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- W2044717078 abstract "Abstract Permeability characteristics of deep‐sea sediments from the East Bermuda Rise and Blake Bahama Outer Ridge areas of the northwestern Atlantic were investigated. The samples were predominantly clay sized, although there were significant percentages of coarser‐grained material. The coefficients of permeability were directly measured by imposing a hydraulic head across the sample and were calculated according to the theory of one‐dimensional consolidation. Darcy's measured coefficients of permeability ranged from 7.93 ts 10‐7 cm/sec at a void ratio of 3.66 to 1.10 ts 10‐8 cm/sec at a void ratio of 1.10. Of the two methods (log of time and square root of time) the square root of time method agreed more with the measured permeability values. This is related to the square root of time's reliance on the earlier stages of consolidation, when the excess pore pressures across the sample are greater and secondary effects are reduced. Existing theory based on the physiochemical nature of the clays was inadeq..." @default.
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- W2044717078 date "1982-01-01" @default.
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- W2044717078 title "Permeability of deep‐sea clays: Northwestern Atlantic" @default.
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- W2044717078 doi "https://doi.org/10.1080/10641198209379834" @default.
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