Kinematic parameters of flow constrained by combined dams with through part of tetrahedra in compression region

Every major river in the world consists of mountainous, foothills, and flat areas characterized by different flow regimes. The foothill areas differ in slopes i = 0.001 ÷ 0.004, flow kinetics Fr > 0.15, and the size of sediments. The riverbed is unstable, and the banks are prone to erosion. The...

Full description

Bibliographic Details
Main Authors: Bakiev Masharif, Khalimbetov Azat, Yakubov Kuvonchbek, Sagin Jay, Asamatdinov Ilyas
Format: Article
Language:English
Published: EDP Sciences 2023-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2023/38/e3sconf_conmechydro23_04046.pdf
_version_ 1797775888862937088
author Bakiev Masharif
Khalimbetov Azat
Yakubov Kuvonchbek
Sagin Jay
Asamatdinov Ilyas
author_facet Bakiev Masharif
Khalimbetov Azat
Yakubov Kuvonchbek
Sagin Jay
Asamatdinov Ilyas
author_sort Bakiev Masharif
collection DOAJ
description Every major river in the world consists of mountainous, foothills, and flat areas characterized by different flow regimes. The foothill areas differ in slopes i = 0.001 ÷ 0.004, flow kinetics Fr > 0.15, and the size of sediments. The riverbed is unstable, and the banks are prone to erosion. The construction of coastal protection structures requires solving complex issues related to their design. The analysis showed that most of the studies, including ours, were carried out for the conditions of lowland rivers. This work aims to establish the flow features of the foothill sections of a combined dam with a through part of tetrahedra when the ratio of the through part ℓs to the total length of the dam ℓd is greater than or equal to 0.5, i.e., ℓs/ℓd. ≥ 0.5 The presence of a satellite flow behind the through part, a weakly perturbed core, and the presence of two zones of intense turbulent mixing was experimentally established, and the universality of the velocity distribution, which obeys the theoretical dependence of Schlichting-Abramovich, was confirmed. It is once again confirmed that the dependence is on the slope of the bottom, the Froude number, the degree of constraint, and the formation of "calm" and "critical" flow modes. The nature of the level changes along the length of the compression region in the core, and the satellite flow differ from each other, and the alignments occur in the vertical compression alignment. The problem is implemented for the "calm" mode using an integral relation characterizing the law of conservation of momentum in the flow, the equation of conservation of flow, and the differential equation of uneven motion recorded for the satellite flow behind the through part of the combined dam. The presence of a satellite flow, two zones of intense turbulent mixing, and the different nature of the leveled regime of the main and satellite flows are taken into account. A comparison of theoretical solutions with experimental ones shows their similarity.
first_indexed 2024-03-12T22:42:05Z
format Article
id doaj.art-38b432a1427e47f08cd6c4e25e0121d0
institution Directory Open Access Journal
issn 2267-1242
language English
last_indexed 2024-03-12T22:42:05Z
publishDate 2023-01-01
publisher EDP Sciences
record_format Article
series E3S Web of Conferences
spelling doaj.art-38b432a1427e47f08cd6c4e25e0121d02023-07-21T09:34:23ZengEDP SciencesE3S Web of Conferences2267-12422023-01-014010404610.1051/e3sconf/202340104046e3sconf_conmechydro23_04046Kinematic parameters of flow constrained by combined dams with through part of tetrahedra in compression regionBakiev Masharif0Khalimbetov Azat1Yakubov Kuvonchbek2Sagin Jay3Asamatdinov Ilyas4"Tashkent Institute of Irrigation and Agricultural Mechanization Engineers" National Research University"Tashkent Institute of Irrigation and Agricultural Mechanization Engineers" National Research University"Tashkent Institute of Irrigation and Agricultural Mechanization Engineers" National Research UniversityWestern Michigan University“Gosvodkhoznadzor” in the Republic of KarakalpakstanEvery major river in the world consists of mountainous, foothills, and flat areas characterized by different flow regimes. The foothill areas differ in slopes i = 0.001 ÷ 0.004, flow kinetics Fr > 0.15, and the size of sediments. The riverbed is unstable, and the banks are prone to erosion. The construction of coastal protection structures requires solving complex issues related to their design. The analysis showed that most of the studies, including ours, were carried out for the conditions of lowland rivers. This work aims to establish the flow features of the foothill sections of a combined dam with a through part of tetrahedra when the ratio of the through part ℓs to the total length of the dam ℓd is greater than or equal to 0.5, i.e., ℓs/ℓd. ≥ 0.5 The presence of a satellite flow behind the through part, a weakly perturbed core, and the presence of two zones of intense turbulent mixing was experimentally established, and the universality of the velocity distribution, which obeys the theoretical dependence of Schlichting-Abramovich, was confirmed. It is once again confirmed that the dependence is on the slope of the bottom, the Froude number, the degree of constraint, and the formation of "calm" and "critical" flow modes. The nature of the level changes along the length of the compression region in the core, and the satellite flow differ from each other, and the alignments occur in the vertical compression alignment. The problem is implemented for the "calm" mode using an integral relation characterizing the law of conservation of momentum in the flow, the equation of conservation of flow, and the differential equation of uneven motion recorded for the satellite flow behind the through part of the combined dam. The presence of a satellite flow, two zones of intense turbulent mixing, and the different nature of the leveled regime of the main and satellite flows are taken into account. A comparison of theoretical solutions with experimental ones shows their similarity.https://www.e3s-conferences.org/articles/e3sconf/pdf/2023/38/e3sconf_conmechydro23_04046.pdf
spellingShingle Bakiev Masharif
Khalimbetov Azat
Yakubov Kuvonchbek
Sagin Jay
Asamatdinov Ilyas
Kinematic parameters of flow constrained by combined dams with through part of tetrahedra in compression region
E3S Web of Conferences
title Kinematic parameters of flow constrained by combined dams with through part of tetrahedra in compression region
title_full Kinematic parameters of flow constrained by combined dams with through part of tetrahedra in compression region
title_fullStr Kinematic parameters of flow constrained by combined dams with through part of tetrahedra in compression region
title_full_unstemmed Kinematic parameters of flow constrained by combined dams with through part of tetrahedra in compression region
title_short Kinematic parameters of flow constrained by combined dams with through part of tetrahedra in compression region
title_sort kinematic parameters of flow constrained by combined dams with through part of tetrahedra in compression region
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2023/38/e3sconf_conmechydro23_04046.pdf
work_keys_str_mv AT bakievmasharif kinematicparametersofflowconstrainedbycombineddamswiththroughpartoftetrahedraincompressionregion
AT khalimbetovazat kinematicparametersofflowconstrainedbycombineddamswiththroughpartoftetrahedraincompressionregion
AT yakubovkuvonchbek kinematicparametersofflowconstrainedbycombineddamswiththroughpartoftetrahedraincompressionregion
AT saginjay kinematicparametersofflowconstrainedbycombineddamswiththroughpartoftetrahedraincompressionregion
AT asamatdinovilyas kinematicparametersofflowconstrainedbycombineddamswiththroughpartoftetrahedraincompressionregion