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- W2800688052 abstract "Marine sediments at different locations and depths are not necessarily similar. Distinctions are (1) sandy/silty sediments, when most particles have settled and almost every particle touches other particles, and (2) mud sediments, where the majority in a layer are suspended so that they do not touch other particles. Most theoretical and analytical modeling over the years has largely been confined to sandy/silty sediments, and some successful models, although arguably heuristic and with adjustable parameters, have emerged. There is also some speculation that such models might apply equally well for mud sediments. The present authors in recent years have concentrated on the development of a fundamentals-based model for mud sediments, although there is as yet insufficient data to adequately test its validity. The present paper speculates on what this model may have in common with models for sandy/silty sediments. There are expectations that the Mallock-Wood model may approximately apply for sound speed predictions at very low frequencies. Arguments are presented to the effect that the physics is sufficiently different for the two sediments types that a substantially different model is needed for mud sediments. One chief distinction is that the solid portion of mud sediments has a portion that is clay particles, and these have substantially different electrolytic and cohesive properties than those of quartz particles." @default.
- W2800688052 created "2018-05-17" @default.
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- W2800688052 date "2018-03-01" @default.
- W2800688052 modified "2023-09-26" @default.
- W2800688052 title "Distinctions among physical types of marine sediments, especially mud, and their possible fundamentals-based and heuristic models" @default.
- W2800688052 doi "https://doi.org/10.1121/1.5035798" @default.
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