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Milodowski, A. E., Goodman, B. A., Morgan, D. J. (1989) Mösbauer spectroscopic study of the decomposition mechanism of ankerite in CO2 atmosphere. Mineralogical Magazine, 53 (372) 465-471 doi:10.1180/minmag.1989.053.372.06

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Reference TypeJournal (article/letter/editorial)
TitleMösbauer spectroscopic study of the decomposition mechanism of ankerite in CO2 atmosphere
JournalMineralogical MagazineISSN0026-461X
AuthorsMilodowski, A. E.Author
Goodman, B. A.Author
Morgan, D. J.Author
Year1989 (September)Volume53
Issue372
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_53/53-372-465.pdf+
DOIdoi:10.1180/minmag.1989.053.372.06Search in ResearchGate
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Mindat Ref. ID1531Long-form Identifiermindat:1:5:1531:2
GUID0
Full ReferenceMilodowski, A. E., Goodman, B. A., Morgan, D. J. (1989) Mösbauer spectroscopic study of the decomposition mechanism of ankerite in CO2 atmosphere. Mineralogical Magazine, 53 (372) 465-471 doi:10.1180/minmag.1989.053.372.06
Plain TextMilodowski, A. E., Goodman, B. A., Morgan, D. J. (1989) Mösbauer spectroscopic study of the decomposition mechanism of ankerite in CO2 atmosphere. Mineralogical Magazine, 53 (372) 465-471 doi:10.1180/minmag.1989.053.372.06
In(1989, September) Mineralogical Magazine Vol. 53 (372) Mineralogical Society
Abstract/NotesAbstractMössbauer spectroscopy has been used to identify the iron-containing products that are formed during the thermal decomposition of ankerite in a CO2 atmosphere. The decomposition takes place in three stages and evidence is produced to show that the first stage involves decomposition of ankerite to yield a periclase-wustite solid solution, (Mg,Fe)O, along with calcite and CO2, the periclase-wustite then reacting with CO2 to produce magnesioferrite (MgFe2O4) and CO. In the second stage the magnesioferrite and calcite react to produce periclase and dicalcium ferrite. The third stage does not involve reaction of Fe-containing phases and corresponds to the decomposition of calcite to CaO.

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Milodowski, A.E., Morgan, D.J., Warne, S.St.J. (1989) Thermal analysis studies of the dolomite-ferroan dolomite-ankerite series. II. decomposition mechanism in flowing CO2 atmosphere. Thermochimica Acta, 152. 279-297 doi:10.1016/0040-6031(89)85398-5
Richardson, S., Vaughan, D. J. (1989) Arsenopyrite: a spectroscopic investigation of altered surfaces. Mineralogical Magazine, 53 (370) 223-229 doi:10.1180/minmag.1989.053.370.09
Dasgupta, D. R. (1967) Thermal decomposition of dolomite and ankerite. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (277) 138-141 doi:10.1180/minmag.1967.036.277.22
Charnock, J. M., Garner, C. D., Pattrick, R. A. D., Vaughan, D. J. (1989) EXAFS and Mössbauer spectroscopic study of Febearing tetrahedrites. Mineralogical Magazine, 53 (370) 193-199 doi:10.1180/minmag.1989.053.370.06
Vaughan, D. J. (1989) Spectroscopic Studies of Minerals: Principles, Applications and Advances. Mineralogical Magazine, 53 (370) 133 doi:10.1180/minmag.1989.053.370.01
Bayliss, Peter, Freeman, Kim J. (1989) Mineral nomenclature: fernandinite. Mineralogical Magazine, 53 (372) 511 doi:10.1180/minmag.1989.053.372.12
Taylor, D. (1989) Thermal decomposition of Li8(Al6Si6O24)Cl2. Mineralogical Magazine, 53 (371) 380-382 doi:10.1180/minmag.1989.053.371.15
Carpenter, M. A., Salje, E. (1989) Time-dependent Landau theory for order/disorder processes in minerals. Mineralogical Magazine, 53 (372) 483-504 doi:10.1180/minmag.1989.053.372.09
Tlili, A., Smith, D. C., Beny, J.-M., Boyer, H. (1989) A Raman microprobe study of natural micas. Mineralogical Magazine, 53 (370) 165-179 doi:10.1180/minmag.1989.053.370.04
Goodman, B. A., Wilson, M. J. (1973) A study of the weathering of a biotite using the Mössbauer effect. Mineralogical Magazine, 39 (304) 448-454 doi:10.1180/minmag.1973.039.304.07
Richardson, S., Vaughan, D. J. (1989) Surface alteration of pentlandite and spectroscopic evidence for secondary violarite formation. Mineralogical Magazine, 53 (370) 213-222 doi:10.1180/minmag.1989.053.370.08
 
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