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  • Liquid limit and specific surface of clay particles
    Dolinar, Bojana, 1956- ; Trauner, Ludvik
    In this paper a new method for determining the liquid limit of nonexpanding soils is presented. The liquid limit value primarily depends on the type and quantity of clay minerals in soils. This ... relationship, however, has never beenpresented in general analytical form that would enable a consistent determination of the influence of mineralogical properties of different soils on the liquid limit. The findings described in the article define those mineralogical properties of soils, which determine the quantity of water at the liquid limit. It was found that the water content at the liquid limit depends on the size and the quantity of clay grains in soils that contain onlynonexpanding minerals. In case of expanding minerals in soils, the size and the quantity of clays determine only the quantity of intergrain water, while the total water content depends on the quantity of interlayer water also.
    Vir: Geotechnical testing journal. - ISSN 0149-6115 (Vol. 27, no. 6, Nov. 2004, str. 580-584)
    Vrsta gradiva - članek, sestavni del
    Leto - 2004
    Jezik - angleški
    COBISS.SI-ID - 9130006

vir: Geotechnical testing journal. - ISSN 0149-6115 (Vol. 27, no. 6, Nov. 2004, str. 580-584)

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