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Thermodynamics of arsenates, selenites and sulphates in oxidising zone of sulphides ore deposits. VIII. Field of Thermal Stability of Synthetic Analog of Chalcomenite, its Dehydration and Dissociation. / Fokina, E.L.; Klimova, E.V.; Charykova, M.V.; Krivovichev, V.G.; Platonova, N.V.; Semenova, V.V.; Depmeier, W.

в: Geology of Ore Deposits, Том 56, № 7, 2014, стр. 538-545.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Fokina, EL, Klimova, EV, Charykova, MV, Krivovichev, VG, Platonova, NV, Semenova, VV & Depmeier, W 2014, 'Thermodynamics of arsenates, selenites and sulphates in oxidising zone of sulphides ore deposits. VIII. Field of Thermal Stability of Synthetic Analog of Chalcomenite, its Dehydration and Dissociation', Geology of Ore Deposits, Том. 56, № 7, стр. 538-545. https://doi.org/10.1134/S1075701514070058

APA

Fokina, E. L., Klimova, E. V., Charykova, M. V., Krivovichev, V. G., Platonova, N. V., Semenova, V. V., & Depmeier, W. (2014). Thermodynamics of arsenates, selenites and sulphates in oxidising zone of sulphides ore deposits. VIII. Field of Thermal Stability of Synthetic Analog of Chalcomenite, its Dehydration and Dissociation. Geology of Ore Deposits, 56(7), 538-545. https://doi.org/10.1134/S1075701514070058

Vancouver

Fokina EL, Klimova EV, Charykova MV, Krivovichev VG, Platonova NV, Semenova VV и пр. Thermodynamics of arsenates, selenites and sulphates in oxidising zone of sulphides ore deposits. VIII. Field of Thermal Stability of Synthetic Analog of Chalcomenite, its Dehydration and Dissociation. Geology of Ore Deposits. 2014;56(7):538-545. https://doi.org/10.1134/S1075701514070058

Author

Fokina, E.L. ; Klimova, E.V. ; Charykova, M.V. ; Krivovichev, V.G. ; Platonova, N.V. ; Semenova, V.V. ; Depmeier, W. / Thermodynamics of arsenates, selenites and sulphates in oxidising zone of sulphides ore deposits. VIII. Field of Thermal Stability of Synthetic Analog of Chalcomenite, its Dehydration and Dissociation. в: Geology of Ore Deposits. 2014 ; Том 56, № 7. стр. 538-545.

BibTeX

@article{4fd4a9752347470c97900a1091ea4a5c,
title = "Thermodynamics of arsenates, selenites and sulphates in oxidising zone of sulphides ore deposits. VIII. Field of Thermal Stability of Synthetic Analog of Chalcomenite, its Dehydration and Dissociation",
abstract = "{\textcopyright} 2014, Pleiades Publishing, Ltd. The objective of this paper is to study the thermal stability of the synthetic analog of chalcomenite, CuSeO3 · 2H2O, and its dehydration and dissociation, in an experimental context. The study has been carried out by a comprehensive application of thermogravimetry (TG), differential scanning calorimetry (DSC), and high-temperature X-ray diffraction at a temperature range of 25–600°C. It has been established that CuSeO3 · 2H2O dehydrates at 202–264°C in three stages corresponding to the formation of intermediate CuSeO3 · 2H2O and CuSeO3 · 1/3H2O hydrate phases. At 480–595°C anhydrous CuSeO3 breaks down into CuO and SeO2 via the formation of a Cu4O(SeO3)3 phase. Enthalpies of the reactions at each stage of the CuSeO3 · 2H2O dehydration and CuSeO3 dissociation have been determined and their kinetic analysis has been carried out.",
author = "E.L. Fokina and E.V. Klimova and M.V. Charykova and V.G. Krivovichev and N.V. Platonova and V.V. Semenova and W. Depmeier",
year = "2014",
doi = "10.1134/S1075701514070058",
language = "English",
volume = "56",
pages = "538--545",
journal = "Geology of Ore Deposits",
issn = "1075-7015",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "7",

}

RIS

TY - JOUR

T1 - Thermodynamics of arsenates, selenites and sulphates in oxidising zone of sulphides ore deposits. VIII. Field of Thermal Stability of Synthetic Analog of Chalcomenite, its Dehydration and Dissociation

AU - Fokina, E.L.

AU - Klimova, E.V.

AU - Charykova, M.V.

AU - Krivovichev, V.G.

AU - Platonova, N.V.

AU - Semenova, V.V.

AU - Depmeier, W.

PY - 2014

Y1 - 2014

N2 - © 2014, Pleiades Publishing, Ltd. The objective of this paper is to study the thermal stability of the synthetic analog of chalcomenite, CuSeO3 · 2H2O, and its dehydration and dissociation, in an experimental context. The study has been carried out by a comprehensive application of thermogravimetry (TG), differential scanning calorimetry (DSC), and high-temperature X-ray diffraction at a temperature range of 25–600°C. It has been established that CuSeO3 · 2H2O dehydrates at 202–264°C in three stages corresponding to the formation of intermediate CuSeO3 · 2H2O and CuSeO3 · 1/3H2O hydrate phases. At 480–595°C anhydrous CuSeO3 breaks down into CuO and SeO2 via the formation of a Cu4O(SeO3)3 phase. Enthalpies of the reactions at each stage of the CuSeO3 · 2H2O dehydration and CuSeO3 dissociation have been determined and their kinetic analysis has been carried out.

AB - © 2014, Pleiades Publishing, Ltd. The objective of this paper is to study the thermal stability of the synthetic analog of chalcomenite, CuSeO3 · 2H2O, and its dehydration and dissociation, in an experimental context. The study has been carried out by a comprehensive application of thermogravimetry (TG), differential scanning calorimetry (DSC), and high-temperature X-ray diffraction at a temperature range of 25–600°C. It has been established that CuSeO3 · 2H2O dehydrates at 202–264°C in three stages corresponding to the formation of intermediate CuSeO3 · 2H2O and CuSeO3 · 1/3H2O hydrate phases. At 480–595°C anhydrous CuSeO3 breaks down into CuO and SeO2 via the formation of a Cu4O(SeO3)3 phase. Enthalpies of the reactions at each stage of the CuSeO3 · 2H2O dehydration and CuSeO3 dissociation have been determined and their kinetic analysis has been carried out.

U2 - 10.1134/S1075701514070058

DO - 10.1134/S1075701514070058

M3 - Article

VL - 56

SP - 538

EP - 545

JO - Geology of Ore Deposits

JF - Geology of Ore Deposits

SN - 1075-7015

IS - 7

ER -

ID: 5749559