Foundation Engineering Handbook 1991
DOI: 10.1007/978-1-4615-3928-5_3
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Soil Technology and Engineering Properties of Soils

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Cited by 21 publications
(9 citation statements)
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“…Similarly, from , we obtain the estimate K ≈ 4.07 × 10 −15 m 2 . The estimates for permeability of sandstone available in the literature vary a great deal and range from 1.0 × 10 −15 to 1.5 × 10 −10 m 2 (e.g., Farmer 1968; Serafim 1968; Winterkorn and Fang 1975; Jaeger and Cook 1976; Lama and Vutukuri 1978; Costa and Baker 1981). Recently, Lock et al (2003) investigated the use of the image analysis of the pore structure for the estimation of the permeability of sandstone.…”
Section: Computational Modelingmentioning
confidence: 99%
“…Similarly, from , we obtain the estimate K ≈ 4.07 × 10 −15 m 2 . The estimates for permeability of sandstone available in the literature vary a great deal and range from 1.0 × 10 −15 to 1.5 × 10 −10 m 2 (e.g., Farmer 1968; Serafim 1968; Winterkorn and Fang 1975; Jaeger and Cook 1976; Lama and Vutukuri 1978; Costa and Baker 1981). Recently, Lock et al (2003) investigated the use of the image analysis of the pore structure for the estimation of the permeability of sandstone.…”
Section: Computational Modelingmentioning
confidence: 99%
“…For example, use of correlations based on natural soils that relate liquid limit (Terzaghi and Peck 1967) or plasticity index (Wroth and Wood . In terms of the swelling index, observed values were generally less than the compression index by a factor of 10, which is typical for a variety of soils (Winterkorn and Fang 1975). The influence of biofilm on swelling is modest but consistent for both soils tested.…”
Section: Consolidationmentioning
confidence: 68%
“…Pycnometer test was conducted in order to be used in hydrometer analysis in accordance with ASTM D 854 and the specific bulk density of the soils tested were found to be in the range of 2.4 -2.8 g/cm 3 . The results are shown in Table 3 below.…”
Section: Pycnometer Test Results (Unit Weight Of Solids)mentioning
confidence: 99%
“…Liquid phase, on the other hand, is usually an aqueous electrolyte solution. Depending on the biological activity in the soil and its location along with the effects of its contact with the atmosphere, the gas phase may have a different secondary composition [3]. Soil, as a result of several different materials it contains, emerges as a carrier material beneath the foundation of structures and as a material used to produce soil structures (earth dam, land reclamation, banks, etc.).…”
Section: Introductionmentioning
confidence: 99%