Titlebook: Deep-Sea Sediments; Physical and Mechani Anton L. Inderbitzen Book 1974 Springer Science+Business Media New York 1974 Atlantic Ocean.Indian

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In Situ Measurement of Sediment Acoustic Properties During Coringwhich has been developed for attachment to sediment corers in order to obtain an in situ sound-speed profile during a coring operation. The system uses two electroacoustic transducers mounted in the cutting head of the corer and associated electronic circuitry to measure the travel time of an acoust

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Sea-Floor Soil Mechanics and Trafficability Measurements with the Tracked Vehicle “RUM”he use of RUM in a soil mechanics and trafficability study program is also described. Highlights of over 400 operating hours on the sea floor at depths ranging from 40 to 1880 meters illustrates the problems encountered and the experience that has been obtained in this program. A limited amount of d

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Erodibility of Fine Abyssal Sedimentles exposed to bottom currents. Important controls on these forces involve the dynamics of turbulent boundary-layer flow, the physical and chemical nature of the sediment particles, and the past history of the sediment, including effects of flocculation and the activity of benthic organisms. Time sc

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The Effects of the Benthic Fauna on the Physical Properties of Deep-Sea Sedimentshe results are a variety of identifiable structures which are abundant both at the sediment-water interface and preserved in deeper layers. These “Lebensspuren” are always common in sediments, except where sedimentation rates or other physical processes have obscured them..In the deep sea, invertebr

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https://doi.org/10.1057/9780230117655ht, water content, void ratio, and shear strength. At best, most of the correlations provide only an approximation and are restricted to the sediment type or local area from which the basis for the correlation was developed.

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Developmental Biology Protocols sediments is that under equal loads the carbonate sediments do not consolidate to as low a final void ratio as noncarbonates..The permeability of the sediments undergoing consolidation testing were determined by the use of the time-compression curves. The relationship between void ratio and coeffic