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dc.creatorDragičević, Slavoljub
dc.creatorPripuzić, Mirjana
dc.creatorŽivković, Nenad
dc.creatorNovković, Ivan
dc.creatorKostadinov, Stanimir
dc.creatorLangović, Marko
dc.creatorMilojković, Boban
dc.creatorČvorović, Zoran
dc.date.accessioned2019-03-21T16:10:06Z
dc.date.available2019-03-21T16:10:06Z
dc.date.issued2017
dc.identifier.issn2073-4441
dc.identifier.urihttp://jakov.kpu.edu.rs/handle/123456789/773
dc.description.abstractThe fluvial process is characterized by an intense meandering riverbed. The aim of this study was to perform a reconstruction of the lateral migration of a 15 km length of an active meandering river during the period 1930-2016. River morphological changes were analyzed and quantified from cadastral maps and aerial photographs as well as by geodetic survey and GIS. Hydrological characteristics and extreme hydrological events were evaluated in relation to bank erosion rate. The rate of bank erosion was markedly different from the long-term studied meanders, just like in the short-term period. During the 87 years of observation (from 1930 to 2016), the length of the Kolubara River was enlarged by 3.44 km. The average migration rate of the Kolubara River for monitored meanders in the period 1930-2010 was 1.9 myear(-1), while in the period 2010-2016, the average migration rate was 3.3 myear(-1). The rate of bank erosion was more intensive across the entire short-term period than during the longer period, and the maximum annual rate of bank erosion during the period 2010-2016 varied between 0.3 and 11.5 m. It is very likely that in the period from 2010, frequent discharge variations and rapid change of its extreme values caused more intensive bank erosion. These research results will be valuable for river channel management, engineering (soft and hard engineering), and planning purposes (predicting changes in river channel form) in the Kolubara River Basin.en
dc.publisherMDPI AG
dc.relationinfo:eu-repo/grantAgreement/MESTD/Integrated and Interdisciplinary Research (IIR or III)/43007/RS//
dc.rightsopenAccess
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.sourceWater
dc.subjectchannel migrationen
dc.subjectriverbank erosion and accretionen
dc.subjectbank-full dischargeen
dc.subjectKolubara Riveren
dc.titleSpatial and Temporal Variability of Bank Erosion during the Period 1930-2016: Case StudyKolubara River Basin (Serbia)en
dc.typearticle
dc.rights.licenseBY
dcterms.abstractЛанговић, Марко; Припузић, Мирјана; Новковић, Иван; Милојковић, Бобан; Костадинов, Станимир; Чворовић, Зоран; Драгичевић, Славољуб; Живковић, Ненад;
dc.citation.volume9
dc.citation.issue10
dc.citation.other9(10): -
dc.citation.rankM22
dc.identifier.doi10.3390/w9100748
dc.identifier.fulltexthttp://jakov.kpu.edu.rs/bitstream/id/2846/771.pdf
dc.identifier.scopus2-s2.0-85030542900
dc.identifier.wos000414707500025
dc.type.versionpublishedVersion


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