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- W1568640508 abstract "Publisher Summary Illite as a non-swelling clay mineral of layer structure plays a very important role in this chapter. This special role is due to the fact that both sides of the surface of the silicate lamellae are made up of SiO 4 -tetrahedron planar lattices, and this structure — even when hydrophobized — is identical with the surface structure of montmorillonite and vermiculite, both of which are of the swelling type. The specific immersion wetting enthalpies of kaolinite, illite, and their organophilic derivatives are shown in this chapter. These data reveal that the heat of immersion in methanol is the highest in the case of the dialyzed mineral, and on increasing surface modification, its value decreases. The comparison of immersion wetting enthalpies relative to unit mass of the adsorbent is justified only in case if the specific surface area of the adsorbent is constant. Since dry organocomplexes have layer structure and their basal spacing can be determined by X-ray diffraction, it is possible to gain information about the structure (more precisely, the arrangement of the interlamellar chains) of the suspended and swollen adsorbent subjected to liquid sorption studies." @default.
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- W1568640508 date "1996-01-01" @default.
- W1568640508 modified "2023-09-27" @default.
- W1568640508 title "Chapter 3.9 Adsorption and immersional wetting on hydrophilic and hydrophobic silicates" @default.
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- W1568640508 doi "https://doi.org/10.1016/s0167-2991(06)81047-5" @default.
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