Journal of Geotechnical and Geoenvironmental Engineering · 2015 · 111 citations · 68 references
AgricultureEarth SciencesSoil SciencesGeotechnical EngineeringSoil ClassificationSoil ScienceElectrical Conductivity Of SoilsParticle-size ClassesSoil Electrical Conductivity SensingSoil PermeabilitySoil PorositySoil TextureFines ContentGeotechnical CharacterizationLiquid LimitPore Water Electrical ConductivitySensitivitySoil Electrical Conductivity TestingSoil Texture Characterization
The 75-μm particle size is used to discriminate between fine and coarse grains. Further analysis of fine grains is typically based on the plasticity chart. Whereas pore-fluid-chemistry-dependent soil response is a salient and distinguishing characteristic of fine grains, pore-fluid chemistry is not addressed in current classification systems. Liquid limits obtained with electrically contrasting pore fluids (deionized water, 2-M NaCl brine, and kerosene) are combined to define the soil “electrical sensitivity.” Liquid limit and electrical sensitivity can be effectively used to classify fine grains according to their fluid-soil response into no-, low-, intermediate-, or high-plasticity fine grains of low, intermediate, or high electrical sensitivity. The proposed methodology benefits from the accumulated experience with liquid limit in the field and addresses the needs of a broader range of geotechnical engineering problems.
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J. M. Bradford · Soil Science Society of America Journal · 1976 · 2.1K citations
An Introduction to Clay Colloid Chemistry
H. van Olphen, Pa Ho Hsu · Soil Science · 1978 · 980 citations
The drained residual strength of cohesive soils
J. F. Lupini, A. E. Skinner, P. R. Vaughan · Géotechnique · 1981 · 681 citations