By Edwin L. Hamilton (auth.), Anton L. Inderbitzen (eds.)
As a part of its carrying on with software to stimulate enhanced uncomplicated examine within the marine atmosphere, the workplace of Naval examine, Ocean technology and expertise department, backed a sequence of closed seminar-workshops in 1972-1973. each one seminar concentrated upon one re seek sector of marine geology that's fairly new and short of a serious assessment and speeded up aid. the themes components selected for the seminars have been: 1. traditional gases in marine sediments and their mode of distribution, 2. nephelometry and the optical homes of ocean waters, three. actual and engineering homes of deep-sea sediments, and four. physics of sound in marine sediments. The pursuits of every seminar-workshop have been to convey into sharper concentration the state-of-the-science inside every one topic quarter, to impression a point of coordination one of the investigators operating inside of each one of those parts and to supply the sea technological know-how and know-how department assistance for nationwide application help. This volume.contains lots of the papers offered on the semi nar at the actual and engineering homes of deep-sea sediments. The seminar used to be held at Airlie apartment, Airlie, Virginia on April 24- 27, 1973 and used to be prepared and chaired via A. Inderbitzen. The at tendees have been invited from one of the prime investigators during this box from either the engineering and medical disciplines. each one attendee used to be asked to arrange a paper inside his region of spe ciality.
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Additional resources for Deep-Sea Sediments: Physical and Mechanical Properties
Soc. , ~, 1-15, 1956. Hamilton, E. , H. P. Bucker, D. L. Keir, and J. A. Whitney, Velocities of compressional and shear waves in marine sediments determined in situ from a research submersible, J. Geophys. , 11, 4039-4049, 1970. Hamilton, E. , D. P. H. Sherrer, Bengal, Bering Geophys. , G. Moore, E. C. Buffington, J. R. Curray, and Sediment velocities from sonobuoys: Bay of Sea, Japan Sea, and Northeast Pacific, J. in press. Hastrup, O. , Digital analysis of acoustic reflectivity in the Tyrrhenian Abyssal Plain, J.
Yield Theories The Hvorslev (1960) failure criterion is basically an extension of the Hohr-Coulomb theory. which incorporates a factor to take into account the void ratio at failure. fO' v, and B are parameters for the particular soil and ef is the void ratio on the failure plane. critica1state method. is advanced to predict stress-strain behavior of clays. The critical state methods are fully discussed and developed in a textbook by Schofield and Wroth (1968). ctive stress state and void ratio.
K = bulk modulus, dynes/cm 2 x 1010. ~ = rigidity (shear) modulus, dynes/cm 2 x 10 10 . a = Poisson's Ratio. Vs velocity of shear wave, m/sec. SE = Standard error of the mean. Vs No. Avg. SE Samples 37 62 27 47 27 2 15 5 13 13 9 412 17 324 12 263 12 18 50 19 250 417 472 447 363 270 PREDICTION OF DEEP-SEA SEDIMENT PROPERTIES 33 clays. These cases were not included in the averages shown in Tables 5 and 6. For this reason, and because of rounding off to a lower number of decimal places, the average values in the tables usually cannot be exactly interrelated with the elastic equations.