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Somersetite, Pb8O(OH)4(CO3)5, a new complex hydrocerussite-related mineral from the Mendip Hills, England. / Siidra , O.I.; Nekrasova , D.O.; Turner, Rick; Zaitsev, A.N.; Chukanov, N.V.; Polekhovsky, Y.S.; Spratt, John; Rumsey, M.S.

In: Mineralogical Magazine, Vol. 82, No. 5, 10.2018, p. 1211-1224.

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Siidra , OI, Nekrasova , DO, Turner, R, Zaitsev, AN, Chukanov, NV, Polekhovsky, YS, Spratt, J & Rumsey, MS 2018, 'Somersetite, Pb8O(OH)4(CO3)5, a new complex hydrocerussite-related mineral from the Mendip Hills, England', Mineralogical Magazine, vol. 82, no. 5, pp. 1211-1224. https://doi.org/10.1180/minmag.2017.081.087

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Author

Siidra , O.I. ; Nekrasova , D.O. ; Turner, Rick ; Zaitsev, A.N. ; Chukanov, N.V. ; Polekhovsky, Y.S. ; Spratt, John ; Rumsey, M.S. / Somersetite, Pb8O(OH)4(CO3)5, a new complex hydrocerussite-related mineral from the Mendip Hills, England. In: Mineralogical Magazine. 2018 ; Vol. 82, No. 5. pp. 1211-1224.

BibTeX

@article{ad8722f3dd7847c4a33b7f4b910dc5e4,
title = "Somersetite, Pb8O(OH)4(CO3)5, a new complex hydrocerussite-related mineral from the Mendip Hills, England",
abstract = "The new mineral somersetite, has been found at Ton Works ('Merehead quarry') in Somerset, England, United Kingdom. Somersetite is green or white (typically it is similar visually to hydrocerussite-like minerals but with a mint-green tint), forms plates and subhedral grains up to 5 mm across and up to 2 mm thick. In bi-coloured crystals it forms very thin intergrowths with plumbonacrite. The empirical formula of somersetite is Pb8.00C5.00H4.00O20. The simplified formula is Pb8O(OH)(4)(CO3)(5) ,which requires: PbO = 87.46, CO2 = 10.78, H2O = 1.76, total 100.00 wt.%.The infrared spectrum of somersetite is similar to that of plunbonacrite and, to a lesser degree, bydrocerussite. Somersetite is hexagonal, P6(3)/mmc, a = 5.2427(7), c = 40.624(6) , V = 967.0(3) (3) and Z = 2. The eight strongest reflections of the powder X-ray diffraction (XRD) pattern [d,(I)(hkl)] are: 4.308(33) (103), 4.148(25)(104), 3.581(40)(107), 3.390(100)(108), 3.206(55)(109), 2.625(78)(110), 2.544(98)(0.0.16) and 2.119(27)(1.0.17). The crystal structure was solved from single-crystal XRD data giving R-1 = 0.031. The structure of somersetite is unique and consists of the alternation of the electroneutral plumbonacrite-type [Pb5O (OH)(2)(CO3)(3)](0) and hydrocerussite-type [Pb-3(OH)(2)(CO3)(2)](0) blocks separated by stereochemically active lone electron pairs on Pb-2(+). There are two blocks of each type per unit cell in the structure, which corresponds to the formula [Pb5O(OH)(2)(CO3)(3)][Pb-3(OH)(2)(CO3)(2)] or Pb8O(OH)(4)(CO3)(5) in a simplified representation. The 2D blocks are held together by weak Pb-O bonds and weak interactions between lone pairs.",
keywords = "somersetite, hydrocerussite, plumbonacrite, new mineral, lead, carbonate, layered structure, Merehekul quarry, Torr works, lone electron pair, CRYSTAL-STRUCTURE, MEREHEAD QUARRY, PB4SO4(CO3)(2)(OH)(2), MACPHERSONITE, OXYCHLORIDE, CHEMISTRY",
author = "O.I. Siidra and D.O. Nekrasova and Rick Turner and A.N. Zaitsev and N.V. Chukanov and Y.S. Polekhovsky and John Spratt and M.S. Rumsey",
year = "2018",
month = oct,
doi = "10.1180/minmag.2017.081.087",
language = "English",
volume = "82",
pages = "1211--1224",
journal = "Mineralogical Magazine",
issn = "0026-461X",
publisher = "Mineralogical Society",
number = "5",

}

RIS

TY - JOUR

T1 - Somersetite, Pb8O(OH)4(CO3)5, a new complex hydrocerussite-related mineral from the Mendip Hills, England

AU - Siidra , O.I.

AU - Nekrasova , D.O.

AU - Turner, Rick

AU - Zaitsev, A.N.

AU - Chukanov, N.V.

AU - Polekhovsky, Y.S.

AU - Spratt, John

AU - Rumsey, M.S.

