Subaqueous sediment gravity flows undergoing progressive solidification
Subaqueous sediment gravity flows undergoing progressive solidification
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发表时间：
2006
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通讯作者：
Amiruddin;H. Sekiguchi;S. Sassa
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作者：
Amiruddin;H. Sekiguchi;S. Sassa
高度集中的泥沙流可能发生在水下或滨水地区松散压实的颗粒状斜坡破裂后。这种泥沙流动对海岸填充物、水下管道和其他此类海洋设施的完整性有相当大的影响。然而，高浓度沉积物-水混合物的物理本质上是复杂的，需要通过基本方法进行更多的发展(Shanmugam，1996；Ilstad等人)。2004年)。
Highly concentrated sediment flows may occur following failures of loosely compacted, granular slopes underwater or in waterfront areas. The mobility of such sediment flows is of considerable interest to the integrity of coastal fills, underwater pipelines and other such marine facilities. However, the physics of highly concentrated sediment-water mixtures is complex in nature and calls for more development through fundamental approaches (Shanmugam 1996; Ilstad et al. 2004).