Abstract. The new mineral batoniite,
[Al8(OH)14(H2O)18](SO4)5 ⋅ 5H2O,
was discovered in the Cetine di Cotorniano Mine, Chiusdino, Siena,
Tuscany, Italy. It occurs as hemispherical aggregates composed of brittle
tabular crystals, up to 1 mm in size, white to colorless in color, with a
white streak and a vitreous to greasy luster. Batoniite is biaxial negative,
with α= 1.4833(6), β= 1.4948(6), γ= 1.5019(5)
(589 nm), and 2V(meas.)= 71(1)∘. Electron microprobe
analysis, affected by the dehydration of batoniite under the chamber vacuum,
gave (in wt %) the following: Al2O3 33.48, Fe2O3 0.05, SO3
33.00, and H2Ocalc 44.41, total 110.94. It corresponds to the chemical
formula (Al7.98Fe0.013+)Σ7.99(SO4)5.01(OH)13.95(H2O)18 ⋅ 5H2O. Batoniite is triclinic, belonging to space group P1‾, with a= 9.1757(6), b= 12.0886(9), c= 20.9218(15) Å, α= 82.901(3),
β= 87.334(3), γ= 86.999(2)∘, V= 2297.8(3) Å3, and Z= 2. The crystal structure was refined to R1= 0.0916
for 8118 unique reflections with Fo>4σ(Fo) and
811 refined parameters and 60 restraints. Batoniite is characterized by
isolated [Al8(OH)14(H2O)18]10+ polyoxocations,
H-bonded to five interstitial (SO4)2− and five H2O groups. In
type material, it is associated with gypsum and a poorly crystallized Al–Fe
sulfate. The crystallization of batoniite is probably due to the action of
H2SO4 on Al-bearing rocks of Paleozoic age cropping out in the
Garibaldi Tunnel, the lowest mining level of the Cetine di Cotorniano Mine.