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Salt Intrusion, Tides and Mixing in Multi-Channel Estuaries - PhD: UNESCO-IHE Institute, Delft (Hardcover): Anh Duc Nguyen Salt Intrusion, Tides and Mixing in Multi-Channel Estuaries - PhD: UNESCO-IHE Institute, Delft (Hardcover)
Anh Duc Nguyen
R5,822 Discovery Miles 58 220 Ships in 12 - 19 working days

Multi-channel estuaries, such as the Mekong Delta in Vietnam and the Scheldt in the Netherlands, have characteristics of both the river and the sea, forming a unique environment influenced by tidal movements of the sea and freshwater flow of the river. This study addresses a number of knowledge gaps in multi-channel estuaries by developing a predictive analytical approach for salinity intrusion and discharge estimate in multi-channel estuaries. The new approach agrees well with 1-D hydrodynamic models and observations, indicating its applicability in practice. Most importantly, the study has successfully developed a new theory and a new equation to quantify tidal pumping due to ebb-flood channel residual circulation and the related salt dispersion.

Salt Intrusion, Tides and Mixing in Multi-Channel Estuaries - PhD: UNESCO-IHE Institute, Delft (Paperback): Anh Duc Nguyen Salt Intrusion, Tides and Mixing in Multi-Channel Estuaries - PhD: UNESCO-IHE Institute, Delft (Paperback)
Anh Duc Nguyen
R2,818 Discovery Miles 28 180 Ships in 12 - 19 working days

Multi-channel estuaries, such as the Mekong Delta in Vietnam and the Scheldt in the Netherlands, have characteristics of both the river and the sea, forming a unique environment influenced by tidal movements of the sea and freshwater flow of the river. This study addresses a number of knowledge gaps in multi-channel estuaries by developing a predictive analytical approach for salinity intrusion and discharge estimate in multi-channel estuaries. The new approach agrees well with 1-D hydrodynamic models and observations, indicating its applicability in practice. Most importantly, the study has successfully developed a new theory and a new equation to quantify tidal pumping due to ebb-flood channel residual circulation and the related salt dispersion.

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