On the relationship between induced polarization and surface area in metal-sand and clay-sand mixtures

By L. Slater, D. Ntarlagiannis, D. Wishart. 2006

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An overview of the spectral induced polarization method for near-surface applications (2012, background): “As outlined at the end of the previous section, this statement holds today, although some of the above controls have been further investigated in laboratory studies over the past 15 years, including mainly textural parameters (e.g., Vanhala, 1997; Slater and Lesmes, 2002; Scott and Barker, 2003; Bin”
Cycling of extracellular DNA in the soil environment (2007, background): “Montmorillonite and kaolinite clays have specific surface areas of 812m2 g 1 (Petersen et al., 1996) and 10.97m2 g 1 (Slater et al., 2006), respectively, whereas Ottawa grade sand has a surface area of 0.0485m2 g 1 (Slater et al., 2006).”
Geophysical Properties of the Near Surface Earth: Electrical Properties (2015, background): “There now exists a substantial volume of literature demonstrating a power-law dependence of s00 on Spor, the surface area to pore volume ratio (B€orner and Sch€on, 1991; B€orner et al., 1996; Knight and Nur, 1987b; Sch€on, 2004; Slater and Lesmes, 2002; Slater et al., 2006) as shown in Figure 21.”
Modeling Soil Processes: Review, Key Challenges, and New Perspectives (2016, background): “, 2015), spectral-induced polarization (Slater et al., 2006), ground-penetrating radar (Huisman et al.”