Alkali sulfates with aphthitalite-like structures from fumaroles of the tolbachik volcano, kamchatka, russia. iii. solid solutions and exsolutions

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Alkali sulfates with aphthitalite-like structures from fumaroles of the tolbachik volcano, kamchatka, russia. iii. solid solutions and exsolutions. / SHCHIPALKINA, NADEZHDA V.; PEKOV, IGOR V.; BRITVIN, SERGEY N.; KOSHLYAKOVA, NATALIA N.; SIDOROV, EVGENY G.

In: Canadian Mineralogist, Vol. 59, No. 4, 13.09.2021, p. 713-727.

Research output: Contribution to journal › Article › peer-review

BibTeX

@article{ff6d3901d86a42aa9ddaf4e6c7b41e8d,

title = "Alkali sulfates with aphthitalite-like structures from fumaroles of the tolbachik volcano, kamchatka, russia. iii. solid solutions and exsolutions",

abstract = "Six different exsolution types are found in crystals of aphthitalite-group alkali sulfates from exhalations of the active Arsenatnaya fumarole, Tolbachik volcano, Kamchatka, Russia. The coexisting minerals in these exsolutions are metath{\'e}nardite, ideally Na2SO4 (P63/mmc), and vanthoffite, Na6Mg(SO4)4 (P21/c) (Type I); metath{\'e}nardite and belomarinaite, KNaSO4 (P3m1) (Type II); th{\'e}nardite, Na2SO4 (Fddd), and aphthitalite, K3Na(SO4)2 (P3m1) (Type III); aphthitalite and arcanite, K2SO4 (Pnma) (Type IV); metath{\'e}nardite and natroaphthitalite, KNa3(SO4)2 (P3m1) (Type V); and two chemical varieties of metath{\'e}nardite (Type VI). The exsolution processes occur in crystals belonging to the high-temperature, hexagonal Na2SO4(I) (= metath{\'e}nardite, P63/mmc) structure type with different K:Na ratios formed at temperatures higher than 500 8C. The similarity and hexagonal close-packed nature of the crystal structures of the coexisting phases, all representatives of aphthitalite-like structure types, cause the coherent conjugation of domains during diffusion and cation ordering in the parent phase. The breakdown of solid solution can be facilitated by the mosaic character of crystals of a parent phase (incoherent grain boundaries) and the presence of coherent twin boundaries. The heating of samples with exsolution Types II and V up to 700 8C over 24 h shows that diffusion of K and Na through the domain borders does not result in the complete disorder of these cations and the extinction of domains with different crystal structures.",

keywords = "Aphthitalite, Arcanite, Belomarinaite, Cation ordering, Fumarole, K2SO4-Na2SO4 system, Metath{\'e}nardite, Natroaphthitalite, Solid-state transformation, Tolbachik volcano",

author = "SHCHIPALKINA, {NADEZHDA V.} and PEKOV, {IGOR V.} and BRITVIN, {SERGEY N.} and KOSHLYAKOVA, {NATALIA N.} and SIDOROV, {EVGENY G.}",

note = "Nadezhda V. Shchipalkina, Igor V. Pekov, Sergey N. Britvin, Natalia N. Koshlyakova, Evgeny G. Sidorov; Alkali sulfates with aphthitalite-like structures from fumaroles of the Tolbachik volcano, Kamchatka, Russia. III. Solid solutions and exsolutions. The Canadian Mineralogist 2021;; 59 (4): 713–727. doi: https://doi.org/10.3749/canmin.2000105",

year = "2021",

month = sep,

day = "13",

doi = "10.3749/canmin.2000105",

language = "English",

volume = "59",

pages = "713--727",

journal = "Canadian Mineralogist",

issn = "0008-4476",

publisher = "Mineralogical Association of Canada",

number = "4",

}

RIS

TY - JOUR

T1 - Alkali sulfates with aphthitalite-like structures from fumaroles of the tolbachik volcano, kamchatka, russia. iii. solid solutions and exsolutions

AU - SHCHIPALKINA, NADEZHDA V.

AU - PEKOV, IGOR V.

AU - BRITVIN, SERGEY N.

AU - KOSHLYAKOVA, NATALIA N.

AU - SIDOROV, EVGENY G.

