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Biggar, G. M., O'Hara, M. J. (1969) Temperature control and calibration in quench furnaces and some new temperature measurements in the system CaO–MgO–Al2O3–SiO2. Mineralogical Magazine, 37 (285) 1-15 doi:10.1180/minmag.1969.037.285.01

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Reference TypeJournal (article/letter/editorial)
TitleTemperature control and calibration in quench furnaces and some new temperature measurements in the system CaO–MgO–Al2O3–SiO2
JournalMineralogical Magazine
AuthorsBiggar, G. M.Author
O'Hara, M. J.Author
Year1969 (March)Volume37
Issue285
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_37/37-285-1.pdf+
DOIdoi:10.1180/minmag.1969.037.285.01Search in ResearchGate
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Mindat Ref. ID6228Long-form Identifiermindat:1:5:6228:6
GUID0
Full ReferenceBiggar, G. M., O'Hara, M. J. (1969) Temperature control and calibration in quench furnaces and some new temperature measurements in the system CaO–MgO–Al2O3–SiO2. Mineralogical Magazine, 37 (285) 1-15 doi:10.1180/minmag.1969.037.285.01
Plain TextBiggar, G. M., O'Hara, M. J. (1969) Temperature control and calibration in quench furnaces and some new temperature measurements in the system CaO–MgO–Al2O3–SiO2. Mineralogical Magazine, 37 (285) 1-15 doi:10.1180/minmag.1969.037.285.01
In(1969, March) Mineralogical Magazine Vol. 37 (285) Mineralogical Society
Abstract/NotesSummaryTechniques associated with temperature control and measurement in quench furnaces are described and a study made of calibration problems. Systematic temperature errors as great as 30°C in published results from separate laboratories are explicable. A comprehensive redetermination of temperatures of invariant equilibria in systems containing CaO, MgO, Al2O3, SiO2, Na2O, Fe-O2, has been initiated and the results to date are presented, including approximate determinations of three invariant equilibria in the system CaO-MgO-Al2O3-SiO2 involving liquid, monticellite, spinel, and two of merwinite, periclase, and forsterite, which are important in the melting of magnesia refractories, and precise determinations of the three newly recognized invariant equilibria involving liquid, spinel, diopside, and two of forsterite, melilite, and anorthite.


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