|
|
|
|||||||||||||||||
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |
Univ. Kiel, Inst. Anorg. Chem., Kiel, Federal Republic of Germany
Hydrous sodium silicate, synthesis from aqueous suspensions containing SiO 2 and NaOH with SiO 2 /NaOH ratios ranging from 5 to 20 and H 2 O/NaOH ratios from 50 to 500 at 100-150 degrees C. Transformation: magadiite --> kenyaite --> quartz. Formation of kenyaite at 100 degrees C requires several months; reaction times decreased at higher temperatures but quartz forms rapidly. Synthetic kenyaites form spherical aggregates of well-developed plates. Intracrystalline reactivity. Through exchange of protons for the interlayer sodium ions, kenyaite is transformed into a crystalline silicic acid.--Modified journal abstract.
This record provided courtesy of AGI/GeoRef.
This article has been cited by other articles:
![]() |
C. EYPERT-BLAISON, F. VILLIERAS, L. J. MICHOT, M. PELLETIER, B. HUMBERT, J. GHANBAJA, and J. YVON Surface heterogeneity of kanemite, magadiite and kenyaite: a high-resolution gas adsorption study Clay Minerals, September 1, 2002; 37(3): 531 - 542. [Abstract] [Full Text] [PDF] |
||||
![]() |
H. O. Pastore, H. O. Pastore, M. Munsignatti, and A. J.S. Mascarenhas ONE-STEP SYNTHESIS OF ALKYLTRIMETHYLAMMONIUM-INTERCALATED MAGADIITE Clays and Clay Minerals, April 1, 2000; 48(2): 224 - 229. [Abstract] [Full Text] [PDF] |
||||
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |