Submerged hydraulic jump: a computational analysis in different scales
ABSTRACT Advancements in computational capabilities have enabled engineers and scientists to numerically model complex turbulent phenomena such as hydraulic jumps. This research assesses the capability of numerically simulating a hydraulic jump that occurs in the UHE Porto Colômbia's stilling b...
Ausführliche Beschreibung
Autor*in: |
João Pedro Paludo Bocchi [verfasserIn] Daniela Guzzon Sanagiotto [verfasserIn] Eder Daniel Teixeira [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch ; Portugiesisch |
Erschienen: |
2024 |
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Schlagwörter: |
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Übergeordnetes Werk: |
In: Revista Brasileira de Recursos Hídricos - Associação Brasileira de Recursos Hídricos, 2016, 29(2024) |
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Übergeordnetes Werk: |
volume:29 ; year:2024 |
Links: |
Link aufrufen |
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DOI / URN: |
10.1590/2318-0331.292420230089 |
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Katalog-ID: |
DOAJ09282806X |
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10.1590/2318-0331.292420230089 doi (DE-627)DOAJ09282806X (DE-599)DOAJba4eb4da2cc74f71af0cc90d41a077d1 DE-627 ger DE-627 rakwb eng por TC1-978 TC401-506 GE1-350 João Pedro Paludo Bocchi verfasserin aut Submerged hydraulic jump: a computational analysis in different scales 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier ABSTRACT Advancements in computational capabilities have enabled engineers and scientists to numerically model complex turbulent phenomena such as hydraulic jumps. This research assesses the capability of numerically simulating a hydraulic jump that occurs in the UHE Porto Colômbia's stilling basin at a flow rate of 4,000 m3/s. To achieve this, simulation results were compared with data from three hydraulic physical models (scales 1:32, 1:50, and 1:100) and full-scale measurements. The simulations employed the Ansys CFX solver, utilizing a Reynolds-Averaged Navier-Stokes (RANS) approach, the RNG κ-ε turbulence model, and the Volume of Fluid (VOF) method for air-water interactions. Various variables were analyzed, with satisfactory results for mean pressures, conjugated depths, roller length, water profile in less aerated areas, and mean velocity at the submerged hydraulic jump upstream section, with errors below 10%. However, the submerged hydraulic jump's start position and the representation of the water surface profile in the region near the jump toe yielded more disparate results. In conclusion, the methods and conditions applied in the simulations are apt for representing variables less impacted by aeration phenomena, establishing CFD simulations as a valuable tool for hydraulic jump analysis. Hydraulic jump Submerged hydraulic jump CFD RANS Technology T Hydraulic engineering River, lake, and water-supply engineering (General) Geography. Anthropology. Recreation G Environmental sciences Daniela Guzzon Sanagiotto verfasserin aut Eder Daniel Teixeira verfasserin aut In Revista Brasileira de Recursos Hídricos Associação Brasileira de Recursos Hídricos, 2016 29(2024) (DE-627)893151513 (DE-600)2899348-2 23180331 nnns volume:29 year:2024 https://doi.org/10.1590/2318-0331.292420230089 kostenfrei https://doaj.org/article/ba4eb4da2cc74f71af0cc90d41a077d1 kostenfrei http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2318-03312024000100201&lng=en&tlng=en kostenfrei http://www.scielo.br/pdf/rbrh/v29/2318-0331-rbrh-29-e2.pdf kostenfrei https://doaj.org/toc/2318-0331 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 29 2024 |
