Prediction of salinity intrusion in mixed estuaries
The longitudinal, tidal averaged salinity distribution in a mixed estuary is represented by the one-dimensional convective diffusion (or dispersion) equation, which forms the starting point for salinity intrusion prediction. Normally, in the prediction of salinity intrusion in an estuary, solution o...
محفوظ في:
| المؤلف الرئيسي: | |
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| مؤلفون آخرون: | |
| التنسيق: | Theses and Dissertations |
| اللغة: | English |
| منشور في: |
2009
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| الموضوعات: | |
| الوصول للمادة أونلاين: | http://hdl.handle.net/10356/19413 |
| الوسوم: |
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| المؤسسة: | Nanyang Technological University |
| اللغة: | English |
| الملخص: | The longitudinal, tidal averaged salinity distribution in a mixed estuary is represented by the one-dimensional convective diffusion (or dispersion) equation, which forms the starting point for salinity intrusion prediction. Normally, in the prediction of salinity intrusion in an estuary, solution of the dispersion equation often ends up having complicated models. The major disadvantage of these models is that they need a large amount of data on estuary geometry and tidal information before calibration can be carried out. |
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