Time-of-flight neutron diffraction studies of clay-fluid interactions under basin conditions

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doi: 10.1180/000985500546657
Authors:Skipper, N. T.; Williams, G. D.; de Siqueira, A. V. C.; Lobban, C.; Soper, A. K.
Author Affiliations:Primary:
University College London, Department of Physics and Astronomy, London, United Kingdom
Other:
Rutherford Appleton Laboratory, United Kingdom
Volume Title:Mineral diagenesis and reservoir quality, the way forward
Volume Authors:Bain, D. C., editor; Hall, P. L.; Shaw, H. F.; Spears, D. A.
Source:Clay Minerals, 35(1), p.283-290; Sixth Cambridge conference on Mineral diagenesis and reservoir quality, the way forward, Cambridge, United Kingdom, March 26-27, 1998, edited by D. C. Bain, P. L. Hall, H. F. Shaw and D. A. Spears. Publisher: Mineralogical Society, London, United Kingdom. ISSN: 0009-8558
Publication Date:2000
Note:In English. 21 refs.; illus.
Summary:Neutron diffraction experiments can provide an extremely high-resolution structural picture of clay-fluid systems. Here we describe the application of time-of-flight neutron scattering to hydrated clays, including discussion of issues such as isotopic labelling, sample containment, and data analysis. Recent studies of hydrated vermiculites under ambient conditions are used as an example. We then describe a new high-pressure/high-temperature sample environment that is being used to study clay-fluid interactions, in situ under hydrostatic sedimentary basin conditions. This environment enables us to approximate conditions encountered during burial, at depths of up to 10 km.
Sections:Clay minerals
Subsections:Petrology; weathering; soils
Subjects:Chemical analysis; Chemical properties; Clay mineralogy; Clay minerals; Experimental studies; Geochemistry; Methods; Mineral-water interface; Neutron diffraction analysis; Sheet silicates; Silicates; Vermiculite
Abstract Numbers:01M/131
Record ID:2000057300
Copyright Information:GeoRef, Copyright 2019 American Geosciences Institute.
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