1990
DOI: 10.1021/cm00011a009
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Synthesis of metal hydroxide-layer silicate intercalation compounds (metal = Mg(II), Ca(II), Mn(II), Fe(II), Co(II), Ni(II), Zn(II), and Cd(II))

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Cited by 22 publications
(15 citation statements)
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“…Access to the gallery micropores was claimed for the LDH-Si802o 8-intercalates with gallery heights of ~7 ik. A related approach to mixed layered silicate metal (II) hydroxide compounds was reported by Ohtsuka et al (1990). The addition of a base to an aqueous suspension of sodium tetrasilicic mica exchanged with M(II) (Mg, Ca, Mn, Ni, Zn and Co, etc.)…”
Section: Resultsmentioning
confidence: 99%
“…Access to the gallery micropores was claimed for the LDH-Si802o 8-intercalates with gallery heights of ~7 ik. A related approach to mixed layered silicate metal (II) hydroxide compounds was reported by Ohtsuka et al (1990). The addition of a base to an aqueous suspension of sodium tetrasilicic mica exchanged with M(II) (Mg, Ca, Mn, Ni, Zn and Co, etc.)…”
Section: Resultsmentioning
confidence: 99%
“…In future work, these mechanisms will be examined for natural clay minerals, such as montmorillonite. Performing the cation exchange at a slightly increased pH (>8) is shown in the literature 46 48 to produce condensed chlorite-type interlayers only and therefore may double the adsorption capacity for CO 2 . Given the compact nature of clay minerals, this can make them volumetrically competitive compared to MOFs and mesoporous carbon.…”
Section: Discussionmentioning
confidence: 99%
“…This reaction produces a structure similar to chlorite. The transition metals of Mn 2+, Fe 2+, Co 2+, and Ni 2+ show similar intercalating behavior as more typical non-transition metals, such as Mg e § or AP + (Brindley and Kao, 1980;Ohtsuka et al, 1990;Yamanaka and Brindley, 1978). Transition elements generate interesting physical properties, including two-dimensional magnetic effects (e.g., Takahashi et al, 1986Takahashi et al, , 1988.…”
Section: Introductionmentioning
confidence: 96%
“…The mica-like material, NaMgzsSi4010F2, used by Ohtsuka et al (1990) and Takahashi et al (1986Takahashi et al ( , 1988) is similar to vermiculite owing to its high layer charge. However, its properties are similar to smectite in both small particle size and high-swelling behavior.…”
Section: Introductionmentioning
confidence: 99%