Саопштење са скупа штампано у изводу

објављена

енглески

Marina Čokorilo Ilić, Vesna Ristić Vakanjac, Dušan Polomčić, Dragoljub Bajić, Jelena Ratković, Bojan Hajdin

Mathematical modeling to define catchment size and real evapotranspiration (case study: Andrića karst spring, Western Serbia)

National Conference with international participation “GEOSCIENCES 2018”

Bulgarian Geological Sciety

2018

Water resources in karst are extremely important sources of drinking water supply. The quality of groundwater formed in karst aquifers is generally high and in most cases only chlorination is required. However, from a hydrogeological perspective, these water resources are the least studied. Often only basic information is available on catchment size, groundwater reserves (dynamic and static, if any) and groundwater balance. Detailed hydrogeological investigations and long-term monitoring of karst spring discharges are needed to acquire such information. In Serbia, only one spring (the source of the Mlava River) is being continuously monitored. Other karst springs are either not monitored at all or observed for short periods of time, usually to address a specific problem. In 1995, the National Hydrometeorological Service of Serbia established gauging stations at another 5 karst springs, including Andrića Vrelo (Andrića Spring) in Western Serbia, Zlatibor District. Monitoring of the 5 springs was discontinued between 2004 and 2006.

135

136

0007-3938

Zapadna Srbija

karstno vrelo, veličina sliva, stvarna evapotranspiracija, karstno vrelo Andrića

karst spring, catchment size, real evapotranspiration, Andrića karst spring

М30

М34

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Creative Commons – Attribution-NonComercial-Share Alike 4.0 International

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