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Geochemical evaluation of geothermal resources in Toyama Prefecture, Japan, based on the chemical and isotopic characteristics of hot spring waters

机译:日本富山县地热资源的地球化学评价,基于热泉水化学和同位素特征

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摘要

The chemical compositions, including hydrogen and oxygen isotopes, of 35 hot spring waters in Toyama Pre-fecture, central Japan, were analyzed to examine their geochemical characteristics and geothermal resources. The hot spring water samples were classified into two groups: low and high chloride (Cl-) concentrations of less than and greater than 2000 mg/L, respectively. The samples in the low-salinity group were determined to be of meteoric origin and Ca2+-HCO3- type. The samples in the high-salinity group were determined to be of Na+-Ca2+-Cl- type and assumed to contain a mixture of fossil seawater and meteoric water. In the eastern area of the study region, the Na+/K+ and SiO2 concentrations were lower and higher, respectively, than those in other areas, which corresponded to high-temperature geothermal resources. Thus, the subsurface information obtained in this study enabled effective use of the low to medium geothermal resources in Toyama Prefecture.
机译:分析了日本中部富山富山富山上的35个温泉水的化学成分,包括氢和氧同位素,以检查其地球化学特征和地热资源。将热弹簧水样品分为两组:低于和大于2000mg / L的低氯化物(CL-)浓度。将低盐分基团中的样品测定为陨石来源和Ca2 + -HCO3型。测定高盐度基团中的样品是Na + -Ca2 + -Cl型,并假设含有化石海水和陨石的混合物。在研究区的东部地区,纳+ / k +和SiO2浓度分别比其它区域的浓度分别较低,更高,该区域对应于高温地热资源。因此,在该研究中获得的地下信息使得能够有效地利用富山县的低至中等地热资源。

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