Numerical Investigation of Dissolved Oxygen Transportation through a Coupled SWE and Streeter–Phelps Model

Dissolved oxygen (DO) reflects the self-purification ability of a water body and is also an important indicator for quantifying the water quality. The morphological changes in the cross sections of river channels will affect the hydraulic conditions, and the distribution of pollutants and DO may als...

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Main Authors: Jiaxin Wu, Xiaoxiang Yu
Format: Article
Language:English
Published: Hindawi Limited 2021-01-01
Series:Mathematical Problems in Engineering
Online Access:http://dx.doi.org/10.1155/2021/6663696
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spelling doaj-7b104f1471424751967ed9686fd63c4a2021-02-22T00:00:06ZengHindawi LimitedMathematical Problems in Engineering1563-51472021-01-01202110.1155/2021/6663696Numerical Investigation of Dissolved Oxygen Transportation through a Coupled SWE and Streeter–Phelps ModelJiaxin Wu0Xiaoxiang Yu1State Key Laboratory of Hydraulics and Mountain River EngineeringBoyada Reconnaissance Layout Design Co., LtdDissolved oxygen (DO) reflects the self-purification ability of a water body and is also an important indicator for quantifying the water quality. The morphological changes in the cross sections of river channels will affect the hydraulic conditions, and the distribution of pollutants and DO may also be affected, possibly resulting in local oxygen deficits and pollution. To effectively predict the water quality, a coupled model is introduced in this study. The shallow water equation (SWE) is adopted to calculate the hydrodynamic processes, and the modified Streeter–Phelps model is further coupled with the SWE model to evaluate the reaeration. By applying this model, mass transportation and reaeration in rivers are analyzed. The influences of the sudden cross-sectional changes in the river channel on the DO distribution and the reaeration ability are identified. The results reveal that a certain degree of expansion in the river is conducive to reaeration and can also accelerate the consumption of pollutants through the water body’s self-purification. DO transport in two real terrains, including a mountain basin and plain river, is extensively investigated, and the results indicate that the morphological characteristics in the mountain basin will cause the concentration distribution to form inside dead zones, while in the plain, the distribution will form a fan-shaped downstream zone.http://dx.doi.org/10.1155/2021/6663696
collection DOAJ
language English
format Article
sources DOAJ
author Jiaxin Wu
Xiaoxiang Yu
spellingShingle Jiaxin Wu
Xiaoxiang Yu
Numerical Investigation of Dissolved Oxygen Transportation through a Coupled SWE and Streeter–Phelps Model
Mathematical Problems in Engineering
author_facet Jiaxin Wu
Xiaoxiang Yu
author_sort Jiaxin Wu
title Numerical Investigation of Dissolved Oxygen Transportation through a Coupled SWE and Streeter–Phelps Model
title_short Numerical Investigation of Dissolved Oxygen Transportation through a Coupled SWE and Streeter–Phelps Model
title_full Numerical Investigation of Dissolved Oxygen Transportation through a Coupled SWE and Streeter–Phelps Model
title_fullStr Numerical Investigation of Dissolved Oxygen Transportation through a Coupled SWE and Streeter–Phelps Model
title_full_unstemmed Numerical Investigation of Dissolved Oxygen Transportation through a Coupled SWE and Streeter–Phelps Model
title_sort numerical investigation of dissolved oxygen transportation through a coupled swe and streeter–phelps model
publisher Hindawi Limited
series Mathematical Problems in Engineering
issn 1563-5147
publishDate 2021-01-01
description Dissolved oxygen (DO) reflects the self-purification ability of a water body and is also an important indicator for quantifying the water quality. The morphological changes in the cross sections of river channels will affect the hydraulic conditions, and the distribution of pollutants and DO may also be affected, possibly resulting in local oxygen deficits and pollution. To effectively predict the water quality, a coupled model is introduced in this study. The shallow water equation (SWE) is adopted to calculate the hydrodynamic processes, and the modified Streeter–Phelps model is further coupled with the SWE model to evaluate the reaeration. By applying this model, mass transportation and reaeration in rivers are analyzed. The influences of the sudden cross-sectional changes in the river channel on the DO distribution and the reaeration ability are identified. The results reveal that a certain degree of expansion in the river is conducive to reaeration and can also accelerate the consumption of pollutants through the water body’s self-purification. DO transport in two real terrains, including a mountain basin and plain river, is extensively investigated, and the results indicate that the morphological characteristics in the mountain basin will cause the concentration distribution to form inside dead zones, while in the plain, the distribution will form a fan-shaped downstream zone.
url http://dx.doi.org/10.1155/2021/6663696
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