Soil Erosion Small Catchment Matijevića Brook (West Serbia)
Erozija zemlјišta malog sliva Matijevića potok (zapadna Srbija)
Author
Sekularac, Gordana
Djuric, Milena
Aksic, Miroljub
Jelic, Miodrag
Jakisic, Tanja
Keywords
catchmentsoil erosion
gully
sediment
sliv
erozijа zemljišta
vododerina
nanos
Metadata
Show full item recordAbstract
Due to a variety of both natural and anthropogenic erosion factors, the general
condition of the Matijevića brook torrential catchment area has contributed to the
overall picture of soil erosion intensity in the area. From the aspect of belonging to the
type of torrential flow stream Matijevića brook is the gully (F) with mean annual
erosion-induced sediment yield Wyear from 206,39 m3 year-1 and total annual specific
sediment yield at the confluence of the the Matijevića brook in Tinja (left tributary of
Kamenica, which the river flows into the West Morava with her left hand) where Ggod sp
-1
were 75.51 m3 km-2 yr-1. Usled različitih činilaca procesa erozije, prirodnih i antropogenog, opšti
uslovi područja bujičnog toka Matijevića potok, doprineli su sagledavanju intenziteta
erozije zemljišta sliva. Sa aspekta pripadnosti tipu bujičnog toka Matijevića potok je
vododerina (F) sa srednjegodišnjom količinom erozionog nanosa (Wgod) od 206,39 m3
god-1 i specifičnom godišnjom količinom ukupnog erozionog nanosa, koja dospeva do
ušća Matijevića potoka u Tinju (leva pritoka Kamenice, koja se u reku Zapadnu Moravu
uliva sa njene leve strane), Ggod sp
-1, od 75,51 m3 km-2 god-1.