Hostname: page-component-586b7cd67f-dlnhk Total loading time: 0 Render date: 2024-11-30T16:50:08.746Z Has data issue: false hasContentIssue false
  • English
  • Français

X-ray identification of randomly interstratified illite-smectite in mixtures with discrete illite

Published online by Cambridge University Press:  09 July 2018

Jan Środoń
Jan Środoń*
Affiliation:
Polish Academy of Sciences, Institute of Geology, 31-002 Kraków, Senacka 3, Poland
Get access Rights & Permissions [Opens in a new window]

Abstract

Proportions of the component layers in randomly interstratified illite-smectites can be determined precisely in the presence of discrete illite if two reflections (at 15–16 and 31–32°2θ Cu Kα) are strong enough to be measured accurately. The method takes into account the variable thickness of the smectite-ethylene glycol complex and involves a correction for the interference from illite reflections.

Résumé

Résumé

Les proportions des feuillets composant une illite/smectite interstratifiée au hasard, peuvent être déterminées avec précision en présence d'illite pure si deux réflexions sont suffisamment fortes pour qu'elles puissent être mesurées avec précision (à 15-16 et 31-32°20 CuKα). La méthode tient compte de l'épaisseur variable du complexe smectite-éthylène glycol et utilise une correction de l'interférence due aux réflexions de l'illite.

Kurzreferat

Kurzreferat

Die Anteile der Schichtkomponenten von unregelmäßig wechselgelagerten Illit-Smectiten lassen sich in Gegenwart von Illit genau bestimmen, wenn zwei Reflexe (bei 15-16 und 31-32°20,CuKα) deutlich genug sind, um genau gemessen werden zu können. Die Methode berücksichtigt die variable Dicke des Smectit-Ethylenglycol-Komplexes und beinhaltet eine Korrektur für die Interferenzen von Illitreflexen.

Resumen

Resumen

La proporción de los diferentes componentes de un mineral interestratificado al azar ilita-esmectita puede ser determinada exactamente en presencia de cantidades discretas de ilita si dos reflexiones (a 15-16 y 31-32°20CuKα) son lo suficientemente fuertes para ser medidas exactamente. El método se basa en el espesor variable del complejo esmectia-etilenglicol e incluye una correción por la interferencia de las reflexiones de la ilita.

Type
Research Article
Information
Clay Minerals , Volume 16 , Issue 3 , September 1981 , pp. 297 - 304
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1981

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Eslinger, E.V. & Savin, S.M. (1976) Init. Reports on the Deep Sea Drilling Project XXXV, 489. U.S. Government Printing Office, Washington.Google Scholar
Frey, E. & Lagaly, G. (1979) Proc. Int. Clay Conf. Oxford, 131.Google Scholar
Hoffman, J.Ch. (1979) PhD thesis, Case Western Reserve Univ., Cleveland Ohio, USA.Google Scholar
Hoffman, J. & Hower, J. (1979) Spec. PubL Soc. econ. Paleont. Mineral., Tulsa 26.Google Scholar
Hower, J., Eslinger, E.V., Hower, M.E. & Perry, E.A. (1976) Bull. geol. Soc. Am. 87, 725.Google Scholar
Jackson, M.L. (1974) Soil Chemical Analysis—Advanced Course. Publ. by the Author, Madison, Wisconsin.Google Scholar
Lagaly, G. (1981) Clay Miner. 16, 1.Google Scholar
Parachoniak, W. & Środoń, J. (1973) Mineralogia Polonica 4, 37.Google Scholar
Perry, E.A. & Hower, J. (1970) Clays Clay Miner. 18, 165.Google Scholar
Reynolds, R.C. & Hower J., (1970) Clays Clay Miner. 18, 25.Google Scholar
Robertson, H.E., Weir, A.H. & Woods, R.D. (1968) Clays Clay Miner. 16, 239.Google Scholar
Schultz, L.G. (1978) Prof. Pap. U.S. geol. Surv. 1064-A.Google Scholar
Shutov, V.D., Drits, V.A. & Sakharov, B.A. (1969) Proc. Int. Clay Conf. Tokyo 1, 523.Google Scholar
Środoń, J. (1976) Prace Miner. 49, 7.Google Scholar
Środoń, J. (1980) Clays Clay Miner. 28, 401.Google Scholar
Środoń, J & Eberl, D.D. (1980) Clay Miner. 15, 317.Google Scholar