Fast phase analysis of mineral powders

X-ray diffraction (XRD) is an effective method for determination of the phase composition of unknown crystalline and amorphous materials. The analysis is performed by comparing diffraction peak positions and intensity values with the reference patterns of known compounds maintained in the ICDD Powder Diffraction File (PDF). Routine characterization is completed quickly with a minimum of operator involvement. Subsequent analyses, including quantitative analysis of identified phases, are easily accomplished. The goal of this work is to quickly identify the major phases in a series of unknown mineral powders using the MiniFlex. Data reduction and Search/Match analysis was performed using the JADE software package. Bulk samples were ground into fine powders using a mortar and pestle. Specimens were prepared from the samples by smearing on glass slides coated with a thin layer of Vaseline. No special effort was made to control the preferred orientation in the grains. Standard θ/2θ data were collected using the MiniFlex diffractometer.

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Figure 1: Analysis of a pure mineral. The top hit is for this sample is Heazlewoodite, a nickel sulfide mineral.

The MiniFlex was able to identify the major phases of the minerals with little sample preparation and a short analysis time. The total time for the first two scans presented was 10 minutes. Increased analysis time will significantly increase the signal to noise ratio and will thus improve the detection limits of minor phases.

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Figure 2: The upper scan is identified as albite. The lower scan has the same albite peaks, as well as a number of peaks from a second phase, identified as microcline.

Data set 3 was acquired in a longer period of times, since the peaks were not as intense as in the other samples. The data presented has been smoothed and background corrected. The stick patterns from the PDF file of the best search/match results are printed below each scan. "Good" Search/Match results match both the position and intensity of peaks. In a good match, there will be no unidentified peaks. Since many compounds have similar crystal structures, S/M results will list several "good" matches. Additional information about the sample may be needed to definitively identify a phase.

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Figure 3: A multiphase sample. This sample was run more slowly than the others to get higher intensity, which makes it easier to effectively identify many of the peaks. Major phases include quartz, halite, clinochlore and either illite or muscovite.

The Rigaku MiniFlex benchtop X-ray diffractometer, combined with the Jade analytical software package, is an effective tool for phase identification of unknown mineral samples. Clear interpretation of the presence of absence of various phases can be performed quickly and with a high degree of confidence. Phase identification is easily performed, even on quick data collection scans with high statistical noise. Specimen preparation for most standard materials is minimal since chunk materials as well as powder samples can be analyzed.


The fifth generation MiniFlex is a general purpose X-ray diffractometer that can perform qualitative and quantitative analysis of polycrystalline materials. The MiniFlex is available in two variations. Operating at 600 watts (X-ray tube), the MiniFlex 600 is twice as powerful as other benchtop models, enabling faster analysis and improved overall throughput. Running at 300 watts (X-ray tube), the new MiniFlex 300 does not require an external heat exchanger. Each model is engineered to maximize flexibility in a benchtop package. Read more...

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