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DOI10.1007/s11069-020-04007-7
Recent and historical tsunami deposits from Lake Tokotan, eastern Hokkaido, Japan, inferred from nondestructive, grain size, and radioactive cesium analyses
Shinozaki T.; Sawai Y.; Ito K.; Hara J.; Matsumoto D.; Tanigawa K.; Pilarczyk J.E.
发表日期2020
ISSN0921030X
起始页码713
结束页码730
卷号103期号:1
英文摘要Geological evidence of recent tsunamis from sediment samples collected from Lake Tokotan, a coastal lagoon in eastern Hokkaido, northern Japan, was detected using computed tomography (CT) and soft X-ray images, grain size, and radionuclide profiles. Initial field observations revealed that sediments had no discernable sedimentary structures at the top of the core. However, results of CT imaging, soft X-ray, and grain size analyses show evidence for three invisible sand layers that are intercalated with mud layers. These sand layers exhibit trends of landward fining and thinning. Furthermore, the distribution of sand layers was limited to the center and seaward parts of the lake. Vertical profiles of cesium and lead concentrations in combination with recent eyewitness accounts indicated that these sand layers are correlated with the 1973 Nemuro-oki, 1960 Chilean, and 1952 Tokachi-oki tsunami events. The deeper part of the sediment cores includes three volcanic ash layers and three prehistoric coarse sand layers. The prehistoric layers are correlated with unusually large tsunamis that were geologically identified in previous studies from eastern Hokkaido. These findings suggest that nondestructive techniques, in combination with radionuclide analysis, allow for detection of frequent but faint tsunami deposits. This technique allows for an improved understanding of the history of tsunami inundation in Lake Tokotan and of other locations for which stratigraphic evidence for faint tsunamis layers is not readily apparent from field assessments. © 2020, Springer Nature B.V.
关键词Computed tomographyHokkaidoRadioactive cesium and leadTsunami deposit
英文关键词cesium isotope; coastal lagoon; grain size; nondestructive testing; radionuclide; sand; sediment core; tsunami; Hokkaido; Japan
语种英语
来源期刊Natural Hazards
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/205936
作者单位Center for Research in Isotopes and Environmental Dynamics (CRiED), University of Tsukuba, Tennodai 1-1-1, Tsukuba, Ibaraki 305-8577, Japan; Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST), Higashi 1-1-1-C7, Tsukuba, Ibaraki 305-8567, Japan; Department of Earth Sciences, Centre for Natural Hazards Research, Simon Fraser University, 8888 University Dr., Burnaby, BC V5A 1S6, Canada; Division of Marine Science, School of Ocean Science and Technology, University of Southern Mississippi, 1020 Balch Blvd., Stennis Space Center, MS 39529-9904, United States
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Shinozaki T.,Sawai Y.,Ito K.,et al. Recent and historical tsunami deposits from Lake Tokotan, eastern Hokkaido, Japan, inferred from nondestructive, grain size, and radioactive cesium analyses[J],2020,103(1).
APA Shinozaki T..,Sawai Y..,Ito K..,Hara J..,Matsumoto D..,...&Pilarczyk J.E..(2020).Recent and historical tsunami deposits from Lake Tokotan, eastern Hokkaido, Japan, inferred from nondestructive, grain size, and radioactive cesium analyses.Natural Hazards,103(1).
MLA Shinozaki T.,et al."Recent and historical tsunami deposits from Lake Tokotan, eastern Hokkaido, Japan, inferred from nondestructive, grain size, and radioactive cesium analyses".Natural Hazards 103.1(2020).
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