TECHNICAL NOTES
Apr 1, 1984
Phase Relations in Marine Soils
Publication: Journal of Geotechnical Engineering
Volume 110, Issue 4
Abstract
Pore water in marine sediments contains dissolved salts. For marine clays and biogenous oozes which have high void ratios, the dissolved salts should be taken into account in determining soil void ratio, water content, dry density, specific gravity, porosity and degree of saturation. This paper presents phase relations for marine sediments and provides correct equations for various index properties. It also provides equations for different relations taking into account the necessary corrections for dissolved salts in marine soils.
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References
1.
Holtz, R. D., and Kovacs, W. D., “An Introduction to Geotechnical Engineering,” Prentice‐Hall, Inc., Englewood Cliffs, N.J., 1981, chapter 2.
2.
Lambe, T. W., and Whitman, R. V., “Soil Mechanics,” John Wiley and Sons, Inc., New York, N.Y., 1969, chapter 3.
3.
V. W. R. Scientific Catalog, Van Water and Rogers Co., 3745 Bayshore Blvd., Brisbane, Calif., 94005, 1982–83, p. 1115.
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Copyright © 1984 ASCE.
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Published online: Apr 1, 1984
Published in print: Apr 1984
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Iraj Noorany, M. ASCE
Prof. of Civ. Engrg., San Diego State Univ. San Diego, Calif. 92182
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Terms of Use: ASCE Library Cards are for individual, personal use only. Reselling, republishing, or forwarding the materials to libraries or reading rooms is prohibited.
Terms of Use: ASCE Library Cards are for individual, personal use only. Reselling, republishing, or forwarding the materials to libraries or reading rooms is prohibited.