Japan Geoscience Union Meeting 2015

Presentation information

Oral

Symbol S (Solid Earth Sciences) » S-VC Volcanology

[S-VC49] Hydrothermal systems of volcanoes

Mon. May 25, 2015 2:15 PM - 4:00 PM 102B (1F)

Convener:*Yasuhiro Fujimitsu(Department of Earth Resources Engineering, Faculty of Engineering, Kyushu University), Tsuneomi Kagiyama(Graduate School of Science, Kyoto University), Takeshi Ohba(Department of chemistry, School of Science, Tokia University), Chair:Yasuhiro Fujimitsu(Department of Earth Resources Engineering, Faculty of Engineering, Kyushu University), Shogo Komori(National Institute of Advanced Industrial Science and Technology)

3:45 PM - 4:00 PM

[SVC49-07] Numerical modeling for a broad geothermal system of Kuju Volcano

*Yasuhiro FUJIMITSU1, Yohei ITO2, Jun NISHIJIMA1, Daisuke OKA3 (1.Faculty of Engineering, Kyushu University, 2.Graduate School of Engineering, Kyushu University, 3.Geological Survey of Hokkaido, Hokkaido Research Organization)

Keywords:Kuju Volcano, broad geothermal system, hydrothermal system, numerical model

The Kuju volcanic field is located in the southwestern part of Oita prefecture, Japan, and consists of some andesitic volcanoes. There are many hot springs and several geothermal power stations (Hatchobaru, Otake, Takigami etc.) in this field. In the previous studies on the Kuju volcanic field, the numerical models were mainly for the power station areas or the center of Kuju Volcano where fumarolic activity appears. Therefore, we constructed a new conceptual model that includes the center of the volcano and all of the geothermal power station areas in order to attempting to construct an integrative numerical model of a broad geothermal system that has the scale of the volcanic field to explain the existence of the hydrothermal systems, which are generated by a heat source like a magma chamber in the volcanic field. Based on this conceptual model, we constructed a numerical model that replicates the hydrothermal systems of the geothermal power station areas roughly although the numerical model is relatively simple.