All rights reserved Miletić, Zoran Topalović, Milun Burlica, Čedomir application/pdf 4460895 bytes info:eu-repo/semantics/article Institut za šumarstvo srp Zbornik radova Instituta za šumarstvo number: 44-45 startpage: 21 endpage: 36 https://unilib.phaidrabg.rs/o:7114 ISSN: 0351-9147 Ispitivana su hidrološka svojstva zemljišta i vodni bilans po modelu Tornthweite-a na šest lokaliteta na serpentinitima. Za dve hidrološke godine od kojih je jedna znatno suvlja, a druga znatno vlažnija od prosečne. Za iste lokalitete ustanovljen je faktor erodibilnosti zemljišta po metodu R. Lala. Izvršeno je poređenje različitih evoluciono genetskih stadijuma zemljišta na serpentinitima u količini otekle vode i njihovoj erodiblinosti. Hydrological characteristics of the soil and water balance were researched after Tornthweite's model at six localities on serpentinites in two hydrological years of which one was considerably drier, and the other was considerably moister than the average. Factor of soil erodibility was determined for the same localities using R. Lat's method. Different evolution-genetic stages of the soil on serpentinites were compared regarding the quantity of runoff water and erodibility. HIDROLOŠKE KARAKTERISTIKE SERPENTINITSKIH ZEMLJIŠTA I NJIHOVA ERODIBILNOST HYDROLOGICAL CHARACTERISTICS OF SERPENTINITE SOILS AND THEIR ERODIBILITY serpentinites, soil type-, water infiltration and retention, runoff, erosion serpentiniti, tip zemljista, primanje i zadrzavanje vode, oticanje, erozija 2001