2023
DOI: 10.1016/j.heliyon.2023.e17367
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Suspended sediment transport generated by non-hydrostatic hydrodynamics in Northern Waters of Aceh, Indonesia

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Cited by 3 publications
(1 citation statement)
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“…In order to be in accordance with its functions, a complete port must have a pier, breakwater, port pool, shipping lanes, passenger and goods terminals, fish landing terminals, processing , and waste disposal facilities (reception facilities/garbage and sewage treatment and disposal facilities), emergency response systems, as well as port operation supporting facilities such as warehouses, container processing facilities, stacking yards, fish auction places, cold storage for fishery products, road networks, electricity networks, telecommunications networks, clean water networks, drainage networks, various loading and unloading equipment, workshops and different hydro-acoustic surveys [1][2][3] Suspended sediment mainly consists of sediment types, namely fine sand, silt, and clay (with an average size of 63 m), carried to rivers and streams from the highlands and transported downstream [4][5][6] . Over time, under certain conditions, such as reduced flow velocity and momentum, sediment can, therefore, temporarily accumulate in channels or riverbeds, and under most common hydraulic systems, entrained and remobilized sediments return to the outflow [7][8].…”
Section: Introductionmentioning
confidence: 99%
“…In order to be in accordance with its functions, a complete port must have a pier, breakwater, port pool, shipping lanes, passenger and goods terminals, fish landing terminals, processing , and waste disposal facilities (reception facilities/garbage and sewage treatment and disposal facilities), emergency response systems, as well as port operation supporting facilities such as warehouses, container processing facilities, stacking yards, fish auction places, cold storage for fishery products, road networks, electricity networks, telecommunications networks, clean water networks, drainage networks, various loading and unloading equipment, workshops and different hydro-acoustic surveys [1][2][3] Suspended sediment mainly consists of sediment types, namely fine sand, silt, and clay (with an average size of 63 m), carried to rivers and streams from the highlands and transported downstream [4][5][6] . Over time, under certain conditions, such as reduced flow velocity and momentum, sediment can, therefore, temporarily accumulate in channels or riverbeds, and under most common hydraulic systems, entrained and remobilized sediments return to the outflow [7][8].…”
Section: Introductionmentioning
confidence: 99%