DOI: 10.5110/jjseg.20.3
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Abstract: In this study, a test area is chosen in the region of the Ryoke granitic rocks, in Kawachinagano city, Osaka Pref., where rocks are weathered relatively uniformly and continuously to a considerable degree from the top to the depth. Core samples from there are examined by the various experiments. First of all, alternation of mineral particles is examined by X-Ray diffraction and ignition loss, and then, void ratio, specific surface area, and pore size distribution of core samples are determined. Moreover, the r… Show more

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