2015
DOI: 10.1021/acs.iecr.5b03207
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Structure of the Carbonate-Intercalated Layered Double Hydroxides: A Reappraisal

Abstract: Carbonate-intercalated layered double hydroxides have hitherto been thought to crystallize with rhombohedral symmetry (space group R3̅m). This widely accepted structure model comprises positively charged metal hydroxide layers wherein the cations are disordered. However, spectroscopic studies and simple chemical considerations militate against the possibility of cation disorder. This study shows that the observed powder X-ray diffraction pattern can indeed be fit to a cation-ordered crystal with monoclinic sym… Show more

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Cited by 26 publications
(35 citation statements)
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“…Despite the general viewpoint that the 3 R polytype is the most common for hydrotalcite-supergroup minerals, crystal-structure studies of members that combine the M 2+ : M 3+ ratio of 2:1 and a rhombohedral stacking sequence indicate a high tendency for the M 2+ and M 3+ cations to form × superstructures within brucite-type layers that results in a monoclinic symmetry (Table 2) due to the disappearance of threefold axes (synthetic LDHs with Li:Al = 1:2 [Sissoko et al ., 1985; Britto et al ., 2008; Britto and Kamath, 2009], quintinite-1 M [Krivovichev et al ., 2010 b , 2012 a , Zhitova et al ., 2016 c ; Jayanthi et al ., 2015]; synthetic LDHs with Zn:Al = 2:1 [Marappa and Kamath, 2015]). It is important to emphasize that a ‘classic’ 3 R polytype was found for a quintinite sample with a very high content of Fe 2+ .…”
Section: Discussionmentioning
confidence: 99%
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“…Despite the general viewpoint that the 3 R polytype is the most common for hydrotalcite-supergroup minerals, crystal-structure studies of members that combine the M 2+ : M 3+ ratio of 2:1 and a rhombohedral stacking sequence indicate a high tendency for the M 2+ and M 3+ cations to form × superstructures within brucite-type layers that results in a monoclinic symmetry (Table 2) due to the disappearance of threefold axes (synthetic LDHs with Li:Al = 1:2 [Sissoko et al ., 1985; Britto et al ., 2008; Britto and Kamath, 2009], quintinite-1 M [Krivovichev et al ., 2010 b , 2012 a , Zhitova et al ., 2016 c ; Jayanthi et al ., 2015]; synthetic LDHs with Zn:Al = 2:1 [Marappa and Kamath, 2015]). It is important to emphasize that a ‘classic’ 3 R polytype was found for a quintinite sample with a very high content of Fe 2+ .…”
Section: Discussionmentioning
confidence: 99%
“…We note that the structural model of the 1 M polytype proposed by us for quintinite-1 M was used by Jayanthi et al . (2015) for synthetic LDHs and applied for the Rietveld structure refinement of the synthetic analogue of zaccagnaite, [Zn 4 Al 2 (OH) 12 ][(CO 3 )(H 2 O) 3 ] (Marappa and Kamath, 2015).…”
Section: Introductionmentioning
confidence: 99%
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“…Also the lattice constant "a" results in a linear combination of ionic radii and molar fraction x. Nevertheless, some local cations order has been documented, and some authors have highlighted longrange cation ordering of organized superstructures [4,9,10]. Anyway results are still controversial.…”
Section: +mentioning
confidence: 99%
“…The important characteristics of LDHs is that these moieties are generally weakly bound to the host lamellas and can therefore either be located during the 3D structure formation or be inserted by subsequent substitution trough anionic exchange [10]. The anions can be grouped as follows:…”
Section: Intercalated Anionsmentioning
confidence: 99%