Bohuslavite, Fe-4(3 )(PO4)(3)(SO4)(OH)(H2O)(10)center dot nH(2)O, a new hydrated iron phosphate-sulfate

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F19%3A73597999" target="_blank" >RIV/61989592:15310/19:73597999 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216224:14310/19:00113471

Výsledek na webu

<a href="https://pubs.geoscienceworld.org/eurjmin/article-abstract/31/5-6/1033/573675" target="_blank" >https://pubs.geoscienceworld.org/eurjmin/article-abstract/31/5-6/1033/573675</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1127/ejm/2019/0031-2892" target="_blank" >10.1127/ejm/2019/0031-2892</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Bohuslavite, Fe-4(3 )(PO4)(3)(SO4)(OH)(H2O)(10)center dot nH(2)O, a new hydrated iron phosphate-sulfate

Popis výsledku v původním jazyce

The new mineral species bohuslavite, Fe-4(3+)(PO4)(3)(SO4)(OH)(H2O)(10)center dot nH(2)O(5 &lt;= n &lt;= 14), has been discovered in the Buca della Vena baryte +/- iron oxides +/- pyrite ore deposit, Apuan Alps, Tuscany (Italy), and in the Horni Mesto deposit, northern Moravia (Czech Republic). It occurs as pinkish to lilac tabular 10011 crystals, with a pseudohexagonal outline, up to 0.25 mm in size, forming globular aggregates up to 1 mm across. At both localities, it is associated with gypsum. Optically, bohuslavite is biaxial negative. Indices of refraction and 2V angles, measured with white light, are alpha = 1.537(2), beta = 1.567(1), gamma = 1.568(1), 2V = 16(3)degrees and alpha = 1.550(2), beta = 1.579(2), gamma = 1.579(1), 2V = 5-10 degrees for the samples from Buca della Vena (BdV) and Horni Mesto (HM), respectively. Dispersion, with r &gt; nu, is slight in BdV sample and it was not observed in HM. In both cases, X approximate to c. No pleochroism was observed. Electron microprobe analyses gave (in wt% - mean of 10 spot analyses on each sample): SO3 10.92, P2O5 25.34, Al2O3 0.26, Fe2O3 40.70, H2O 35.96, total 113.18 (BdV), and SO3 9.32, P2O5 24.84, Al2O3 0.30, Fe2O3 36.63, H2O 32.49, total 103.58 (HIM). The H2O contents were determined through thermo-gravimetric analyses. Mossbauer spectroscopy indicated that all iron occurs as Fe3+. Thus, the empirical formulae of bohuslavite, based on Sigma(Fe,Al) = 4 atoms per formula unit (apfu), are (Fe3.96Al0.04)(PO4)(2).(77)(SO4)(1.06)(OH)(1.56()H2O)(10)center dot 7.90H(2)O (BdV) and (Fe3.96Al0.05)(PO4)(3.02)(SO4)(1.00)(OH)(0.94)(H2O)(10)center dot 5.08H(2)O (HM), ideally Fe-4(3+) (PO4)(3)(SO4)(OH)(H2O)(10)center dot nH(2)O. Bohuslavite is triclinic, space group P (1) over bar, with a = 13.376(3), b = 13.338(3), c = 10.863(4) angstrom, alpha = 92.80(2), beta = 91.03(2), gamma = 119.92(2)degrees, V = 1675.7(9) angstrom(3) , Z = 2 (sample BdV). The crystal structure was solved and refined to R-1 = 0.232 on the basis of 2177 unique reflections with F-o &gt; 4 sigma (F-o) and 208 refined parameters. Its crystal structure is based on {001} heteropolyhedral layers with composition [Fe-4(PO4)(3)O(OH)(H2O)(10)]. These layers are decorated, on both sides, by SO(4 )groups. Additional H2O groups are hosted in the interlayers and in the [001] channels. The name bohuslavite honours the Czech mineralogist and geologist Bohuslav Fojt for his contributions to mineralogy and economic geology. A third occurrence of bohuslavite from the Jeremias Gluck mine, Garnsdorf near Saalfeld, Thuringia (Germany), is briefly discussed.

