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hyperpycnal inflow
释义
hyperpycnal inflow
hyperpycnal inflow
[
¦hī·pər¦pik·nəl ′in‚flō
]
(hydrology)
A denser inflow that occurs when a sediment-laden fluid flows down the side of a basin and along the bottom as a turbidity current.
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更新时间:2025/6/2 12:54:44