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

Marina Mitrašinović, Vesna Ristić Vakanjac, Veljko Marinović, S. Milanović, Ljiljana Vasić, D. Polomcic
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Abstract

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.
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岩溶含水层对地表径流形成的影响:以塞尔维亚雷萨瓦河流域为例
本文比较了Manasija修道院(上游)和Svilajnac镇(下游)测量站的Resava河的流态。水文分析包括多年监测期(1982-2020年)。考虑到总体监测期和特征年,对Svilajnac站(683 km2)和Manasija修道院站(358k m2)监测的集水区的水量预算和基流指数进行了评估。结果表明,上游流域的比径流量比整个流域高出约50%。原因是上游集水区55%为岩溶,而其余部分为非岩溶。干旱年份的情况类似。然而,在丰水年份,整个集水区的比径流量高于上游集水区的比径流。
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