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Rečni meandri na kraških poljih
Author(s) -
Luka Černuta
Publication year - 2010
Publication title -
dela
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.162
H-Index - 8
eISSN - 1854-1089
pISSN - 0354-0596
DOI - 10.4312/dela.34.7.115-141
Subject(s) - geography , humanities , hydrology (agriculture) , forestry , geology , geotechnical engineering , art
Rečni meandri predstavljajo najpogostejšo tlorisno obliko nižinskih rek. Na (pre)oblikovanje rečnih meandrov na kraških poljih najizraziteje vpliva režim poplavnih voda. Poplave namreč narekujejo prostorsko-časovno conacijo meandrotvornih procesov, od česar zavisi obstoj meandrotvorno aktivne oziroma meandrotvorno pasivne faze razvoja meandrov. Šolski primer meandrov, nastalih zaradi delovanja in součinkovanja preučevanih meandrotvornih procesov, predstavljajo meandri Dobravke na Radenskem polju.River meanders present the most frequent planform of lowland rivers. Their formation on poljes mostly depends on flood water regime. Flooding dictates space-time zonation of meandering processes, of which the existence of active or passive phase of planform modification depends. Studied meanders of the stream Dobravka on the Radensko polje represent an excellent example of meanders (re)formed by meandering processes (inter)actions

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