Index Properties of Organic and Slightly Organic Soils

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Abstract:

Conflicting results in the effect of OC on Atterberg limits need to a clarification with more studies. The observation that why PL increases in the higher rate than LL would be interesting issue to more investigation. Thus, this paper is focused on the index properties of OS (Site A) and SOS (Site B). It was found that removing OC in Site A affect particle size distribution by a dispersion phenomena while no effect was observed in Site B. Presence of average 13.6 % OC in site A leaded to increase in liquid and plastic limits for 6.1% and 26.9 %, respectively.

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Advanced Materials Research (Volumes 291-294)

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3454-3458

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July 2011

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© 2011 Trans Tech Publications Ltd. All Rights Reserved

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[1] British Standards Institution, Methods of Testing for Soils for Civil Engineering Purposes, 1990, BS 1377.

Google Scholar

[2] Buckman, H. O., Bradly, N. C. (1999). The nature and properties of soils, 12th edition. New Delhi: Prentice Hall.

Google Scholar

[3] Day. Robert W, Soil Testing Manual: Procedures, Classification Data, and Sampling Practices, Mc Graw-Hill Professional Publishing, California, (2000).

Google Scholar

[4] Department of Irrigation and Drainage, Sarawak, 2004, pp.3-4. See www. did. sarawak. gov/my/peat/peat_main. html.

Google Scholar

[5] Huat, B. B. K. (2006). Deformation and Shear Strength Characteristics of Some Tropical Peat and Organic Soil. Pertanika J. Sci & Technol. 14(1&2): 61-74.

Google Scholar

[6] Huat, B. B. K., Maail S., Mohamed T. A (2005). Effect of Chemical Admixtures on the Engineering Properties of Tropical Peat Soils. American J. of Engineering and Applied Sciences, 2 (7): 1113-1120.

DOI: 10.3844/ajassp.2005.1113.1120

Google Scholar

[7] Malkawi. A.I. Husein, Alawneh. A. S, Abu-Safaqah. O.T. (1999). Effect of organic matter on the physical and physicochemical properties of an illitic soil. Applied Clay Science 14 259-278.

DOI: 10.1016/s0169-1317(99)00003-4

Google Scholar

[8] Odell, R.T., Thornburn, T.H., Mckenzie, L.J. (1960). Relationship of Atterberg limits to some other properties of Illinois soils. Proceedings of the Soil Science Society of America 24 _4., 297–300.

DOI: 10.2136/sssaj1960.03615995002400040025x

Google Scholar

[9] PAUL, M. A., BARRAS, B. F. (1999). Role of organic material in the plasticity of Bothkennar clay. Geotechnique 49, , 529-535.

DOI: 10.1680/geot.1999.49.4.529

Google Scholar

[10] Rahman, R. A., Mannan, M. A. (1995). Effect of Organic Load on Basic Geotechnical Properties of Compacted Sand-kaolinite Mixture. PertaikaJ. Sci & Technol, 3(1), 87-98.

Google Scholar

[11] Schumacher, B. A. (2002).

Google Scholar

[12] Zentar, R., Abriak, N. E., Dubois, V. (2009). Effects of salts and organic matter on Atterberg limits of dredged marine sediments. Applied Clay Science, 42, 391-397.

DOI: 10.1016/j.clay.2008.04.003

Google Scholar