Abstract
The compression behavior of a silicate-rich oil shale from the Green River formation in the pressure range 0.0-2.4 GPa was studied using in situ high pressure X-ray pair distribution function (PDF) measurements for the sample contained within a Paris-Edinburgh cell. The real-space local structural information in the PDF, G(r), was used to evaluate the compressibility of the oil shale. Specifically, the pressure-induced reduction in the medium- to long-range atom distances (∼6-20 Å) yielded an average sample compressibility corresponding to a bulk modulus of ca. 61-67 GPa. A structural model consisting of a three phase mixture of the principal crystalline oil shale components (quartz, albite and Illite) provided a good fit to the ambient pressure PDF data (R ∼ 30.7%). Indeed the features in the PDF beyond ∼6 Å, were similarly well fit by a single phase model of the highest symmetry, highly crystalline quartz component. The factors influencing the observed compression behavior are discussed.
| Original language | English |
|---|---|
| Pages (from-to) | 9980-9982 |
| Number of pages | 3 |
| Journal | Journal of Physical Chemistry C |
| Volume | 112 |
| Issue number | 27 |
| DOIs | |
| State | Published - Jul 10 2008 |
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