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Flume experiment on flow division ratio of bifurcated Jiaomen outlet in the Zhujiang River
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Peng Yao1, 2, Zhibin Yu2, Min Su2, 3, *, Xinxi An2, Zeng Zhou1, 2
Haiyang Xuebao | 2022, 44(6) : 106 - 115
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Haiyang Xuebao | 2022, 44(6): 106-115
Article
Flume experiment on flow division ratio of bifurcated Jiaomen outlet in the Zhujiang River
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Peng Yao1, 2, Zhibin Yu2, Min Su2, 3, *, Xinxi An2, Zeng Zhou1, 2
Affiliations
  • 1. State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China
  • 2. Jiangsu Key Laboratory of Coast Ocean Resources Development and Environment Security, Nanjing 210098, China
  • 3. State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200241, China
Published: 2022-05-25 doi: 10.12284/hyxb2022055
Outline
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The Jiaomen outlet is the main flood and sediment discharge of the Zhujiang River. It is connected with Humen outlet through a lateral branch, namely the Fuzhou Channel. The flow and sediment division ratio of the bifurcated Jiaomen outlet are important for flood control and navigation safety of the Guangdong-Hong Kong-Macao Greater Bay Area. Focusing on the flow division ratio of the Fuzhou Channel, this study designed a series of scaled physical experiments to explore the relationship between flow division ratio of the Fuzhou Channel and the flow of Jiaomen outlet and adjacent Humen outlet. The dimension of the physical model is based on morphological characteristics in the vicinity of the Jiaomen outlet nowadays. Results of the experiment are in good agreement with the filed measurements under two different flow conditions, demonstrating a reliable model performance. Subsequently, series of experiments have been carried out by varying upstream discharges of Humen and Jiaomen. Experimental results indicate that the division ratio of the Fuzhou Channel depicts a positive relationship with the flow velocity ratio between Humen and Jiaomen. Thus, the flow division ratio of the Fuzhou Channel depends on both Humen and Jiaomen. The experimental results further suggest that, under present geomorphic situation, if the upstream velocity ratio between Humen and Jiaomen decreases to 0.35, the Fuzhou Channel would shift from the main branch to secondary. The research results can provide a reference for the artificial regulation of Jiaomen outlet and its flood and navigation safety.

Jiaomen outlet  /  Fuzhou Channel  /  bifurcated estuary  /  flow division ratio  /  flume experiment
Peng Yao, Zhibin Yu, Min Su, Xinxi An, Zeng Zhou. Flume experiment on flow division ratio of bifurcated Jiaomen outlet in the Zhujiang River[J]. Haiyang Xuebao, 2022 , 44 (6) : 106 -115 . DOI: 10.12284/hyxb2022055
Year 2022 volume 44 Issue 6
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Article Info
doi: 10.12284/hyxb2022055
  • Receive Date:2021-06-16
  • Online Date:2026-02-01
  • Published:2022-05-25
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History
  • Received:2021-06-16
  • Revised:2021-10-11
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Affiliations
    1. State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China
    2. Jiangsu Key Laboratory of Coast Ocean Resources Development and Environment Security, Nanjing 210098, China
    3. State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200241, China
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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