2019
DOI: 10.1016/j.scitotenv.2018.08.329
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Variations in bar material grain-size and hydraulic conditions of managed and re-naturalized reaches of the gravel-bed Bečva River (Czech Republic)

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Cited by 12 publications
(2 citation statements)
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“…Originally, it was a wandering gravel-bed river with the typical characteristics of an active channel with a hundred-metre width and an intensive bedload transport (Odra River Board State Enterprise, 2016). Such river patterns and processes were typical for neighbouring basins up to the first half of the 20th century before extensive regulation works were conducted (Škarpich, Galia, & Hradecký, 2016;Škarpich, Galia, Ruman, & Máčka, 2019). Currently, the river reach in Příbor has a degraded hydromorphological state, and two main types of pressure were identified by field evaluation.…”
Section: Study River Reach and River Assessmentmentioning
confidence: 96%
“…Originally, it was a wandering gravel-bed river with the typical characteristics of an active channel with a hundred-metre width and an intensive bedload transport (Odra River Board State Enterprise, 2016). Such river patterns and processes were typical for neighbouring basins up to the first half of the 20th century before extensive regulation works were conducted (Škarpich, Galia, & Hradecký, 2016;Škarpich, Galia, Ruman, & Máčka, 2019). Currently, the river reach in Příbor has a degraded hydromorphological state, and two main types of pressure were identified by field evaluation.…”
Section: Study River Reach and River Assessmentmentioning
confidence: 96%
“…They are shaped through the deposition and reworking of loose sedimentary material transported by the water flow to locations where there is a local decrease in transport capacity. This process is typically associated with the channel geometry, with deposits most often found on the inner banks of bends, in areas of local channel widening, or in zones with flow obstacles that allow for the dispersion of the flow energy (e.g., downstream transversal structures like check dams and weirs or behind stable large wood) (Abbe and Montgomery 1996;Hey et al 1982;Jaballah et al 2015;Škarpich et al 2019). These bars are typically described as "forced" due to their formation process, in contrast to "periodic bars", which are large sediment deposits formed as a result of morphodynamic instability (Duró et al 2016).…”
Section: Introductionmentioning
confidence: 99%