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| 02154nam 2200325za 4500 |
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001 | 9.840754 |
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003 | CaOODSP |
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005 | 20221107151924 |
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007 | cr ||||||||||| |
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008 | 170731s1970 oncd ob f000 0 eng d |
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040 | |aCaOODSP|beng |
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043 | |an-cn--- |
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086 | 1 |aM38-8/93E-PDF|zM38-8/93 |
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245 | 04|aThe mechanism of the formation of lead hexaferrite |h[electronic resource] / |cW.S. Bowman ... [et al.]. |
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260 | |aOttawa : |bQueen's Printer, |c1970. |
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300 | |a8 p. : |bcharts |
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490 | 1 |aReprint series ; |vRS 93 |
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500 | |aCover title. |
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500 | |a"Mineral Sciences Division." |
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500 | |a"Reprinted from the Journal of the Canadian Ceramic Society, (1969), vol. 38, pp. 1-8." |
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500 | |aHistorical publication digitized from print 2017 [by Natural Resources Canada]. |
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504 | |aIncludes bibliographical references. |
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520 | 3 |a"Studies of the mechanism of the formation of lead hexaferrite from its constituent oxides have been conducted. The reactions were studied by differential thermal analysis, thermogravimetric analysis, X-ray diffraction procedures and by magnetic susceptibility measurements. It was found that the nature of the intermediate product(s) was dependent upon the technique of mixing, and the time and temperature of heating. There is an indication that there may be considerable variations in the temperature dependence of the various possible intermediate reactions. A kinetic model describing the behaviour of the system is postulated. The intermediate compounds observed were 2PbO.Fe2O3 and PbO.2Fe2O3. The latter can be distinguished from the structurally-similar PbO.6Fe2O3 by the use of magnetic susceptibility measurements"--Abstract, p. 1. |
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692 | 07|2gccst|aCeramics |
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700 | 1 |aBowman, W. S. |
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710 | 1 |aCanada. |bNatural Resources Canada. |
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710 | 1 |aCanada. |bDepartment of Energy, Mines and Resources. |
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710 | 1 |aCanada. |bMines Branch. |
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830 | #0|aReprint series - Dept. of Energy, Mines and Resources, Mines Branch ;|vRS 93|w(CaOODSP)9.834843 |
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856 | 40|qPDF|s1.75 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M38-8/M38-8-93-eng.pdf |
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