Název v anglickém jazyce

Bohuslavite, Fe-4(3 )(PO4)(3)(SO4)(OH)(H2O)(10)center dot nH(2)O, a new hydrated iron phosphate-sulfate

Popis výsledku anglicky

The new mineral species bohuslavite, Fe-4(3+)(PO4)(3)(SO4)(OH)(H2O)(10)center dot nH(2)O(5 &lt;= n &lt;= 14), has been discovered in the Buca della Vena baryte +/- iron oxides +/- pyrite ore deposit, Apuan Alps, Tuscany (Italy), and in the Horni Mesto deposit, northern Moravia (Czech Republic). It occurs as pinkish to lilac tabular 10011 crystals, with a pseudohexagonal outline, up to 0.25 mm in size, forming globular aggregates up to 1 mm across. At both localities, it is associated with gypsum. Optically, bohuslavite is biaxial negative. Indices of refraction and 2V angles, measured with white light, are alpha = 1.537(2), beta = 1.567(1), gamma = 1.568(1), 2V = 16(3)degrees and alpha = 1.550(2), beta = 1.579(2), gamma = 1.579(1), 2V = 5-10 degrees for the samples from Buca della Vena (BdV) and Horni Mesto (HM), respectively. Dispersion, with r &gt; nu, is slight in BdV sample and it was not observed in HM. In both cases, X approximate to c. No pleochroism was observed. Electron microprobe analyses gave (in wt% - mean of 10 spot analyses on each sample): SO3 10.92, P2O5 25.34, Al2O3 0.26, Fe2O3 40.70, H2O 35.96, total 113.18 (BdV), and SO3 9.32, P2O5 24.84, Al2O3 0.30, Fe2O3 36.63, H2O 32.49, total 103.58 (HIM). The H2O contents were determined through thermo-gravimetric analyses. Mossbauer spectroscopy indicated that all iron occurs as Fe3+. Thus, the empirical formulae of bohuslavite, based on Sigma(Fe,Al) = 4 atoms per formula unit (apfu), are (Fe3.96Al0.04)(PO4)(2).(77)(SO4)(1.06)(OH)(1.56()H2O)(10)center dot 7.90H(2)O (BdV) and (Fe3.96Al0.05)(PO4)(3.02)(SO4)(1.00)(OH)(0.94)(H2O)(10)center dot 5.08H(2)O (HM), ideally Fe-4(3+) (PO4)(3)(SO4)(OH)(H2O)(10)center dot nH(2)O. Bohuslavite is triclinic, space group P (1) over bar, with a = 13.376(3), b = 13.338(3), c = 10.863(4) angstrom, alpha = 92.80(2), beta = 91.03(2), gamma = 119.92(2)degrees, V = 1675.7(9) angstrom(3) , Z = 2 (sample BdV). The crystal structure was solved and refined to R-1 = 0.232 on the basis of 2177 unique reflections with F-o &gt; 4 sigma (F-o) and 208 refined parameters. Its crystal structure is based on {001} heteropolyhedral layers with composition [Fe-4(PO4)(3)O(OH)(H2O)(10)]. These layers are decorated, on both sides, by SO(4 )groups. Additional H2O groups are hosted in the interlayers and in the [001] channels. The name bohuslavite honours the Czech mineralogist and geologist Bohuslav Fojt for his contributions to mineralogy and economic geology. A third occurrence of bohuslavite from the Jeremias Gluck mine, Garnsdorf near Saalfeld, Thuringia (Germany), is briefly discussed.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

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OECD FORD obor

10504 - Mineralogy

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2019

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

EUROPEAN JOURNAL OF MINERALOGY

ISSN

0935-1221

e-ISSN

—

Svazek periodika

31

Číslo periodika v rámci svazku

5-6

Stát vydavatele periodika

DE - Spolková republika Německo

Počet stran výsledku

14

Strana od-do

1033-1046

Kód UT WoS článku

000505169400015

EID výsledku v databázi Scopus

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