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The effects of spring-neap tide on sediment bedding on tidal flats: A numerical study
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Mengpiao Xu1, 2, Peihua Dong2, Jun Ma3, Feng Luo1, Changkuan Zhang1, Daidu Fan4, Zeng Zhou1, 4, 5, *
Haiyang Xuebao | 2021, 43(10) : 70 - 80
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Haiyang Xuebao | 2021, 43(10): 70-80
Article
The effects of spring-neap tide on sediment bedding on tidal flats: A numerical study
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Mengpiao Xu1, 2, Peihua Dong2, Jun Ma3, Feng Luo1, Changkuan Zhang1, Daidu Fan4, Zeng Zhou1, 4, 5, *
Affiliations
  • 1State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China
  • 2China Design Group, Nanjing 210014, China
  • 3Channel Management Office of Hangzhou Port and Waterway Administration, Hangzhou 310016, China
  • 4School of Ocean and Earth Sciences, Tongji University, Shanghai 200092, China
  • 5Jiangsu Key Laboratory of Coast Ocean Resources Development and Environment Security, Hohai University, Nanjing 210098, China
Published: 2021-10-25 doi: 10.12284/hyxb2021125
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The formation of vertical sedimentary rhythmic layers of tidal flat mainly depends on periodic tidal conditions, including flood and ebb tide, spring and neap tide, seasonal and longer term scale tidal characteristics. In order to investigate the distribution and mechanism of sediment bedding on tidal flats, a one-dimensional numerical model was used to simulate the rhythmic layers of long-term tidal flat bedding layers under spring and neap tidal cycles. Results indicate that the periodicity of spring-neap tide is the main reason for the rhythmicity of sedimentary bedding. One couplet in the rhythm layer corresponds to the spring-neap tidal period, which is formed by the mud-dominated layer during the neap tide and the sand-dominated layer during the spring tide. The thicknesses of layers also show a cyclical change: bedding layers are thicker during the spring tide and thinner during the neap tide. The boundary sediment concentration is also an important factor affecting the structure of tidal couplets. An increasing boundary concentration of silt makes the tidal rhythm layer coarser and increases the overall thickness of the sand-dominated layer. When the boundary sediment concentration significantly increases, the vertical tidal rhythm layers on the tidal flat are more intact with an evident increase in layer thickness. The formation and characteristics of tidal bedding layers are the result of the joint action of many factors (e.g., waves, storms, biological factors and etc.), which await further research effort in the future.

tidal flat  /  sediment sorting  /  tidal rhythm layers  /  numerical simulation
Mengpiao Xu, Peihua Dong, Jun Ma, Feng Luo, Changkuan Zhang, Daidu Fan, Zeng Zhou. The effects of spring-neap tide on sediment bedding on tidal flats: A numerical study[J]. Haiyang Xuebao, 2021 , 43 (10) : 70 -80 . DOI: 10.12284/hyxb2021125
Year 2021 volume 43 Issue 10
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doi: 10.12284/hyxb2021125
  • Receive Date:2020-04-08
  • Online Date:2026-02-26
  • Published:2021-10-25
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History
  • Received:2020-04-08
  • Revised:2020-06-30
Affiliations
    1State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China
    2China Design Group, Nanjing 210014, China
    3Channel Management Office of Hangzhou Port and Waterway Administration, Hangzhou 310016, China
    4School of Ocean and Earth Sciences, Tongji University, Shanghai 200092, China
    5Jiangsu Key Laboratory of Coast Ocean Resources Development and Environment Security, Hohai University, Nanjing 210098, 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
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种数
Number of
species
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Percentage of total
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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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