. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography 78 KELLER 450r 400 O 350 300 fr? 250 *â z LU >â z 200 o V OL LU ISO tâ < £ 100 50 â GRAIN. 140 1 50 160 170 180 190 2 00 2 10 WET UNIT WEIGHT (g/cm3) Figure 1. Fixed relationship of wet unit weight to water content for two grain specific gravities This field of study, recently referred to as Marine Geotech- nique, has advanced rapidly during these past fifteen years. It has advanced not only in regard to gaining a better u
. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography 78 KELLER 450r 400 O 350 300 fr? 250 *â z LU >â z 200 o V OL LU ISO tâ < £ 100 50 â GRAIN. 140 1 50 160 170 180 190 2 00 2 10 WET UNIT WEIGHT (g/cm3) Figure 1. Fixed relationship of wet unit weight to water content for two grain specific gravities This field of study, recently referred to as Marine Geotech- nique, has advanced rapidly during these past fifteen years. It has advanced not only in regard to gaining a better understanding of deep-sea sediments, but by sizably increasing the number of re- searchers working in the field. Although there is as yet relative- ly little known about the mass physical properties of deep-sea sedi- ments, a number of interrelationships (Hamilton, 1956; Moore and Shumway, 1959; Richards, 1961, 1962) and regional generalizations made on the distribution of these properties over the North Atlan- tic and North Pacific basins (Keller and Bennett, 1968) and the Mediterranean (Keller and Lambert, 1971) have been defined. With the advent of the M0H0LE Project and later the J0IDES Deep-Sea Drilling Project, a limited amount of mass property data have be- come available from depths as great as 1015 m below the sea floor (Hamilton, 1964; Moore, 1964; Creager et al., 1973). Most of the basic relationships between the index properties of terrestrial deposits were established long ago by those working in soil mechanics. More recent studies of deep-sea sediments have 965. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Atlantic Oceanographic and Meteorological Laboratories; Pacific Oceanographic Laboratories; United States. Environmental Science Services Administration. Research Laboratories; Enviro
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