We carried out a gamma-ray spectra survey to discuss the relation between geothermal manifestations and gamma-ray intensities for three radioactive elements,
10K,
214Bi and
208Tl, in the Komatsu geothermal area, near Hatchoubaru geothermal power station in Oita prefecture, where a typical hydrothermal fractured type reservoir was developed. A data analysis method, based on Covell (1959) method, including the error estimation of observed data was used in this study Using detection limits of gamma-ray from each element, based on Currie (1966) method, was also proposed in this data processing. The results of field survey showed high gamma-ray intensity areas for Bi well correspond to high lm-depth temperature areas. This means that
222Ra, the parent element of Bi, comes up to the surface together with circulating thermal water. High intensity areas for Tl correspond to the locations of fumaroles distributed around high lm-depth temperature areas. This fact is interpreted that Tl is accumulated in places where the thermal water comes up to the surface rapidly, because
222Rn, the parent element of Tl, has a very short half-life. We can conclude the high gamma-ray intensities of Bi and Tl to be potential indicators for the existence of upflows of thermal water.
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