Journal of the Geothermal Research Society of Japan
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Volume 31 , Issue 1
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  • Hideaki HASE, Takeshi HASHIMOTO, Yasunori NISHIDA, Mitsuru UTSUGI, Hir ...
    Volume 31 (2009) Issue 1 Pages 27-37
    Released: February 26, 2010
    JOURNALS FREE ACCESS
    Usu volcano is located at southwestern part of Hokkaido, which is one of the most active volcanoes in Japan. We conducted self-potential (SP) surveys on the volcano, since July to December 2006. The compiled SP map reveals positive anomalies around Gin-numa crater and northwestern part of Ko-Usu, and a negative anomaly on the top of O-Usu lava dome on the summit caldera. The locations of the positive anomalies are corresponding to the fumarolric area, which are likely to be affected by hydrothermal system beneath the volcano. To confirm the consideration, we conducted numerical simulations of groundwater flow and SP of the electrokinetic origin within the volcano. The simulation results indicated the existences of, (a) hydrothermal upwelling driven by the intruded conduit beneath Usu-shinzan as a heat source, (b) a caprock layer at the upper margin of the hydrothermal and (c) low-resistivity channels from the upper margin of the hydrothermal area to the surface.
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Articles
  • Maki IKEGAMI, Junya MASUDA, Yoshihito KOMANIWA, Hiroshi ASANUMA, Hiroa ...
    Volume 31 (2009) Issue 1 Pages 39-50
    Released: February 26, 2010
    JOURNALS FREE ACCESS
    There are quite a few hot springs and spas in Japan, where people utilize hot spring water directly for bathing and waste it. Waste heat from baths in those spas could be reused for the other purposes. Cascade systems for utilizing waste heat for room heating and for hot water supply are studied in this paper, focusing on the economical and the environmental benefits.
    In this paper, a typical hot spring bath in Tohoku Area which has 60 [L/min] and 40 [°C] of hot spring waste water is assumed. We discuss cascade systems where the heat demand is the only room heating of bathroom and hot water supply to showers.
    A simulator with MATLAB Simulink was developed to analyze dynamic behavior of four options of the cascade systems; case 1 is a system in which waste heat is supplied to a heat pump first for room heating, and to a heat exchanger second for hot water supply to a water heater; case 2 is a system in which the order of the heat pump and the heat exchanger is reverse to the case 1; in case 3, waste heat is utilized only for the hot water supply through the heat exchanger; in case 4, waste heat is used only for the room heating by the heat pump system. A conventional fossil fuel system that does not utilize waste heat was also analyzed as case 5 for a reference case.
    The estimated heat demand for the hot water supply to showers is 6-15 times larger than that for the room heating. Hence, nearly 2/3 of the running costs and CO2 emission in the case 4 and 5 are cut in the cases 1-3 which has the heat exchange system to supply hot water. The payback time for the initial costs of the case 3 is the shortest and it is only 1-2 years. The utilization of waste heat for the demand for hot water supply to showers is generally the most efficient way to improve the economical and environmental benefits.
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  • Hiroaki OKUBO, Hikari FUJII, Ryuichi ITOI
    Volume 31 (2009) Issue 1 Pages 51-62
    Released: February 26, 2010
    JOURNALS FREE ACCESS
    Laboratory experiments of co-axial heat exchangers were carried out in a sand layer. The experiments were intended to investigate characteristics of heat exchange performance under various groundwater flow conditions. Results of laboratory experiments showed that heat exchange rates increase with the increase of groundwater velocity.
    A three-dimensional numerical model considering advection effect of groundwater flow was developed. The model was verified with the experiment results.
    Finally, the relationship between apparent thermal conductivity and groundwater velocity was estimated by the developed numerical model in a field scale. The relationship showed that the apparent thermal conductivity increases with the increase of groundwater velocity.
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