Hydrotalcite-like and manasseite-like minerals occur as polytypes in rhombohedral and hexagonal forms, respectively. The general formula is [Mg1-xAlx(OH)2]x+ [(CO3)x/2 . nH2O]x- , where x = 0.25 to 0.33 (Drits et al., 1987). In general, the structure is a brucite-like positively charged layer separated by CO3 anions and H2O as interlayer material, but substitutions are common. The International Mineralogical Association recognizes different species (below), based primarily on chemical differences, although there are many other un-named forms. These minerals occur in saline deposits, pegmatites, and serpentinites. Hydrothermal synthesis is relatively easy, as is anion exchange.
Cf., anionic clay (Part A), double metal hydroxides (Part A)
barbertonite Mg6Cr2(OH)16CO3 . 4(H2O)
carrboydite (Ni,Cu)5.90Al4.48(OH)21.69(SO4,CO3)2.78 . 3.67(H2O)
chlormagaluminite (Mg3.55Fe2+0.27Na0.05)(Al1.93Fe3+0.07Ti0.01)(OH)12 . Cl2CO3 . 2(H2O)
coalingite Mg10Fe3+2(OH)24CO3 . 2(H2O); Mg16Fe3+2(OH)36CO3 . 2(H2O)
desautelsite Mg6Mn2(OH)16CO3 . 4(H2O)
honessite [Ni5.55Mg0.10Fe3+2.35(OH)16](SO4)1.18 . nH2O
hydrohonessite [Ni5.43Fe3+2.57(OH)16](SO4)1.286.95H2O . 0.98NiSO4
hydrotalcite Mg6Al2(OH)16CO3 . 4(H2O); Mg4Al2(OH)12SO4 . 3(H2O)
iowaite Mg4.63Fe3+1.32(OH)12Cl1.33 . 1.95(H2O)
manasseite Mg6Al2(OH)16CO3 . 4(H2O); Mg4Al2(OH)12CO3 . 3(H2O)
meixnerite Mg6Al2(OH)16(OH)2 . 4(H2O)
motukoreaite [Mg1.82Mn0.03Zn0.02Al1.12(OH)5.15] . [Na0.07K0.07 (CO3)0.40(SO3)0.41 . 2.7(H2O)]
mountkeithite [(Mg8.15Ni0.85)(Fe3+1.31Cr1.02Al0.65)(OH)24](CO3)1.11(SO4)0.38(Mg1.76Ni0.18)(SO4)1.94(H2O)9.39
pyroaurite Mg6Fe3+2(OH)16CO3 . 4.5(H2O); Mg4Ni2+2Fe3+2(OH)16CO3 . 4(H2O)
reevesite Ni6Fe2+2(OH)16CO3 . 4(H2O)
sjögrenite Mg6Fe3+2(OH)16CO3 . 4.5(H2O)
stichtite Mg6Cr3(OH)16CO3 . 4(H2O); [Mg5.94(Cr1.29Al0.51Fe3+0.25)(OH)15.1][(CO3)1.473.7(H2O)]
takovite Ni6Al2(OH)16CO3OH . 4(H2O); [Ni5Mg0.10Fe3+0.13Al2.81(OH)14.42](CO3)2.27 . 5.4(H2O);
Ni6Al2(OH)16SO4OH . nH2O
wermlandite [Mg3.55(Al0.57Fe3+0.41)2(OH)18](Ca0.6Mg0.4)(SO4)2 . 12(H2O)
woodwardite Cu4Al2(OH)12SO4 . 2-4H2O