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10.1590/2318-0331.292420230089 doi (DE-627)DOAJ09282806X (DE-599)DOAJba4eb4da2cc74f71af0cc90d41a077d1 DE-627 ger DE-627 rakwb eng por TC1-978 TC401-506 GE1-350 João Pedro Paludo Bocchi verfasserin aut Submerged hydraulic jump: a computational analysis in different scales 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier ABSTRACT Advancements in computational capabilities have enabled engineers and scientists to numerically model complex turbulent phenomena such as hydraulic jumps. This research assesses the capability of numerically simulating a hydraulic jump that occurs in the UHE Porto Colômbia's stilling basin at a flow rate of 4,000 m3/s. To achieve this, simulation results were compared with data from three hydraulic physical models (scales 1:32, 1:50, and 1:100) and full-scale measurements. The simulations employed the Ansys CFX solver, utilizing a Reynolds-Averaged Navier-Stokes (RANS) approach, the RNG κ-ε turbulence model, and the Volume of Fluid (VOF) method for air-water interactions. Various variables were analyzed, with satisfactory results for mean pressures, conjugated depths, roller length, water profile in less aerated areas, and mean velocity at the submerged hydraulic jump upstream section, with errors below 10%. However, the submerged hydraulic jump's start position and the representation of the water surface profile in the region near the jump toe yielded more disparate results. In conclusion, the methods and conditions applied in the simulations are apt for representing variables less impacted by aeration phenomena, establishing CFD simulations as a valuable tool for hydraulic jump analysis. Hydraulic jump Submerged hydraulic jump CFD RANS Technology T Hydraulic engineering River, lake, and water-supply engineering (General) Geography. Anthropology. Recreation G Environmental sciences Daniela Guzzon Sanagiotto verfasserin aut Eder Daniel Teixeira verfasserin aut In Revista Brasileira de Recursos Hídricos Associação Brasileira de Recursos Hídricos, 2016 29(2024) (DE-627)893151513 (DE-600)2899348-2 23180331 nnns volume:29 year:2024 https://doi.org/10.1590/2318-0331.292420230089 kostenfrei https://doaj.org/article/ba4eb4da2cc74f71af0cc90d41a077d1 kostenfrei http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2318-03312024000100201&lng=en&tlng=en kostenfrei http://www.scielo.br/pdf/rbrh/v29/2318-0331-rbrh-29-e2.pdf kostenfrei https://doaj.org/toc/2318-0331 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 29 2024 |
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10.1590/2318-0331.292420230089 doi (DE-627)DOAJ09282806X (DE-599)DOAJba4eb4da2cc74f71af0cc90d41a077d1 DE-627 ger DE-627 rakwb eng por TC1-978 TC401-506 GE1-350 João Pedro Paludo Bocchi verfasserin aut Submerged hydraulic jump: a computational analysis in different scales 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier ABSTRACT Advancements in computational capabilities have enabled engineers and scientists to numerically model complex turbulent phenomena such as hydraulic jumps. This research assesses the capability of numerically simulating a hydraulic jump that occurs in the UHE Porto Colômbia's stilling basin at a flow rate of 4,000 m3/s. To achieve this, simulation results were compared with data from three hydraulic physical models (scales 1:32, 1:50, and 1:100) and full-scale measurements. The simulations employed the Ansys CFX solver, utilizing a Reynolds-Averaged Navier-Stokes (RANS) approach, the RNG κ-ε turbulence model, and the Volume of Fluid (VOF) method for air-water interactions. Various variables were analyzed, with satisfactory results for mean pressures, conjugated depths, roller length, water profile in less aerated areas, and mean velocity at the submerged hydraulic jump upstream section, with errors below 10%. However, the submerged hydraulic jump's start position and the representation of the water surface profile in the region near the jump toe yielded more disparate results. In conclusion, the methods and conditions applied in the simulations are apt for representing variables less impacted by aeration phenomena, establishing CFD simulations as a valuable tool for hydraulic jump analysis. Hydraulic jump Submerged hydraulic jump CFD RANS Technology T Hydraulic engineering River, lake, and water-supply engineering (General) Geography. Anthropology. Recreation G Environmental sciences Daniela Guzzon Sanagiotto verfasserin aut Eder Daniel Teixeira verfasserin aut In Revista Brasileira de Recursos Hídricos Associação Brasileira de Recursos Hídricos, 2016 29(2024) (DE-627)893151513 (DE-600)2899348-2 23180331 nnns volume:29 year:2024 https://doi.org/10.1590/2318-0331.292420230089 kostenfrei https://doaj.org/article/ba4eb4da2cc74f71af0cc90d41a077d1 kostenfrei http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2318-03312024000100201&lng=en&tlng=en kostenfrei http://www.scielo.br/pdf/rbrh/v29/2318-0331-rbrh-29-e2.pdf kostenfrei https://doaj.org/toc/2318-0331 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 29 2024 |
