative and amount of water they receive is much less than the water that comes out of them and if it were not rivers such as Anguran Chay, Qalah Chay and Qranqon Chay, Ghezel Ozan become dry completely.

 

 

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