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Rheological Properties of Allophane Colloid

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Rheology
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Abstract

There are many volcanic soils containing allophane in the countries of volcanic soil like Italy, Newzealand, and Japan. The most particular rheological property of allophane is thixotropic, and it happens often in earth work that remolding of soil by machine makes difficult conditions to continue work. The shearing strength of allophane soil goes down to a half or more and soil erosion increases when it gets wet or dry excessively. These mechanical properties result from the surface forces between soil particles.

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References

  1. Y. Kitagawa, “Unit particles of allophane”, Amer. Mineral., 52, 690–708 (1967).

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  2. K. Wada, “Structural schem of soil allophane”, Amer. Mineral., 52, May-June (1967).

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  3. L. Barclay, A. Harrington and R. H. Ottewill, “The measurement of forces between particles in disperse systems”, Kolloid-Z. u. Z. Polymere, 250, 655–666 (1972).

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  4. R. Yasutomi and S. Sudo, “A method of measuring some physical properties of soil with a forced oscillation viscometer”, Soil Sci., 105, 336–341 (1967).

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© 1980 Springer Science+Business Media New York

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Yasutomi, R., Senō, M. (1980). Rheological Properties of Allophane Colloid. In: Astarita, G., Marrucci, G., Nicolais, L. (eds) Rheology. Springer, Boston, MA. https://doi.org/10.1007/978-1-4684-3743-0_116

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  • DOI: https://doi.org/10.1007/978-1-4684-3743-0_116

  • Publisher Name: Springer, Boston, MA

  • Print ISBN: 978-1-4684-3745-4

  • Online ISBN: 978-1-4684-3743-0

  • eBook Packages: Springer Book Archive

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