B. Lanson et al., Structure of H-exchanged hexagonal birnessite and its mechanism of formation from Na-rich monoclinic buserite at low pH, AM MINERAL, 85(5-6), 2000, pp. 826-838
The structural transformation of high pH Na-rich buserite (NaBu) to H-excha
nged hexagonal birnessite (HBi) at low pH was studied by simulation of expe
rimental X-ray diffraction patterns. Four HBi samples were prepared by equi
libration of NaBu at constant pH in the range pH 5-2. The samples differ fr
om each other by the presence or one (at pH 2 and 3) or two (at pH 4 and 5)
phases, and by the structural heterogeneity of these phases which decrease
s with decreasing pH. The sample obtained at pH 5 is a 4:1 physical mixture
of a 1H phase (a = 4.940 Angstrom. b = a/root 3 = 2.852 Angstrom, c = 7.23
5 Angstrom, beta = 90 degrees, gamma = 90 degrees) and of a 1M phase (a = 4
.940 Angstrom, b = a/root 3 = 2.852 Angstrom, c= 7.235 Angstrom, beta = 119
.2 degrees, gamma = 90 degrees) in which successive layers are shifted with
respect to each other by +a/3 along the a axis as in chalcophanite. Both t
he 1H and 1M phases contain very few well-defined stacking faults at pH 5.
At pH 3, the sample is a 8:5 physical mixture of a 1H phase containing 15%
of monoclinic layer pairs and of a 1M phase containing 40% of orthogonal la
yer pairs. Any further decrease of the pH leads to the formation of a singl
e defective 1H phase. This III phase contains 20% and 5% of monoclinic laye
r pairs at pH 3 and 2, respectively. Independent of pH, all phases contain
0.833 Mn-layer cations, 0.167 vacant layer sites, and 0.167 interlayer Mn c
ations located either above or below layer vacancies per octahedron. A stru
ctural formula is established at each pH.
The origin of the observed phase and structural heterogeneities has been an
alyzed. 1H and 1M phases are assumed to inherit their specific structural a
nd crystal chemical features from the two distinct NaBu modifications. NaBu
type I, with a high proportion of Mn-layer(4+) cations, is thought to be r
esponsible for the monoclinic layer stacking because this configuration all
ows Mn cations from adjacent layers to be as far as possible from each othe
r, thus minimizing the electrostatic repulsion between these high charge ca
tions. In contrast, NaBu type Il has a high interlayer charge induced by Mn
-layer(3+) for Mn-layer(4+) substitutions. Consequently, the 1H phase has a
high amount of interlayer protons and achieves compensation of the unfavor
able overlap of layer and interlayer Mn cations, in projection on the nb-pl
ane, by the presence of strong hydrogen bondings between layers, The higher
proportion of defined stacking faults in both 1H and 1M phases at pn 3 com
pared to pH 5 can be attributed to the increase in reaction rate with decre
asing pH. At lower pH (3 and 2) the formation or strong hydrogen bonds betw
een adjacent layers controls the layer stacking mode and leads to the forma
tion of a unique 1H phase. The proportion of well-defined stacking faults i
n this phase decreases from pH 3 to 2.