| 河口浑浊带成因综述 |
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| 引用本文： | 时伟荣,沈焕庭.河口浑浊带成因综述[J].地球科学进展,1993,8(1):8-13. |
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| 作者姓名： | 时伟荣 沈焕庭 |
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| 作者单位： | 华东师范大学河口海岸研究所，华东师范大学河口海岸研究所，华东师范大学河口海岸研究所 上海 200062，上海 200062，上海 200062 |
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| 基金项目： | 国家自然科学幕金资助项目。 |
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| 摘 要： | 综述了国内外对河口浑浊带成因机制的研究，归纳成六条。并简要介绍了对成因机制的综合性研究。
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| 关 键 词： | 河口浑浊带 成因机制 |
| 收稿时间： | 1992-02-23 |
REVIEW ON THE FORMATION OF ESTUARINE TURBIDITY MAXIMUM |
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| Shi Weirong,Shen Huanting and Li Jiufa.REVIEW ON THE FORMATION OF ESTUARINE TURBIDITY MAXIMUM[J].Advance in Earth Sciences,1993,8(1):8-13. |
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| Authors: | Shi Weirong Shen Huanting and Li Jiufa |
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| Institution: | Institute of Estuarine and Coastal Research; East China Normal University 200062 |
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| Abstract: | The present paper reviews the researches in the formation mechanisms of the estuarine turbidity maximum.The turbidity maximum play a very important role in mud transport in estuarines. It is typically present in partially to well-mixed estuarines. Though its formation had been contributed mainly (even solely) to the trapping mechanism caused by the vertical gravitational circulation in estuarines, a turbidity maximum may be generated by following proceses: the settling and scouring lag effect, the flocculation,the estuarine circulation, the stockes drift, the tidal current and the resuspension of bottom sediments. Either of the six generating proceses may be predominant in estuarines of different hydrodynamic regimes. Their predominance is controlled by the equilibrium between the tidal and riverine dynamics. Thus the estuarine comparison and the mechanism study are the important toics in the estuarine mud transport research. |
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| Keywords: | Estuarine turbidity maximum Formation mechanism |
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