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Merck
CN

220736

Sigma-Aldrich

弗洛里西®

100-200 mesh

别名:

活性硅酸镁, 硅酸镁

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关于此项目

经验公式(希尔记法):
MgO3Si
化学文摘社编号:
分子量:
100.39
EC 号:
MDL编号:
UNSPSC代码:
12352200
PubChem化学物质编号:
NACRES:
SB.52
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表单

powder

质量水平

技术

gas chromatography (GC): suitable

粒径

100-200 mesh

转变温度

transition temp 650 °C (activation temperature)

SMILES字符串

[Mg++].[O-][Si]([O-])=O

InChI

1S/Mg.O3Si/c;1-4(2)3/q+2;-2

InChI key

FKHIFSZMMVMEQY-UHFFFAOYSA-N

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应用

活化的硅酸镁,可用作气相色谱中的吸附剂。

法律信息

Florisil is a registered trademark of U.S. Silica Company

储存分类代码

13 - Non Combustible Solids

WGK

nwg

闪点(°F)

Not applicable

闪点(°C)

Not applicable


历史批次信息供参考:

分析证书(COA)

Lot/Batch Number

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Separation of lipid classes by chromatography on florisil.
Carroll KK.
Journal of Lipid Research, 2(2), 135-141 (1961)
E Gefen et al.
Comparative biochemistry and physiology. Part A, Molecular & integrative physiology, 182, 58-63 (2014-12-17)
Scorpions exhibit some of the lowest recorded water loss rates among terrestrial arthropods. Evaporative water loss to the surrounding environment occurs mainly through the integument, and thus its resistance to water loss has paramount significance for the ability of scorpions
Iyad Rashid et al.
International journal of pharmaceutics, 411(1-2), 18-26 (2011-03-23)
A directly compressible excipient has been developed by co-processing starch with magnesium silicate. The foregoing was achieved either by co-precipitation of magnesium silicate onto different types of starch or by dry granulation of maize starch with magnesium silicate. A variety
Iyad Rashid et al.
Journal of pharmaceutical sciences, 98(12), 4887-4901 (2009-08-20)
When chitin is used in pharmaceutical formulations, processing of chitin with metal silicates is advantageous, from both an industrial and pharmaceutical perspective, compared to processing using silicon dioxide. Unlike the use of acidic and basic reagents for the industrial preparation
Li Zhang et al.
Proceedings of the National Academy of Sciences of the United States of America, 110(16), 6292-6295 (2013-04-12)
Knowledge of the structural properties of mantle phases is critical for understanding the enigmatic seismic features observed in the Earth's lower mantle down to the core-mantle boundary. However, our knowledge of lower mantle phase equilibria at high pressure (P) and

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