N1 - Nadezhda V. Shchipalkina, Igor V. Pekov, Sergey N. Britvin, Natalia N. Koshlyakova, Evgeny G. Sidorov; Alkali sulfates with aphthitalite-like structures from fumaroles of the Tolbachik volcano, Kamchatka, Russia. III. Solid solutions and exsolutions. The Canadian Mineralogist 2021;; 59 (4): 713–727. doi: https://doi.org/10.3749/canmin.2000105

PY - 2021/9/13

Y1 - 2021/9/13

N2 - Six different exsolution types are found in crystals of aphthitalite-group alkali sulfates from exhalations of the active Arsenatnaya fumarole, Tolbachik volcano, Kamchatka, Russia. The coexisting minerals in these exsolutions are metathénardite, ideally Na2SO4 (P63/mmc), and vanthoffite, Na6Mg(SO4)4 (P21/c) (Type I); metathénardite and belomarinaite, KNaSO4 (P3m1) (Type II); thénardite, Na2SO4 (Fddd), and aphthitalite, K3Na(SO4)2 (P3m1) (Type III); aphthitalite and arcanite, K2SO4 (Pnma) (Type IV); metathénardite and natroaphthitalite, KNa3(SO4)2 (P3m1) (Type V); and two chemical varieties of metathénardite (Type VI). The exsolution processes occur in crystals belonging to the high-temperature, hexagonal Na2SO4(I) (= metathénardite, P63/mmc) structure type with different K:Na ratios formed at temperatures higher than 500 8C. The similarity and hexagonal close-packed nature of the crystal structures of the coexisting phases, all representatives of aphthitalite-like structure types, cause the coherent conjugation of domains during diffusion and cation ordering in the parent phase. The breakdown of solid solution can be facilitated by the mosaic character of crystals of a parent phase (incoherent grain boundaries) and the presence of coherent twin boundaries. The heating of samples with exsolution Types II and V up to 700 8C over 24 h shows that diffusion of K and Na through the domain borders does not result in the complete disorder of these cations and the extinction of domains with different crystal structures.

AB - Six different exsolution types are found in crystals of aphthitalite-group alkali sulfates from exhalations of the active Arsenatnaya fumarole, Tolbachik volcano, Kamchatka, Russia. The coexisting minerals in these exsolutions are metathénardite, ideally Na2SO4 (P63/mmc), and vanthoffite, Na6Mg(SO4)4 (P21/c) (Type I); metathénardite and belomarinaite, KNaSO4 (P3m1) (Type II); thénardite, Na2SO4 (Fddd), and aphthitalite, K3Na(SO4)2 (P3m1) (Type III); aphthitalite and arcanite, K2SO4 (Pnma) (Type IV); metathénardite and natroaphthitalite, KNa3(SO4)2 (P3m1) (Type V); and two chemical varieties of metathénardite (Type VI). The exsolution processes occur in crystals belonging to the high-temperature, hexagonal Na2SO4(I) (= metathénardite, P63/mmc) structure type with different K:Na ratios formed at temperatures higher than 500 8C. The similarity and hexagonal close-packed nature of the crystal structures of the coexisting phases, all representatives of aphthitalite-like structure types, cause the coherent conjugation of domains during diffusion and cation ordering in the parent phase. The breakdown of solid solution can be facilitated by the mosaic character of crystals of a parent phase (incoherent grain boundaries) and the presence of coherent twin boundaries. The heating of samples with exsolution Types II and V up to 700 8C over 24 h shows that diffusion of K and Na through the domain borders does not result in the complete disorder of these cations and the extinction of domains with different crystal structures.

KW - Aphthitalite

KW - Arcanite

KW - Belomarinaite

KW - Cation ordering

KW - Fumarole

KW - K2SO4-Na2SO4 system

KW - Metathénardite

KW - Natroaphthitalite

KW - Solid-state transformation

KW - Tolbachik volcano

UR - http://www.scopus.com/inward/record.url?scp=85115772273&partnerID=8YFLogxK

U2 - 10.3749/canmin.2000105

DO - 10.3749/canmin.2000105

M3 - Article

AN - SCOPUS:85115772273

VL - 59

SP - 713

EP - 727

JO - Canadian Mineralogist

JF - Canadian Mineralogist

SN - 0008-4476

IS - 4

ER -

ID: 86274530