COMPARISION BETWEEN TWO NUMERICAL MODELS FOR PREDICATION OF HYDRAULICS AND MORPHOLOGICAL CHANGES IN THE RIVER NILE (FROM KM 633 TO KM 645 UPSTREAM El-RODA GAUGE STATION)

The numerical models have effective and necessary tools for rivers hydrological and morphological studies. Numerical models are useful when results are required on scales applicable for hydrological and morphological changes, where velocity and water depth distributions are significant especially in...

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Main Authors: Radwa Salama, Heba elsersawy
Format: Article
Language:Arabic
Published: Assiut University, Faculty of Engineering 2020-09-01
Series:JES: Journal of Engineering Sciences
Subjects:
Online Access:https://jesaun.journals.ekb.eg/article_109760_feb6c48ee41c4d00b0d2693634491ac9.pdf
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author Radwa Salama
Heba elsersawy
author_facet Radwa Salama
Heba elsersawy
author_sort Radwa Salama
collection DOAJ
description The numerical models have effective and necessary tools for rivers hydrological and morphological studies. Numerical models are useful when results are required on scales applicable for hydrological and morphological changes, where velocity and water depth distributions are significant especially in river reaches. In the present study , two well known hydraulic models are used to simulate the River Nile hydraulics and morphological changes. A sensitivity analysis is carried out for the two models to investigate the features and disadvantages of each model and give recommendations for their further applications. The performance analysis depends on field survey data and simulations. The two models are the SMS modules (FESWMS) model and the (Delft3D) model. The field data were collected for a study reach of 12 km which is located between km 633 to km 645, measured from El-Roda gauge station. The data included geometric and hydraulic data, that were gathered for calibration and validation of the models. The results indicated that both the SMS module and (Delft3D) model predicted the water surface elevations quite well. The sensitivity analysis showed that (Delft3D) model was more logical to mesh resolution than the SMS module and SMS model presented a better fit for the hydraulic variables. However, Delft3D presented a better fit for velocity and morphological changes.
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spelling doaj.art-f6cc235edb0c498586b76372f10efea92023-01-04T14:21:07ZaraAssiut University, Faculty of EngineeringJES: Journal of Engineering Sciences1687-05302356-85502020-09-0148No 574976410.21608/jesaun.2020.39116.1002109760COMPARISION BETWEEN TWO NUMERICAL MODELS FOR PREDICATION OF HYDRAULICS AND MORPHOLOGICAL CHANGES IN THE RIVER NILE (FROM KM 633 TO KM 645 UPSTREAM El-RODA GAUGE STATION)Radwa Salama0Heba elsersawy1Nile Research Institute ,El Kanater Elkhairria,Cairo.Nile Research Institute ,El Kanater ,Elkhairria Cairo.The numerical models have effective and necessary tools for rivers hydrological and morphological studies. Numerical models are useful when results are required on scales applicable for hydrological and morphological changes, where velocity and water depth distributions are significant especially in river reaches. In the present study , two well known hydraulic models are used to simulate the River Nile hydraulics and morphological changes. A sensitivity analysis is carried out for the two models to investigate the features and disadvantages of each model and give recommendations for their further applications. The performance analysis depends on field survey data and simulations. The two models are the SMS modules (FESWMS) model and the (Delft3D) model. The field data were collected for a study reach of 12 km which is located between km 633 to km 645, measured from El-Roda gauge station. The data included geometric and hydraulic data, that were gathered for calibration and validation of the models. The results indicated that both the SMS module and (Delft3D) model predicted the water surface elevations quite well. The sensitivity analysis showed that (Delft3D) model was more logical to mesh resolution than the SMS module and SMS model presented a better fit for the hydraulic variables. However, Delft3D presented a better fit for velocity and morphological changes.https://jesaun.journals.ekb.eg/article_109760_feb6c48ee41c4d00b0d2693634491ac9.pdfmorphological changeshydraulicssmsdelft3d and river nile
spellingShingle Radwa Salama
Heba elsersawy
COMPARISION BETWEEN TWO NUMERICAL MODELS FOR PREDICATION OF HYDRAULICS AND MORPHOLOGICAL CHANGES IN THE RIVER NILE (FROM KM 633 TO KM 645 UPSTREAM El-RODA GAUGE STATION)
JES: Journal of Engineering Sciences
morphological changes
hydraulics
sms
delft3d and river nile
title COMPARISION BETWEEN TWO NUMERICAL MODELS FOR PREDICATION OF HYDRAULICS AND MORPHOLOGICAL CHANGES IN THE RIVER NILE (FROM KM 633 TO KM 645 UPSTREAM El-RODA GAUGE STATION)
title_full COMPARISION BETWEEN TWO NUMERICAL MODELS FOR PREDICATION OF HYDRAULICS AND MORPHOLOGICAL CHANGES IN THE RIVER NILE (FROM KM 633 TO KM 645 UPSTREAM El-RODA GAUGE STATION)
title_fullStr COMPARISION BETWEEN TWO NUMERICAL MODELS FOR PREDICATION OF HYDRAULICS AND MORPHOLOGICAL CHANGES IN THE RIVER NILE (FROM KM 633 TO KM 645 UPSTREAM El-RODA GAUGE STATION)
title_full_unstemmed COMPARISION BETWEEN TWO NUMERICAL MODELS FOR PREDICATION OF HYDRAULICS AND MORPHOLOGICAL CHANGES IN THE RIVER NILE (FROM KM 633 TO KM 645 UPSTREAM El-RODA GAUGE STATION)
title_short COMPARISION BETWEEN TWO NUMERICAL MODELS FOR PREDICATION OF HYDRAULICS AND MORPHOLOGICAL CHANGES IN THE RIVER NILE (FROM KM 633 TO KM 645 UPSTREAM El-RODA GAUGE STATION)
title_sort comparision between two numerical models for predication of hydraulics and morphological changes in the river nile from km 633 to km 645 upstream el roda gauge station
topic morphological changes
hydraulics
sms
delft3d and river nile
url https://jesaun.journals.ekb.eg/article_109760_feb6c48ee41c4d00b0d2693634491ac9.pdf
work_keys_str_mv AT radwasalama comparisionbetweentwonumericalmodelsforpredicationofhydraulicsandmorphologicalchangesintherivernilefromkm633tokm645upstreamelrodagaugestation
AT hebaelsersawy comparisionbetweentwonumericalmodelsforpredicationofhydraulicsandmorphologicalchangesintherivernilefromkm633tokm645upstreamelrodagaugestation