Study on the influence of infiltration on flood propagation with different peak shape coefficients and duration
Traditional flood simulations fail to properly consider the impact of soil infiltration in floodplain areas with high soil infiltration rates. Notably, ignoring soil infiltration will lead to considerable uncertainty in flood simulations. In this paper, a fully hydrodynamic model coupled with the Gr...
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2021
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oai:doaj.org-article:c6c66bcf1bf14387ab8c0b91da7500082021-11-05T20:18:27ZStudy on the influence of infiltration on flood propagation with different peak shape coefficients and duration1366-70171996-975910.2166/wp.2021.193https://doaj.org/article/c6c66bcf1bf14387ab8c0b91da7500082021-08-01T00:00:00Zhttp://wp.iwaponline.com/content/23/4/1059https://doaj.org/toc/1366-7017https://doaj.org/toc/1996-9759Traditional flood simulations fail to properly consider the impact of soil infiltration in floodplain areas with high soil infiltration rates. Notably, ignoring soil infiltration will lead to considerable uncertainty in flood simulations. In this paper, a fully hydrodynamic model coupled with the Green–Ampt infiltration model was used. Taking a natural reach in northern China (HTH in this paper) as a case study, observed flood discharge data were used to analyze the influence of soil infiltration on flood propagation based on the flood propagation simulation results for various inflow conditions. The maximum difference of inundation area is about 25%. The results show that soil infiltration has little effect on the inundation area during the rising stage of a flood. In the late period of a flood, the inundation area considering the effect of infiltration is smaller than that without infiltration, and the smaller the peak coefficient is, the longer the flood duration is, the larger the impact of infiltration on the inundation area. When the peak shape coefficient is 0.42 and the flood duration is 44.4 h, the maximum difference of the inundation area is about 28%. The research results provide a reference for flood management and post-disaster rescue efforts. HIGHLIGHTS Using a fully hydrodynamic model coupled with the Green–Ampt model to simulate the flood propagation.; The model uses graphic processing unit acceleration technology.; Analyzing the influence of soil infiltration on flood based on the flood propagation simulation results.; It is considered that the flood peak shape coefficient has influence on infiltration.; The results provide a reference for flood management and post-disaster rescue efforts.;Jingming HouZhaoan ZhangDawei ZhangBaoshan ShiGuangzhao ChenHongbin ZhangIWA Publishingarticleflood propagationgreen–ampt modelhydrodynamic modelinfiltrationinundation areapeak shape coefficientRiver, lake, and water-supply engineering (General)TC401-506ENWater Policy, Vol 23, Iss 4, Pp 1059-1074 (2021) |
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EN |
topic |
flood propagation green–ampt model hydrodynamic model infiltration inundation area peak shape coefficient River, lake, and water-supply engineering (General) TC401-506 |
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flood propagation green–ampt model hydrodynamic model infiltration inundation area peak shape coefficient River, lake, and water-supply engineering (General) TC401-506 Jingming Hou Zhaoan Zhang Dawei Zhang Baoshan Shi Guangzhao Chen Hongbin Zhang Study on the influence of infiltration on flood propagation with different peak shape coefficients and duration |
description |
Traditional flood simulations fail to properly consider the impact of soil infiltration in floodplain areas with high soil infiltration rates. Notably, ignoring soil infiltration will lead to considerable uncertainty in flood simulations. In this paper, a fully hydrodynamic model coupled with the Green–Ampt infiltration model was used. Taking a natural reach in northern China (HTH in this paper) as a case study, observed flood discharge data were used to analyze the influence of soil infiltration on flood propagation based on the flood propagation simulation results for various inflow conditions. The maximum difference of inundation area is about 25%. The results show that soil infiltration has little effect on the inundation area during the rising stage of a flood. In the late period of a flood, the inundation area considering the effect of infiltration is smaller than that without infiltration, and the smaller the peak coefficient is, the longer the flood duration is, the larger the impact of infiltration on the inundation area. When the peak shape coefficient is 0.42 and the flood duration is 44.4 h, the maximum difference of the inundation area is about 28%. The research results provide a reference for flood management and post-disaster rescue efforts. HIGHLIGHTS
Using a fully hydrodynamic model coupled with the Green–Ampt model to simulate the flood propagation.;
The model uses graphic processing unit acceleration technology.;
Analyzing the influence of soil infiltration on flood based on the flood propagation simulation results.;
It is considered that the flood peak shape coefficient has influence on infiltration.;
The results provide a reference for flood management and post-disaster rescue efforts.; |
format |
article |
author |
Jingming Hou Zhaoan Zhang Dawei Zhang Baoshan Shi Guangzhao Chen Hongbin Zhang |
author_facet |
Jingming Hou Zhaoan Zhang Dawei Zhang Baoshan Shi Guangzhao Chen Hongbin Zhang |
author_sort |
Jingming Hou |
title |
Study on the influence of infiltration on flood propagation with different peak shape coefficients and duration |
title_short |
Study on the influence of infiltration on flood propagation with different peak shape coefficients and duration |
title_full |
Study on the influence of infiltration on flood propagation with different peak shape coefficients and duration |
title_fullStr |
Study on the influence of infiltration on flood propagation with different peak shape coefficients and duration |
title_full_unstemmed |
Study on the influence of infiltration on flood propagation with different peak shape coefficients and duration |
title_sort |
study on the influence of infiltration on flood propagation with different peak shape coefficients and duration |
publisher |
IWA Publishing |
publishDate |
2021 |
url |
https://doaj.org/article/c6c66bcf1bf14387ab8c0b91da750008 |
work_keys_str_mv |
AT jingminghou studyontheinfluenceofinfiltrationonfloodpropagationwithdifferentpeakshapecoefficientsandduration AT zhaoanzhang studyontheinfluenceofinfiltrationonfloodpropagationwithdifferentpeakshapecoefficientsandduration AT daweizhang studyontheinfluenceofinfiltrationonfloodpropagationwithdifferentpeakshapecoefficientsandduration AT baoshanshi studyontheinfluenceofinfiltrationonfloodpropagationwithdifferentpeakshapecoefficientsandduration AT guangzhaochen studyontheinfluenceofinfiltrationonfloodpropagationwithdifferentpeakshapecoefficientsandduration AT hongbinzhang studyontheinfluenceofinfiltrationonfloodpropagationwithdifferentpeakshapecoefficientsandduration |
_version_ |
1718444064529973248 |