2018
DOI: 10.3390/w10050556
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The Impact of Shrubby Floodplain Vegetation Growth on the Discharge Capacity of River Valleys

Abstract: Willow bush growing in floodplains is a dominant form of vegetation in lowland river valleys due to the availability of water and light. Uncontrolled growth of this plant results in a lower capacity of floodplain areas. Vegetation can narrow the active width of water flow, as well as change water flow velocities at hydrometric verticals falling within the floodplain and the main channel. This paper analyses the impact of long-term growth of willow shrubs on flow resistance coefficient values. Both an increase … Show more

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Cited by 14 publications
(6 citation statements)
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“…Very important aspects of protection analyses are studies of riverbed and catchment capacity, which were conducted by Walczak et al (2018) and Laks et al Hämmerling, M., Walczak, N., Walczak, Z., Zawadzki, P. (2019). Assessment of technical conditions of bank protection of watercourses and reservoirs in the city of Poznań.…”
Section: Discussionmentioning
confidence: 99%
“…Very important aspects of protection analyses are studies of riverbed and catchment capacity, which were conducted by Walczak et al (2018) and Laks et al Hämmerling, M., Walczak, N., Walczak, Z., Zawadzki, P. (2019). Assessment of technical conditions of bank protection of watercourses and reservoirs in the city of Poznań.…”
Section: Discussionmentioning
confidence: 99%
“…Vegetation can reduce the active width of a watercourse and alter the velocity of water flow on hydrometric verticals within the floodplain and main channel. It is important to note that this effect is not always negative and can have both positive and negative impacts on the ecosystem (Walczak et al, 2018). The flood regime, in turn, affects the structure of the floodplain vegetation (Wu et al, 2022).…”
Section: Introductionmentioning
confidence: 99%
“…The occurrence of plant communities, such as shrubs of purple willow (Salix purpurea L.) or rushes of common reed (Phragmites australis), influences the flow conditions in the riverbed, and affects, in particular, the spatial distribution of flow velocity and stream turbulence [1][2][3][4]. Such plant hydraulic interaction is not easy to determine as it depends on many variable factors, e.g., plant species and mechanical characteristics [5][6][7] and their stage of development including the density of the plant zone [3,4,7,8]. This interaction also depends on the spatial configuration of the vegetation zone (quasi-regular vegetation development, e.g., in the form of a triangle, circle, rectangle, etc., or the opposite, very irregular) and on the location of the plant community (at riverside (Figure 1), or directly in the river current (Figure 2)).…”
Section: Introductionmentioning
confidence: 99%