Karst aquifer impact on the formation of surface runoff: case study of the Resava River catchment, Serbia

Објеката

Тип
Рад у зборнику
Верзија рада
објављена
Језик
енглески
Креатор
Marina Mitrašinović, Vesna Ristić Vakanjac, Veljko Marinović, Saša Milanović, Ljiljana Vasić, Dušan Polomčić
Извор
National Conference with International Participation “GEOSCIENCES 2022”
Издавач
Sofia : Bulgarian geological society
Датум издавања
2022
Сажетак
The paper compares the flow regimes of the Resava River at the gauging stations of the Manasija Monastery (upper course) and the town of Svilajnac (lower course). The hydrological analysis encompasses a multiyear period of monitoring (1982–2020). The water budget and baseflow index are assessed for the catchment areas monitored by the Svilajnac station (683 km2) and the Manasija Monastery station (358k m2), considering the overall monitoring period and characteristic years. The results indicate that the specific runoff in the upper catchment is about 50% higher than that of the entire catchment. The reason is that the upper catchment is 55 % karst, whereas the remainder is non-karst. The situation is similar in dry years. However, in wet years the specific runoff of the entire catchment is higher than that of the upper catchment.
почетак странице
255
крај странице
258
Просторно покривање
Sliv reke Resave
Subject
hydrogeological characteristics, water regime, water balance, karst aquifer, Resava catchment area
Шира категорија рада
М30
Ужа категорија рада
М33
Права
Отворени приступ
Лиценца
Creative Commons – Attribution-NonComercial 4.0 International
Формат
.pdf

Marina Mitrašinović, Vesna Ristić Vakanjac, Veljko Marinović, Saša Milanović, Ljiljana Vasić, Dušan Polomčić. "Karst aquifer impact on the formation of surface runoff: case study of the Resava River catchment, Serbia" in National Conference with International Participation “GEOSCIENCES 2022”, Sofia : Bulgarian geological society (2022)

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