Morphological analysis and evaluation of Givi-chay River conduit form (northwest of Iran)

In this study, the factors affecting the formation of channel patterns and dynamics in the Givi-chay River during the period 2019–2000 were analysed. To evaluate the river strength, flaw stress and its effects on channel morphology, Landsat 7 and 8 images, topographic maps, geology, and hydrological...

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Main Authors: Elnaz Piroozi, Aghil Madadi, Sayyad Asghari Saraskanrood, Parveen Sihag
Format: Article
Language:English
Published: IWA Publishing 2022-10-01
Series:Water Supply
Subjects:
Online Access:http://ws.iwaponline.com/content/22/10/7851
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author Elnaz Piroozi
Aghil Madadi
Sayyad Asghari Saraskanrood
Parveen Sihag
author_facet Elnaz Piroozi
Aghil Madadi
Sayyad Asghari Saraskanrood
Parveen Sihag
author_sort Elnaz Piroozi
collection DOAJ
description In this study, the factors affecting the formation of channel patterns and dynamics in the Givi-chay River during the period 2019–2000 were analysed. To evaluate the river strength, flaw stress and its effects on channel morphology, Landsat 7 and 8 images, topographic maps, geology, and hydrological and field data were used. According to the results of the calculation of hydrological indicators, in terms of 15, the index, a significant difference is seen among upstream and downstream stations. Therefore, it can be found that the presence of the Givi Dam has created a good platform for intensifying the hydrological and morphological changes of the river plan. The particular strength of the river in all parts of the fourth interval and the ninth, 12th, eighth (second interval) levels causes the erosion threshold to soar. The highest amount of shear stress was observed in the second interval at 12, 13, and 9, respectively. Generally, the changes of the Givi River Plan include expansion of existing meanders, displacement of paths, increase of curvature and formation of small meanders and formation of channel pattern and dynamics, affected by discharge provision, sediment discharge due to dam construction, lithological resistance of the riverbed and human interference. HIGHLIGHTS Factors affecting the formation of channel patterns were analysed.; Givi Dam has created a good platform for intensifying hydrological changes.; Highest amount of shear stress was observed in the second interval at 12, 13, and 9, respectively.; Givi-chay River Plan includes expansion of existing meanders.; Formation of channel pattern and dynamics, affected by discharge provision, sediment discharge due to dam construction.;
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spelling doaj.art-8838b02f23e1415992ee02db56bccb812022-12-22T03:56:18ZengIWA PublishingWater Supply1606-97491607-07982022-10-0122107851787210.2166/ws.2022.279279Morphological analysis and evaluation of Givi-chay River conduit form (northwest of Iran)Elnaz Piroozi0Aghil Madadi1Sayyad Asghari Saraskanrood2Parveen Sihag3 Faculty of Social Sciences, University of Mohaghegh Ardabili, Ardabil, Iran Faculty of Social Sciences, University of Mohaghegh Ardabili, Ardabil, Iran Faculty of Social Sciences, University of Mohaghegh Ardabili, Ardabil, Iran Civil Engineering Department, Chandigarh University, Mohali, India In this study, the factors affecting the formation of channel patterns and dynamics in the Givi-chay River during the period 2019–2000 were analysed. To evaluate the river strength, flaw stress and its effects on channel morphology, Landsat 7 and 8 images, topographic maps, geology, and hydrological and field data were used. According to the results of the calculation of hydrological indicators, in terms of 15, the index, a significant difference is seen among upstream and downstream stations. Therefore, it can be found that the presence of the Givi Dam has created a good platform for intensifying the hydrological and morphological changes of the river plan. The particular strength of the river in all parts of the fourth interval and the ninth, 12th, eighth (second interval) levels causes the erosion threshold to soar. The highest amount of shear stress was observed in the second interval at 12, 13, and 9, respectively. Generally, the changes of the Givi River Plan include expansion of existing meanders, displacement of paths, increase of curvature and formation of small meanders and formation of channel pattern and dynamics, affected by discharge provision, sediment discharge due to dam construction, lithological resistance of the riverbed and human interference. HIGHLIGHTS Factors affecting the formation of channel patterns were analysed.; Givi Dam has created a good platform for intensifying hydrological changes.; Highest amount of shear stress was observed in the second interval at 12, 13, and 9, respectively.; Givi-chay River Plan includes expansion of existing meanders.; Formation of channel pattern and dynamics, affected by discharge provision, sediment discharge due to dam construction.;http://ws.iwaponline.com/content/22/10/7851damgivi-chaymorphological and hydrological indicesriver powershear stress
spellingShingle Elnaz Piroozi
Aghil Madadi
Sayyad Asghari Saraskanrood
Parveen Sihag
Morphological analysis and evaluation of Givi-chay River conduit form (northwest of Iran)
Water Supply
dam
givi-chay
morphological and hydrological indices
river power
shear stress
title Morphological analysis and evaluation of Givi-chay River conduit form (northwest of Iran)
title_full Morphological analysis and evaluation of Givi-chay River conduit form (northwest of Iran)
title_fullStr Morphological analysis and evaluation of Givi-chay River conduit form (northwest of Iran)
title_full_unstemmed Morphological analysis and evaluation of Givi-chay River conduit form (northwest of Iran)
title_short Morphological analysis and evaluation of Givi-chay River conduit form (northwest of Iran)
title_sort morphological analysis and evaluation of givi chay river conduit form northwest of iran
topic dam
givi-chay
morphological and hydrological indices
river power
shear stress
url http://ws.iwaponline.com/content/22/10/7851
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AT aghilmadadi morphologicalanalysisandevaluationofgivichayriverconduitformnorthwestofiran
AT sayyadasgharisaraskanrood morphologicalanalysisandevaluationofgivichayriverconduitformnorthwestofiran
AT parveensihag morphologicalanalysisandevaluationofgivichayriverconduitformnorthwestofiran