Jane M. Hammarstrom E-an Zen 1975 <p>In an effort to evaluate the method of quantitative analysis by X-ray diffraction as a means of determining dawsonite abundances in Green River" oil shale, we performed a series of grinding experiments. Weighed mixtures of dawsonite + quartz and dawsonite + quartz + shale were ground for preset lengths of time, and the following X-ray diffraction peaks were measured for intensity: dawsonite (110) at 15.6 2<span>θ</span> and (211) (002) at 32.1° 2<span>θ</span>, and quartz (100) at 20.9° 2<span>θ</span> and (101) at 26.6° 2<span>θ</span>. Heights and areas were measured. Intensity ratios were plotted as functions of grinding time with a calculated probable error. Intensity ratios generally decrease as grinding time increases. The intensity of the 15.6° peak, D_15.6°, is most affected, and the most drastic reduction occurs during the first 20 min of grinding. The D_32.1° peak is least sensitive to grinding but is subject to interference by other minerals in the shale. We conclude that the X-ray diffraction method is not well adapted to the routine quantitative determination of dawsonite in oil shale of the Green River Formation. </p> application/pdf en U.S. Geological Survey Quantitative determination of dawsonite in Green River Shale by powder-sample X-ray diffraction; effect of grinding article