Self-potential measurement and experimental study related with thermal process of volcano
| Project/Area Number |
05640461
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| Research Category |
Grant-in-Aid for General Scientific Research (C)
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| Allocation Type | Single-year Grants |
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| Research Field |
固体地球物理学
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| Research Institution | Hokkaido University |
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Principal Investigator |
NISHIDA Yasunori Fac.Sci., Hokkaido Univ., Prof., 理学部, 教授 (60000874)
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| Co-Investigator(Kenkyū-buntansha) |
OSHIMA Hiromitsu Fac.Sci., Hokkaido Univ., Instructor, 理学部, 助手 (10213703)
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| Project Period (FY) |
1993 – 1994
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| Project Status |
Completed (Fiscal Year 1994)
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| Budget Amount *help |
¥1,800,000 (Direct Cost: ¥1,800,000)
Fiscal Year 1994: ¥800,000 (Direct Cost: ¥800,000)
Fiscal Year 1993: ¥1,000,000 (Direct Cost: ¥1,000,000)
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| Keywords | self-potential / active volcano / hydrothermal circulation / electro-kinetic effect / electro-kinetic coupling coefficient / 火山 / 界面導電効果 / ζ-電位 / マグマの冷却 |
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| Research Abstract |
1.Self-potential (SP) surveys were conducted on six active volcanoes : Usu-san, Hokkaido Komage-take, Miyake-jima, Tarumae-san, Me-akan-dake and Esan. Large and positive SP anomalies, in both spatial extent (1-2 km) and magnitude (several hundred mV), were observed on the high ground temperature zones of the former for volcanoes. The anomalies are mainly caused by electro-kinetic effect due to the upwellingof the hot ground water triggered by the remnant magma situated at the shallow depth. On the other hand, no significant SP anomaly was observed on the latter two volcanoes, suggesting the hydrothermal circulation of large size has not developed within the edifices. Considering the hot volcanic gas had ejected from the summit crater, it is speculated that the volcanic activity of the both volcanoes is vapor-dominated : vapor cannot transport the electric charge.
2.In order to quantify the SP anomalies in volcanic regions, the field experiment for measuring the in-situ value of the electrokinetic coupling coefficient was made at Atosanupuri-Kawayu district at where the underground hydrological model, such as the flow pass, the amound of flow and so on, has been established. The estimated value was well correlated with the results of the laboratory experiments by other scientists.
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Report
(3 results)
Research Products
(4 results)
