The classification gravel-bed sediment of the Svatava river

Kód výsledku v IS VaVaI

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Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

The classification gravel-bed sediment of the Svatava river

Popis výsledku v původním jazyce

The aim of this study was based on simple granulometric characteristics determine gravel-bed streams Svatava stream because the literature stated appointed only source sand. Furthermore, to demonstrate the influence of bridge construction on the size distribution of the sediment. On the stream Svatava were selected two sites located near the bridge construction there is in fact a greater extent alluvial sediment settles. One at the confluence Svatava and Ohře and the second in the middle of the flow. The sediment was removed before the objects in a flow path stream with bridge construction and for the last bridge on the level of Q1 unaffected deposits. In the laboratory on the basis of particle size analysis was drawn grading curve representing the ratio distribution across the various factions (Cb - rock, G - gravel, S - sand, C - clay). The uniformity coefficien (Cu) and the curvature coefficien (Cc) helped classify sediment. The aim was to determine the most represented a fraction o

Název v anglickém jazyce

The classification gravel-bed sediment of the Svatava river

Popis výsledku anglicky

The aim of this study was based on simple granulometric characteristics determine gravel-bed streams Svatava stream because the literature stated appointed only source sand. Furthermore, to demonstrate the influence of bridge construction on the size distribution of the sediment. On the stream Svatava were selected two sites located near the bridge construction there is in fact a greater extent alluvial sediment settles. One at the confluence Svatava and Ohře and the second in the middle of the flow. The sediment was removed before the objects in a flow path stream with bridge construction and for the last bridge on the level of Q1 unaffected deposits. In the laboratory on the basis of particle size analysis was drawn grading curve representing the ratio distribution across the various factions (Cb - rock, G - gravel, S - sand, C - clay). The uniformity coefficien (Cu) and the curvature coefficien (Cc) helped classify sediment. The aim was to determine the most represented a fraction o

Druh

D - Stať ve sborníku

CEP obor

DA - Hydrologie a limnologie

OECD FORD obor

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Projekt

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Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2015

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název statě ve sborníku

Colloquium on Landscape Management 2015

ISBN

978-80-7509-378-3

ISSN

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e-ISSN

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Počet stran výsledku

6

Strana od-do

71-76

Název nakladatele

Mendelova univerzita v Brně

Místo vydání

Brno

Místo konání akce

Brno

Datum konání akce

15. 12. 2015

Typ akce podle státní příslušnosti

EUR - Evropská akce

Kód UT WoS článku

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