First application of scintillator-based photon-counting computed tomography to rock samples: Preliminary results and prospects

Author:

Ishiguro Ayumi1,Arimoto Makoto1234,Sato Daichi1,Tomoda Takahiro1,Itano Keita5,Tamura Akihiro3,Sugiyama Hironori6,Kawae Takeshi3,Fukuyama Mayuko5,Kataoka Jun4,Terazawa Shinsuke7,Shiota Satoshi7,Morishita Tomoaki38

Affiliation:

1. Graduate School of Natural Science & Technology, Kanazawa University, Kakuma, Kanazawa, Ishikawa 920-1192, Japan

2. Advanced Research Center for Space Science and Technology, Kanazawa University, Kakuma, Kanazawa, Ishikawa 920-1192, Japan

3. Institute of Science and Engineering, Kanazawa University, Kakuma, Kanazawa, Ishikawa 920-1192, Japan

4. Faculty of Science and Engineering, Waseda University, 3-4-1, Okubo, Shinjuku, Tokyo 169-8555, Japan

5. Graduate School of Engineering Science, Akita University, 1-1 Tegata-gakuen-machi, Akita 010-8502, Japan

6. Instrumental Analysis Division, Engineering and Technology Department, Kanazawa University, Kakuma, Kanazawa, Ishikawa 920-1192, Japan

7. Proterial Ltd, 2-15-17 Egawa, Shimamoto, Mishima, Osaka 618-0013, Japan

8. Volcanoes and Earth’s Interior Research Center, Japan Agency for Marine-Earth Science and Technology, 2-15 Natsushima, Kanagawa 237-0061, Japan

Abstract

Abstract Knowledge of the three-dimensional distribution of minerals in a rock sample is of fundamental importance to deciphering a sample’s properties and history. Attenuation-contrast X-ray computed tomography (X-ray CT) is widely used in the geosciences to determine the three-dimensional distributions of minerals or pores, or both. Photon counting CT (PC-CT) uses a novel energy-resolved X-ray detector that allows X-rays with a continuous energy spectrum to be detected separately within arbitrary energy ranges. Here we report the first results of applying laboratory-build PC-CT combined with multi-pixel photon counter (MPPC) to common minerals such as quartz and calcite. In the low-energy range, PC-CT produced higher contrast images than single-energy X-ray CT. Minerals were successfully identified from the relationships between the mean CT values for each energy window and the mean difference between pairs of energy windows. These results suggest that PC-CT can produce high-contrast images of minerals and may be able to distinguish mineral phases with different attenuation curves, even when their CT values are similar. We obtained CT images of minerals in a natural sedimentary rock sample, composed mainly of quartz and carbonate. Although the spatial resolution of the detector in this study was insufficient for the sample, the main carbonate veins were clearly visible as high carbonate-content areas in the PC-CT images. Given some prior knowledge of mineral phases from other methods, it may be possible to use PC-CT imaging to obtain further information about their chemical compositions.

Publisher

Mineralogical Society of America

Reference32 articles.

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5. An introduction to the application of X-ray microtomography to the three-dimensional study of igneous rocks;Baker;Lithos,2012

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