Formation model of alluvial lowlands in Japan toward vulnerability evaluation
Project/Area Number |
23501238
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Research Category |
Grant-in-Aid for Scientific Research (C)
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Allocation Type | Multi-year Fund |
Section | 一般 |
Research Field |
Geography
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Research Institution | The University of Tokyo |
Principal Investigator |
SUGAI Toshihiko 東京大学, 新領域創成科学研究科, 教授 (90251321)
|
Project Period (FY) |
2011 – 2013
|
Project Status |
Completed (Fiscal Year 2013)
|
Budget Amount *help |
¥5,330,000 (Direct Cost: ¥4,100,000、Indirect Cost: ¥1,230,000)
Fiscal Year 2013: ¥1,170,000 (Direct Cost: ¥900,000、Indirect Cost: ¥270,000)
Fiscal Year 2012: ¥1,300,000 (Direct Cost: ¥1,000,000、Indirect Cost: ¥300,000)
Fiscal Year 2011: ¥2,860,000 (Direct Cost: ¥2,200,000、Indirect Cost: ¥660,000)
|
Keywords | 地形 / 沖積層 / 河川 / 災害脆弱性 / 海面変動 / 地殻変動 / 流域環境 / 第四紀 / 氷河性海水準変動 / コースタルプリズム / 河川縦断面形 / 関東平野 / 濃尾平野 / 沖積低地 / 地盤変動 / ボーリング / 活断層 / 津波 / 地震性沈降 / 縄文海進 / 古地震 / 河床縦断面形 / 地下地質 |
Research Abstract |
On the basis of East Japan great earthquake disaster, toward vulnerability evaluation of alluvial low land, the history of the alluvial plain formation and formation environment was elucidated from a global viewpoint. The alluvial bed of the downstream side of the main river of Japan makes a letter of prism generally, and the cross section is proportional with a basin area. In the northeastern Pacific offing earthquake in Japan, liquefaction might tend to be intense at the place where a prism deposited thick. The alluvial bed is formed by the interaction with the sea area through the glacial sea level change, a long-term crustal movement pattern, the combination of climate, flood properties and sediment supply changes of the river basin. A viewpoint of the mass transfer from the land with the order to the sea is indispensable for the regionality elucidation of alluvial plains for hundreds of thousands of years.
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Report
(4 results)
Research Products
(79 results)
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[Presentation] Late Quaternary Avulsion history of the lower Ili River, Central Eurasia controlled by climate and Balkhash lake level changes2013
Author(s)
Shimizu, H., Sugai, T., Kondo, R., Sato, A., Montani, H. Nakayama, Y. and Endo, K.
Organizer
Environment evolution session, IGU Kyoto Regional Conference
Place of Presentation
京都、京都国際会議場
Year and Date
2013-08-06
Related Report
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[Presentation] Last 600 ka terrestorial environment changes reconstructed from analysis of the Uwa Basin-fill Sediment, SW Japan2011
Author(s)
Sugai, T., Sasaki, Y., Ohno, Y., Nishizaki, N., Ikeda, M., Yanagida, M., Kojima, K. and Morita, Y.
Organizer
INQUA XVIIII Congress
Place of Presentation
スイス、ベルン
Year and Date
2011-07-26
Related Report
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[Presentation] Holocene climatic changes of the Balkhash lake region, Kazakhstan reconstructed from high-resolution XRF scanning analyses of the lake sediments coupled with geomorphic investigations of the catchment area2011
Author(s)
Sugai, T., Endo, K., Montani, H., Haraguti, T., Chiba, T., Shimizu, H., Sato, A., Nakayama, Y., Nakamura, A., Aubekerov, B., Sala, R., Jean M., Kubota, J.
Organizer
INQUA XVIIII Congress
Place of Presentation
スイス、ベルン
Year and Date
2011-07-26
Related Report
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[Presentation] Holocene environmental evolution based on Balkhash lake cores in Central Eurasia2011
Author(s)
Endo, K., Sugai, T., Haraguti, T., Suzuki, S., Matsuoka, H. and Nakao, Y.
Organizer
INQUA XVIIII Congress
Place of Presentation
スイス、ベルン
Year and Date
2011-07-26
Related Report
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