journal article·2013-06

Chemistry, morphology and structural characteristics of synthetic Al–Ni and Al–Co-lizardites

María Bentabol, María Dolores Ruiz Cruz

Applied Clay Science· Volume 77-78
Publisher page

Abstract

Abstract Al–Ni and Al–Co lizardites have been synthesized at hydrothermal conditions. The two phases display different morphologies: thin, dominantly curved platelets (Al–Ni); and stacks of very thin platy particles (Al–Co). The X-ray diffraction and transmission/analytical electron microscopy studies have been used to make accurate distinctions among different structural types and chemical populations. Al–Ni bearing lizardite includes a 1M polytype and probably very subordinate amounts of chlorite. Al–Co bearing lizardite includes two 1M polytypes with different cell-parameters, one of these consisting of an apparently modulated structure. Chemically, Al–Ni- and specially Al–Co lizardite consist of a mixture of two populations with tetrahedral compositions ~ Si1.8Al0.2 and Si2.0. In contrast with previously described Al-rich serpentines, our serpentines are characterized by an asymmetrical Al distribution, with VIAl on the order of 1.0 atom per formula unit.
Source: openaire · Quality: candidate unverified · Source record ↗

Research context

OpenAlex topics: Surface Chemistry and Catalysis · Muon and positron interactions and applications · Advanced Materials Characterization Techniques

SciVX discovery tags are terminology-based. OpenAlex topics are source-provided classifications.

References (47)

Show source-provided references
1. Serpentinites from Central Cuba: petrology and HRTEM study10.1127/0935-1221/2002/0014-0905 ↗
2. Polytypism of trioctahedral 1:1 layer silicates10.1346/CCMN.1969.0170605 ↗
3. Determination of chlorite composition by X-ray spacings and intensities10.1346/CCMN.1972.0200606 ↗
4. Structures of layer silicates
5. Structures and composition of other trioctahedral 1:1 phyllosilicates
6. First-principles calculation of the infrared spectrum of lizardite10.2138/am-2002-1003 ↗
7. Hydrothermal synthesis of Mg- and Mg–Ni-rich kaolinite10.1346/CCMN.2006.0540602 ↗
8. Synthesis of Ni-rich 1:1 phyllosilicates10.1346/CCMN.2007.0550604 ↗
9. Hydrothermal synthesis (200°C) of Co-kaolinite and Al–Co-serpentine10.1016/j.clay.2008.06.001 ↗
10. Chemistry, morphology and structural characteristics of synthetic Al-lizardite10.1180/claymin.2010.045.2.131 ↗
11. The structure and chemistry of hydrous nickel-containing silicate and nickel–aluminium hydroxyl minerals10.3406/bulmi.1980.7391 ↗
12. The modulated crystal structure of antigorite: the m=17 polysome10.2138/am-2004-0117 ↗
13. HRTEM evidence for 8-reversals in the m=17 antigorite polysome10.2138/am.2005.1634 ↗
14. High-resolution transmission electron microscopy (HRTEM) investigation of antigorite polysomes (m=15 to 18)10.2138/am.2007.2188 ↗
15. Revised structure models for antigorite: an HRTEM study10.2138/am-2002-1022 ↗
16. Implications of ferrous and ferric iron in antigorite10.2138/am.2012.3926 ↗
17. The layer silicates
18. Fourier transform Raman spectroscopy of kaolinite, dickite and halloysite10.1346/CCMN.1995.0430206 ↗
19. Mössbauer and infrared spectroscopy of lizardite-1T from Monte Fico, Elba10.1007/s002690050167 ↗
20. The chemical composition and infrared spectrum of nickel- and iron-substituted serpentine from a nickeliferous laterite profile, Soroako, Indonesia
21. Textural and structural transformations of kaolinites in aqueous solutions10.1016/S0169-1317(00)00018-1 ↗
22. Polytypes and higher-order structures of antigorite: a TEM study10.2138/am-2003-0104 ↗
23. Brindleyite, a nickel-rich aluminous serpentine mineral analogous to berthierine
24. Martín
25. The crystal structure of lizardite 1T: hydrogen bonds and polytypism
26. Carlosturanite (not picrolite) from Taberg, Sweden10.1180/minmag.1986.050.358.14 ↗
27. Antigorite polysomatism: behaviour during progressive metamorphism10.1007/BF00371235 ↗
28. The crystal structure of Mg end-member lizardite-1T forming polyhedral spheres from the Lizard, Cornwall10.1180/minmag.2010.074.2.277 ↗
29. Ordovician and Pennsylvanian berthierine-bearing flint clays10.1346/CCMN.2000.0480118 ↗
30. 27Al NMR spectroscopy of iron-bearing montmorillonite clays10.1021/j100370a069 ↗
31. The chemical constitution of clays
32. High-resolution NMR of inorganic solids. Influence of magnetic centers on magic-angle sample spinning lineshapes in some natural aliminosilicates
33. Influence of cation size on the curvature of serpentine minerals: HRTEM–AEM study and elastic theory10.1346/CCMN.2003.0510409 ↗
34. The vibrational spectrum of lizardite-1T [Mg3Si2O5(OH)4] at the Γ point: a contribution from an ab initio periodic B3LYP calculation10.2138/am.2009.3127 ↗
35. Zonación mineralógica en el contacto de un cuerpo intrusivo básico (Trías de la Dorsal Bética)
36. Infrared evidence of order–disorder in amesites
37. The effect of aluminium on the infrared spectra of 7Å trioctahedral minerals10.1180/minmag.1979.043.325.14 ↗
38. The IR spectra of ordered amesites
39. Effective ionic radii in oxides and fluorides10.1107/S0567740869003220 ↗
40. Geochemistry and mineralogy of the regolith profile over the Aries kimberlite pipe, Western Australia
41. Hydrothermal and metamorphic berthierine from the Kidd Creek volcanogenic massive sulfide deposit, Timmins, Ontario
42. Ordering in synthetic aluminous serpentines, infrared spectra and cell dimensions10.1007/BF00309857 ↗
43. Sur la présence de nickel dans un gisement de bauxite près de Mégare10.1007/BF00207026 ↗
44. Serpentine minerals: structures and petrology
45. Ab-initio synthesis and TEM confirmation of antigorite in the system MgO–SiO2–H2O10.2138/am-1997-7-814 ↗
46. Study of chrysotile asbestos by a high resolution electron microscope10.1107/S0365110X67003524 ↗
47. Study of microstructures of chrysotile asbestos by a high resolution electron microscope10.1107/S0567739471001402 ↗