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Titlebook: Differential Thermal Analysis; Application and Resu Werner Smykatz-Kloss Book 1974 Springer-Verlag Berlin · Heidelberg 1974 Differentialthe

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发表于 2025-3-21 16:19:26 | 显示全部楼层 |阅读模式
书目名称Differential Thermal Analysis
副标题Application and Resu
编辑Werner Smykatz-Kloss
视频videohttp://file.papertrans.cn/279/278799/278799.mp4
丛书名称Minerals, Rocks and Mountains
图书封面Titlebook: Differential Thermal Analysis; Application and Resu Werner Smykatz-Kloss Book 1974 Springer-Verlag Berlin · Heidelberg 1974 Differentialthe
描述At first glance it may seem presumptuous to want to add yet another to the numerous books on Differential Thermal Analysis (DT A). Thermoanalytical methods have been in use for some time, as shown by the more than five thousand publications containing DT A or TG curves listed by SMOTHERS and CHIANG in the bibliography to their handbook and abstracted in the several volumes of Thermal Analysis Abstracts (TAA), edited by J. P. REDFERN for the International Con­ federation for Thermal Analysis (ICT A). Every three years the proceed­ ings of ICT A meetings are published, bringing the latest results of thermoanalytic research. There is also the Scifax DT A Data Index, edited by R. C. MACKENZIE (1962) and modeled on the ASTM pattern card index (used for X-ray investigations), a compilation of the DT A data for several hundred minerals, and inorganic and organic materials. The theoretical foundations of thermogravimetry and DT A have been described in detail by LEHMANN, DAS and PAETSCH (1953), R. C. MACKENZIE (1957, 1970), DUVAL (1963), WENDLANDT (1964), GARN (1965), F. PAULIK et al. (1966), SMOTHERS and CHIANG (1966), and KEATTCH (1969). Thermoanalytical results are strongly influenced b
出版日期Book 1974
关键词Differentialthermoanalyse; Mineralogie; X-ray; atmosphere; classification; formation; mineral; mineralogy; r
版次1
doihttps://doi.org/10.1007/978-3-642-65951-5
isbn_softcover978-3-642-65953-9
isbn_ebook978-3-642-65951-5Series ISSN 0343-2181
issn_series 0343-2181
copyrightSpringer-Verlag Berlin · Heidelberg 1974
The information of publication is updating

书目名称Differential Thermal Analysis影响因子(影响力)




书目名称Differential Thermal Analysis影响因子(影响力)学科排名




书目名称Differential Thermal Analysis网络公开度




书目名称Differential Thermal Analysis网络公开度学科排名




书目名称Differential Thermal Analysis被引频次




书目名称Differential Thermal Analysis被引频次学科排名




书目名称Differential Thermal Analysis年度引用




书目名称Differential Thermal Analysis年度引用学科排名




书目名称Differential Thermal Analysis读者反馈




书目名称Differential Thermal Analysis读者反馈学科排名




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R. E. Maerker,B. L. Broadhead,M. L. Williamsrt substance should be at the same temperature during heating as long as there is no reaction in the sample. Such is the case with a small sample and an inert reference material that does not differ greatly from the sample chemically (e.g., with silicate samples, burnt kaolinite should be used as the inert substance).
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https://doi.org/10.1007/978-3-642-65951-5Differentialthermoanalyse; Mineralogie; X-ray; atmosphere; classification; formation; mineral; mineralogy; r
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Minerals, Rocks and Mountainshttp://image.papertrans.cn/d/image/278799.jpg
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Pressure Vessel Dosimetry at U.S. PWR Plantsl or other chemical substance during thermal treatment (heating or cooling), the weight and energy changes can be identified and measured very clearly. Weight loss which for example occurs during dehydration or loss of CO., SO. etc., can be determined with a thermobalance, recorded, and graphed vers
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R. E. Maerker,B. L. Broadhead,M. L. Williamsrt substance should be at the same temperature during heating as long as there is no reaction in the sample. Such is the case with a small sample and an inert reference material that does not differ greatly from the sample chemically (e.g., with silicate samples, burnt kaolinite should be used as th
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Identities Welcome and Unwelcome in College,ty of a mineral in the heated sample being responsible for this effect. ., . and . and . have compared the appearence and the temperature of dehydration reactions of unknown clay samples with those of well-known samples. So they received approximate data about the portions of clay minerals in these
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