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Pring, Allan

Publications and source records attributed to Pring, Allan.

The role of Te(IV) and Bi(III) chloride complexes in hydrothermal mass transfer: An X-ray absorption spectroscopic study

Tellurium (Te) and bismuth (Bi) are two metal(loid)s often enriched together with gold (Au) in hydrothermal deposits; however the speciation and transport properties for these two metals in hydrothermal systems are poorly understood. We investigated the effect of chloride on the speciation of Te(IV) and Bi(III) in hydrothermal solutions using in-situ XAS spectroscopy. At ambient temperature, oxy-hydroxide complexes containing the [TeO3] moiety (e.g., H3TeO3+ under highly acidic conditions) predominate in salty solutions over a wide range in pH and salt concentrations. Te(IV)-Cl complexes only appear at pH(25 degrees C) <= 2 and high Cl- activity (>= 10). The highest order Te(IV) chloride complex detected is TeCl4(aq), and contains the [TeCl4] moiety. Upon heating to 199 degrees C, the Te(IV)-Cl complexes become more stable; however they still required highly acidic conditions which are likely to exist only in very limited environments in nature. At ambient temperature, Bi(III) is coordinated to 5.5(5) Cl atoms in high salinity, acidic (HCl >= 0.5 m) chloride solutions. This, combined with large EXAFS-derived structural disorder parameters, suggests that the Bi(III) complex is most likely present as both BiCl52- and BiCl63-. The number of Cl atoms coordinated to Bi(III) decreases with increasing temperature; at around 200 degrees C and above, Bi(III) is coordinated to three Cl atoms. Overall the data show that Te(IV) chloride complexes can be ignored in predicting Te mobility under oxidizing conditions in most geological environments, but that Bi(III) chloride complexes are expected to account for Bi mobility in acidic brines. New thermodynamic properties for Bi(III) chloride complexes are provided to improve reactive transport modeling of Bi up to 500 degrees C. Although higher order complexes such as BiCl52- and BiCl63- exist at ambient temperature, the BiCl3(aq) complex becomes the predominant chloride complex in saline solutions at T >= 200 degrees C.

Etschmann, Barbara E.↗

Kapundaite, (Na,Ca)[subscript 2]Fe[subscript 4][superscript 3+](PO[subscript 4])[subscript 4](OH)[subscript 3]·5H[subscript 2]O, a new phosphate species from Toms quarry, South Australia: Description and structural relationship to mélonjosephite

Kapundaite, ideally (Na,Ca){sub 2}Fe{sub 4}{sup 3+}(PO{sub 4}){sub 4}(OH){sub 3}{center_dot}5H{sub 2}O, is a new mineral (IMA2009-047) from Toms phosphate quarry, Kapunda, South Australia, Australia. The new mineral occurs as cavernous aggregates of fibers up to several centimeters across, associated with leucophosphite, natrodufrenite, and meurigite-Na crystals and amorphous brown, black, and/or greenish coatings. Individual kapundaite crystals are very thin flattened fibers up to a few millimeters in length, but typically no more than a few micrometers in thickness. The main form observed is {l_brace}100{r_brace}; other forms in the [010] zone are present, but cannot be measured. Crystals of kapundaite are pale to golden yellow, transparent to translucent, have a yellow streak and silky luster, and are non-fluorescent. Mohs hardness is estimated to be about 3; no twinning or cleavage was observed. Kapundaite is biaxial (+), with indices of refraction = 1.717(3), {beta} = 1.737(3), and {gamma} = 1.790(3). 2V could not be measured; 2V{sub calc} is 64.7{sup o}. The optical orientation is Z = b, Y {approx} c with weak pleochroism: X = nearly colorless, Y = light brown, Z = pale brown; absorption: Y > Z > X. No dispersion was observed. The empirical chemical formula (mean of seven electron microprobe analyses) calculated on the basis of 24 O is (Ca{sub 1.13}Na{sub 0.95}){sub {Sigma}2.08}(Fe{sub 3.83}{sup 3+}Mn{sub 0.03}Al{sub 0.02}Mg{sub 0.01}){sub {Sigma}3.89}P{sub 3.92}O{sub 16}(OH){sub 3}{center_dot}5H{sub 2.11}O. Kapundaite is triclinic, space group P{sub {bar 1}}, a = 6.317(5), b = 7.698(6), c = 9.768(7) {angstrom}, {alpha} = 105.53(1){sup o}, {beta} = 99.24(2){sup o}, {gamma} = 90.09(2){sup o}, V = 451.2(6) {angstrom}{sup 3}, and Z = 1. The five strongest lines in the powder X-ray diffraction pattern are [d{sub obs} in {angstrom} (I) (hkl)]: 9.338 (100) (001), 2.753 (64) (2{sub {bar 1}}1), 5.173 (52) (011), 2.417 (48) ({sub {ovr 21}}3, 202, 0{sub {bar 1}}4), and 3.828 (45) (0{sub {bar 2}}1). The crystal structure was solved from single-crystal X-ray diffraction data using synchrotron radiation and refined to R{sub 1} = 0.1382 on the basis of 816 unique reflections with F{sub o} > 4{sub {sigma}}F. The structure of kapundaite is based on a unique corrugated octahedral-tetrahedral sheet, which is composed of two types of chains parallel to a. Kapundaite is structurally related to melonjosephite. The mineral is named for the nearest town to the quarry.

36 MATERIALS SCIENCE↗