The role of charcoal on DTA curves of organo-clay complexes: an overview
By S. Yariv. 2004
164 citations recorded by the source corpus.
Subfields: Materials Chemistry, Polymers and Plastics, Spectroscopy
View Paper: https://www.semanticscholar.org/paper/e5bb9174c91d6f6b85f4e653de86b1538bb88e9b
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In Materials Chemistry
In Polymers and Plastics
In Spectroscopy
Citations in the corpus
- Porous clay bricks manufactured with rice husks (2013, background): “The first 5% decrease in the mass occurred in between 20 and 100 C due to the evaporation of physical water [26].”
- Silylation of clay mineral surfaces (2013, background): “In this case, surfactants enter the interlayer spaces mainly by replacing the initial inorganic cations and electrostatic force is the main linkage between surfactant cations and clay mineral (Lagaly, 1981; Yariv, 2004).”
- Thermal Characterization of Surfactant-Modified Montmorillonites (2005, background): “This peak corresponds to the oxidation of residual organic carbonaceous residue (Xie et al., 2001b; Yariv, 2004).”
- Microstructure of HDTMA+-modified montmorillonite and its influence on sorption characteristics (2006, background): “…of Na-Mt is composed of three peaks around 34.4, 107.8 and 619.3ºC, corresponding to surface adsorbed water, hydrated water of the interlayer cations and the structural water (bonded hydroxyl groups that undergo dehydroxylation), respectively (Xie et al. , 2002; Yariv, 2004; He et al. , 2005).”