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Titlebook: Structural Chemistry of Silicates; Structure, Bonding, Friedrich Liebau Book 1985 Springer-Verlag Berlin Heidelberg 1985 ceramic.chemistry

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書(shū)目名稱(chēng)Structural Chemistry of Silicates
副標(biāo)題Structure, Bonding,
編輯Friedrich Liebau
視頻videohttp://file.papertrans.cn/880/879868/879868.mp4
圖書(shū)封面Titlebook: Structural Chemistry of Silicates; Structure, Bonding,  Friedrich Liebau Book 1985 Springer-Verlag Berlin Heidelberg 1985 ceramic.chemistry
描述As natural minerals, silica and silicates constitute by far the largest part of the earth‘s crust and mantle. They are equally important as raw materials and as mass produced items. For this reason they have been the subject of scientific research by geoscientists as well as by applied scientists in cement, ceramic, glass, and other industries. Moreover, intensive fun- damental research on silicates has been carried out for many years because silicates are, due to their enormous variability, ideally suited for the study of general chemical and crystallographic principles. Several excellent books on mineralogy and cement, ceramics, glass, etc. give brief, usually descriptive synopses of the structure of silicates, but do not contain detailed discussions of their structural chemistry. A number of monographs on special groups of silicates, such as the micas and clay min- erals, amphiboles, feldspars, and zeolites have been published which con- tain more crystal chemical information. However, no modern text has been published which is devoted to the structural chemistry of silicates as a whole. Within the last 2 decades experimental and theoretical methods have been so much improved to
出版日期Book 1985
關(guān)鍵詞ceramic; chemistry; crystal; formation; mineral; mineralogy
版次1
doihttps://doi.org/10.1007/978-3-642-50076-3
isbn_softcover978-3-642-50078-7
isbn_ebook978-3-642-50076-3
copyrightSpringer-Verlag Berlin Heidelberg 1985
The information of publication is updating

書(shū)目名稱(chēng)Structural Chemistry of Silicates影響因子(影響力)




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Introduction,long with the compounds in which silicon — oxygen groups constitute the anionic part of the phase (silicates) and compounds, such as SiP.O. in which silicon is considered to be the cationic part. Since all these compounds follow the same structural chemical rules they are summarized under the genera
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Crystal Chemical Classification of Silicates: Special Part,sophisticated. This is also true for the chemical formulae derived in Chap. 5 since they are based on the same classification system. The desired clearness and the undesirable complexity of the system are both a result of the attempt to include all conceivable silicate anions.
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Conclusion,carbon compounds, exhibit an enormous chemical and structural variability. In order to demonstrate this variability, a large number of silicates with different structures were described. Using these silicates as examples, it has been shown that the atomic structure of a silicate is controlled mainly
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