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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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發(fā)表于 2025-3-21 16:19:26 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Differential Thermal Analysis
副標(biāo)題Application and Resu
編輯Werner Smykatz-Kloss
視頻videohttp://file.papertrans.cn/279/278799/278799.mp4
叢書名稱Minerals, Rocks and Mountains
圖書封面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
關(guān)鍵詞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

書目名稱Differential Thermal Analysis影響因子(影響力)




書目名稱Differential Thermal Analysis影響因子(影響力)學(xué)科排名




書目名稱Differential Thermal Analysis網(wǎng)絡(luò)公開度




書目名稱Differential Thermal Analysis網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Differential Thermal Analysis被引頻次




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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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