By Leo Brewer (auth.), John L. Margrave (eds.)
It is a smart excitement to have the ability to honor our unusual colleague, Professor Leo Brewer, at the celebration of his sixty-fifth delivery day, with this detailed quantity of hot temperature technology. Leo and his spouse, Rose, are own buddies of numerous generations of scholars and postdoctoral researchers on the collage of California at Berkeley. Their hindrance and realizing has been vital to many folks during the last 40 years. each one paper during this quantity has no less than one writer who was once a gradu ate pupil or a postdoctoral researcher in Leo's laboratory at Berkeley. the diversity of themes is indicative of the wide-ranging technological know-how performed by way of Brewer-ites and by way of Leo Brewer himself. He has in my view participated within the solution of some of the classical difficulties of high-temperature science-from the warmth of sublimation of graphite to the dissociation en ergy of nitrogen to the prediction of binary and ternary part diagrams. He and his scholars have made significant contributions to atomic and molec ular spectroscopy. He has made major contributions to the boost ment of effective structures for strength conversion and to ceramics. In addi tion to his examine actions, Leo Brewer has been a long-time player within the dynamic undergraduate educating application of the Berkeley Chemistry division. He has supplied the most important perception for stu dents enthusiastic about these career-shaping stories that one endures whereas buying the fundamentals of inorganic, natural, and actual chemistry with that interwoven universal bond of thermodynamics.
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Extra resources for Modern High Temperature Science: A Collection of Research Papers from Scientists, Post-Doctoral Associates, and Colleagues of Professor Leo Brewer in celebration of his 65th birthday
Under these conditions, it appeared of interest critically to assess the literature results for the molecules FeO(g) and MnO(g). In so doing, the original data were first systematically recalculated with the same thermodynamic functions as those used in this work. For the flame spectrophotometric measurements, the incidence of interfering species was next taken into account. D8(FeO) In flame photometric measurements (4, 5), Dg(FeO) was previously calculated by setting the FeO(g) concentration equal to the difference between the known total iron concentration and that of free Fe(g), calculated from atomic line intensities.
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