Cation Exchange Properties of Micas
- 9 July 1970
- journal article
- Published by Mineralogical Society in Clay Minerals
- Vol. 8 (3) , 273-278
- https://doi.org/10.1180/claymin.1970.008.3.05
Abstract
Two phlogopites depleted of potassium by extraction with sodium tetraphenyl boron released resorbed potassium more readily than the original micas, but the large difference in the exchange parameters of the two micas were paralleled by those of their potassium-saturated alteration products. The apparent basal spacings of the potassium-saturated alteration products were about 0·03Å larger than those of the corresponding untreated micas; their broader lines indicate structural irregularities.Keywords
This publication has 9 references indexed in Scilit:
- Cation Exchange Properties of MicasClay Minerals, 1970
- CATION EXCHANGE PROPERTIES OF MICASEuropean Journal of Soil Science, 1969
- Debris from the Sixth Chinese Nuclear TestNature, 1969
- Structural Charge Site Influence on the Interlayer Hydration of Expandable Three-Sheet Clay MineralsClays and Clay Minerals, 1968
- Changes in phlogopites during their artificial alterationClay Minerals, 1967
- Interstratification in Vermiculite and Biotite Produced by Potassium Sorption: I. Evaluation by Simple X-ray Diffraction Pattern InspectionSoil Science Society of America Journal, 1967
- Visible Changes in Macro Mica Particles That Occur with Potassium DepletionClays and Clay Minerals, 1967
- Rate of Potassium Release from Fixed and Native FormsSoil Science Society of America Journal, 1959
- CATION EXCHANGE IN MICACEOUS MINERALSSoil Science, 1954