X-ray powder diffraction" /> Il-mo Kang" /> Il-mo Kang, Suck-Chan Park, Hi-Soo Moon and Jang-Han Yoo
" /> Il-mo Kang, Suck-Chan Park, Hi-Soo Moon and Jang-Han Yoo. Econ. Environ. Geol. 2003;36:1-8. https://doi.org/">Econ. Environ. Geol. 2003; 36(1): 1-8
Published online February 28, 2003
© THE KOREAN SOCIETY OF ECONOMIC AND ENVIRONMENTAL GEOLOGY
Study on expandability and X-ray coherent scattering domain size of bentonite from Gampo and Yonil area, Korea
Il-mo Kang1*, Suck-Chan Park1, Hi-Soo Moon1 and Jang-Han Yoo2
1Department of Earth System Sciences, Yonsei University, 134, Sinchon-dong, Seodaemunku, Seoul, 120-749, Korea
2Korea Institute of Geoscience and mineral Resources, Gajeong-dong 30, Daejeon, 305-350, Korea
Correspondence to : Il-mo Kang
This study was performed to measure expandabilities and scattering domain sizes (CSDs) of bentonite samples from Gampo and Yonil area, Korea, using X-ray powder diffraction (XRD), and to compare their experimental data with those of international standard bentonite samples (SAz-1, STx-1, and SWy-2). Most of Gampo and Yonil bentonite samples comprised randomly interstratified illite-smectite (R0 I-S), and their expandabilities ranged over 77-100%Sxrd from the saddle/001 method. The interstratification deformed 001 peaks of EG-solved samples (M?ring's first principle), which prohibited us from adopting these peaks to measure CSDs using BWA (Ber-taut-Warren-Averbach) method. CSDs of the bentonite samples with R0 I-S could be measured though Dehydration at 300?C after K-saturation,where the deformation originated from the interstratification could be removed effectively. Gampo and Yonil bentonite samples showed that their mean CSDs ranged over 3.8-5.4 interlayers, and that their CSDs distributions were similar to those of Gonzales(STx-1) and Wyoming (SWy-2) bentonite samples.
Keywords
X-ray powder diffraction, bentonite, expandability, coherent scattering domain size, illite-smectite.
Econ. Environ. Geol. 2003; 36(1): 1-8
Published online February 28, 2003
Copyright © THE KOREAN SOCIETY OF ECONOMIC AND ENVIRONMENTAL GEOLOGY.
Study on expandability and X-ray coherent scattering domain size of bentonite from Gampo and Yonil area, Korea
Il-mo Kang1*, Suck-Chan Park1, Hi-Soo Moon1 and Jang-Han Yoo2
1Department of Earth System Sciences, Yonsei University, 134, Sinchon-dong, Seodaemunku, Seoul, 120-749, Korea
2Korea Institute of Geoscience and mineral Resources, Gajeong-dong 30, Daejeon, 305-350, Korea
Correspondence to:
Il-mo Kang
This study was performed to measure expandabilities and scattering domain sizes (CSDs) of bentonite samples from Gampo and Yonil area, Korea, using X-ray powder diffraction (XRD), and to compare their experimental data with those of international standard bentonite samples (SAz-1, STx-1, and SWy-2). Most of Gampo and Yonil bentonite samples comprised randomly interstratified illite-smectite (R0 I-S), and their expandabilities ranged over 77-100%Sxrd from the saddle/001 method. The interstratification deformed 001 peaks of EG-solved samples (M?ring's first principle), which prohibited us from adopting these peaks to measure CSDs using BWA (Ber-taut-Warren-Averbach) method. CSDs of the bentonite samples with R0 I-S could be measured though Dehydration at 300?C after K-saturation,where the deformation originated from the interstratification could be removed effectively. Gampo and Yonil bentonite samples showed that their mean CSDs ranged over 3.8-5.4 interlayers, and that their CSDs distributions were similar to those of Gonzales(STx-1) and Wyoming (SWy-2) bentonite samples.
Keywords
X-ray powder diffraction, bentonite, expandability, coherent scattering domain size, illite-smectite.
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