PY - 2018/10

Y1 - 2018/10

N2 - The new mineral somersetite, has been found at Ton Works ('Merehead quarry') in Somerset, England, United Kingdom. Somersetite is green or white (typically it is similar visually to hydrocerussite-like minerals but with a mint-green tint), forms plates and subhedral grains up to 5 mm across and up to 2 mm thick. In bi-coloured crystals it forms very thin intergrowths with plumbonacrite. The empirical formula of somersetite is Pb8.00C5.00H4.00O20. The simplified formula is Pb8O(OH)(4)(CO3)(5) ,which requires: PbO = 87.46, CO2 = 10.78, H2O = 1.76, total 100.00 wt.%.The infrared spectrum of somersetite is similar to that of plunbonacrite and, to a lesser degree, bydrocerussite. Somersetite is hexagonal, P6(3)/mmc, a = 5.2427(7), c = 40.624(6) , V = 967.0(3) (3) and Z = 2. The eight strongest reflections of the powder X-ray diffraction (XRD) pattern [d,(I)(hkl)] are: 4.308(33) (103), 4.148(25)(104), 3.581(40)(107), 3.390(100)(108), 3.206(55)(109), 2.625(78)(110), 2.544(98)(0.0.16) and 2.119(27)(1.0.17). The crystal structure was solved from single-crystal XRD data giving R-1 = 0.031. The structure of somersetite is unique and consists of the alternation of the electroneutral plumbonacrite-type [Pb5O (OH)(2)(CO3)(3)](0) and hydrocerussite-type [Pb-3(OH)(2)(CO3)(2)](0) blocks separated by stereochemically active lone electron pairs on Pb-2(+). There are two blocks of each type per unit cell in the structure, which corresponds to the formula [Pb5O(OH)(2)(CO3)(3)][Pb-3(OH)(2)(CO3)(2)] or Pb8O(OH)(4)(CO3)(5) in a simplified representation. The 2D blocks are held together by weak Pb-O bonds and weak interactions between lone pairs.

AB - The new mineral somersetite, has been found at Ton Works ('Merehead quarry') in Somerset, England, United Kingdom. Somersetite is green or white (typically it is similar visually to hydrocerussite-like minerals but with a mint-green tint), forms plates and subhedral grains up to 5 mm across and up to 2 mm thick. In bi-coloured crystals it forms very thin intergrowths with plumbonacrite. The empirical formula of somersetite is Pb8.00C5.00H4.00O20. The simplified formula is Pb8O(OH)(4)(CO3)(5) ,which requires: PbO = 87.46, CO2 = 10.78, H2O = 1.76, total 100.00 wt.%.The infrared spectrum of somersetite is similar to that of plunbonacrite and, to a lesser degree, bydrocerussite. Somersetite is hexagonal, P6(3)/mmc, a = 5.2427(7), c = 40.624(6) , V = 967.0(3) (3) and Z = 2. The eight strongest reflections of the powder X-ray diffraction (XRD) pattern [d,(I)(hkl)] are: 4.308(33) (103), 4.148(25)(104), 3.581(40)(107), 3.390(100)(108), 3.206(55)(109), 2.625(78)(110), 2.544(98)(0.0.16) and 2.119(27)(1.0.17). The crystal structure was solved from single-crystal XRD data giving R-1 = 0.031. The structure of somersetite is unique and consists of the alternation of the electroneutral plumbonacrite-type [Pb5O (OH)(2)(CO3)(3)](0) and hydrocerussite-type [Pb-3(OH)(2)(CO3)(2)](0) blocks separated by stereochemically active lone electron pairs on Pb-2(+). There are two blocks of each type per unit cell in the structure, which corresponds to the formula [Pb5O(OH)(2)(CO3)(3)][Pb-3(OH)(2)(CO3)(2)] or Pb8O(OH)(4)(CO3)(5) in a simplified representation. The 2D blocks are held together by weak Pb-O bonds and weak interactions between lone pairs.

KW - somersetite

KW - hydrocerussite

KW - plumbonacrite

KW - new mineral

KW - lead

KW - carbonate

KW - layered structure

KW - Merehekul quarry

KW - Torr works

KW - lone electron pair

KW - CRYSTAL-STRUCTURE

KW - MEREHEAD QUARRY

KW - PB4SO4(CO3)(2)(OH)(2)

KW - MACPHERSONITE

KW - OXYCHLORIDE

KW - CHEMISTRY

UR - https://www.cambridge.org/core/product/identifier/S0026461X18000956/type/journal_article

UR - http://www.mendeley.com/research/somersetite-pb8ooh4co35-new-complex-hydrocerussiterelated-mineral-mendip-hills

U2 - 10.1180/minmag.2017.081.087

DO - 10.1180/minmag.2017.081.087

M3 - Article

VL - 82

SP - 1211

EP - 1224

JO - Mineralogical Magazine

JF - Mineralogical Magazine

SN - 0026-461X

IS - 5

ER -

ID: 36123451