| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 1696281 | Applied Clay Science | 2009 | 5 Pages |
Abstract
The dolomite is a double carbonate; it is a natural source of calcium and magnesium ions. In this study, Mg–Al–CO3 layered double hydroxide was synthesized from the dolomite by a simple method. The effect of synthesis parameters, such as M2+/Al3+ ratio, reaction temperature and pH on their structure, and textural properties were studied. The structure of materials was characterized by X-ray diffraction, Fourier transform infrared spectroscopy, thermogravimetric analysis (TGA) and Brunauer, Emmett, and Teller (BET) measurements.
Keywords
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Authors
Khaled Hosni, Ezzeddine Srasra,