| Project/Area Number |
12480113
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| Research Category |
Grant-in-Aid for Scientific Research (B)
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| Allocation Type | Single-year Grants |
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| Section | 一般 |
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| Research Field |
Natural disaster science
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| Research Institution | Kagoshima University |
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Principal Investigator |
IWAMATSU Akira Kagoshima University, Faculty of Science, Professor, 理学部, 教授 (80018663)
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| Co-Investigator(Kenkyū-buntansha) |
YOKOTA Syuichiro Shimane University, Faculty of Science and Engineering, Professor, 総合理工学部, 教授 (60211653)
IMURA Ryusuke Kagoshima University, Faculty of Science, Associate Professor, 理学部, 助教授 (40284864)
KITAMURA Ryosuke Kagoshima University, Faculty of Engineering, Professor, 工学部, 教授 (70111979)
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| Project Period (FY) |
2000 – 2001
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| Project Status |
Completed (Fiscal Year 2001)
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| Budget Amount *help |
¥12,000,000 (Direct Cost: ¥12,000,000)
Fiscal Year 2001: ¥2,000,000 (Direct Cost: ¥2,000,000)
Fiscal Year 2000: ¥10,000,000 (Direct Cost: ¥10,000,000)
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| Keywords | Shirasu hazard / volcanic glass / hydration / refractive index / weathering |
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| Research Abstract |
Shirasu is a general name for unwelded rhyolitic pyroclastic flow deposit in southern Kyushu, Japan. Shirasu steep slopes are sometimes collapsed during eavy rains. To clarify the weathering process of Shirasu slope surface would be important to predict the collapse of Shirasu. We examined degree of hydration of volcanic glass shards using the refractive index in the order of deterioration of Shirasu slope. At study outcrop, the Shirasu slope surface composed of original pyroclastic flow deposit (layer I), talus deposits and overlying fallout tephra. Talus deposits are subdivided into three layers (layer II to IV in ascending order) by the facies and color. The refractive index of volcanic glass shards (layer I to IV) ranges from 1.4960 to 1.5000. Layer II to IV tend to show high index (1.4978 - 1.4982). On the other hand, layer I have a significantly low index (1.4976) than those of the former layers. Refractive index of dehydrated samples from each layer are 0.002-0.001 lower than those of hydrated glass. There are many incompletely hydrated thick glass shards in layer I. On the other hand, layer II to IV are mainly composed of completely hydrated volcanic glass. We may say that the refractive index of volcanic glass shards is an indicator of the degree of deteriorated Shirasu slope surface.
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