Based on a several years long record of water levels and temperatures in caves between Planinsko polje and the springs of Ljubljanica. Correlation between the data, the discharge of the Unica river and the meteorological data gave new insights into the groundwater dynamics in relation to the recharge events as well as into the hydrological role of Planinsko polje. The work clearly demonstrates caves as important observation points in karst hydrology.
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 "Dynamics Of Underground Water In The Karst Catchment Area Of The Ljubljanica Springs; Dinamika podzemne vode v kraskem zaledju izvirov Ljubljanice")