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ABSTRACT Advancements in computational capabilities have enabled engineers and scientists to numerically model complex turbulent phenomena such as hydraulic jumps. This research assesses the capability of numerically simulating a hydraulic jump that occurs in the UHE Porto Colômbia's stilling basin at a flow rate of 4,000 m3/s. To achieve this, simulation results were compared with data from three hydraulic physical models (scales 1:32, 1:50, and 1:100) and full-scale measurements. The simulations employed the Ansys CFX solver, utilizing a Reynolds-Averaged Navier-Stokes (RANS) approach, the RNG κ-ε turbulence model, and the Volume of Fluid (VOF) method for air-water interactions. Various variables were analyzed, with satisfactory results for mean pressures, conjugated depths, roller length, water profile in less aerated areas, and mean velocity at the submerged hydraulic jump upstream section, with errors below 10%. However, the submerged hydraulic jump's start position and the representation of the water surface profile in the region near the jump toe yielded more disparate results. In conclusion, the methods and conditions applied in the simulations are apt for representing variables less impacted by aeration phenomena, establishing CFD simulations as a valuable tool for hydraulic jump analysis. |
abstractGer |
ABSTRACT Advancements in computational capabilities have enabled engineers and scientists to numerically model complex turbulent phenomena such as hydraulic jumps. This research assesses the capability of numerically simulating a hydraulic jump that occurs in the UHE Porto Colômbia's stilling basin at a flow rate of 4,000 m3/s. To achieve this, simulation results were compared with data from three hydraulic physical models (scales 1:32, 1:50, and 1:100) and full-scale measurements. The simulations employed the Ansys CFX solver, utilizing a Reynolds-Averaged Navier-Stokes (RANS) approach, the RNG κ-ε turbulence model, and the Volume of Fluid (VOF) method for air-water interactions. Various variables were analyzed, with satisfactory results for mean pressures, conjugated depths, roller length, water profile in less aerated areas, and mean velocity at the submerged hydraulic jump upstream section, with errors below 10%. However, the submerged hydraulic jump's start position and the representation of the water surface profile in the region near the jump toe yielded more disparate results. In conclusion, the methods and conditions applied in the simulations are apt for representing variables less impacted by aeration phenomena, establishing CFD simulations as a valuable tool for hydraulic jump analysis. |
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ABSTRACT Advancements in computational capabilities have enabled engineers and scientists to numerically model complex turbulent phenomena such as hydraulic jumps. This research assesses the capability of numerically simulating a hydraulic jump that occurs in the UHE Porto Colômbia's stilling basin at a flow rate of 4,000 m3/s. To achieve this, simulation results were compared with data from three hydraulic physical models (scales 1:32, 1:50, and 1:100) and full-scale measurements. The simulations employed the Ansys CFX solver, utilizing a Reynolds-Averaged Navier-Stokes (RANS) approach, the RNG κ-ε turbulence model, and the Volume of Fluid (VOF) method for air-water interactions. Various variables were analyzed, with satisfactory results for mean pressures, conjugated depths, roller length, water profile in less aerated areas, and mean velocity at the submerged hydraulic jump upstream section, with errors below 10%. However, the submerged hydraulic jump's start position and the representation of the water surface profile in the region near the jump toe yielded more disparate results. In conclusion, the methods and conditions applied in the simulations are apt for representing variables less impacted by aeration phenomena, establishing CFD simulations as a valuable tool for hydraulic jump analysis. |
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