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Survey result of airborne electromagnetic survey in the Hachimantai Sumikawa landslide area; Hachimantai Sumikawa jisuberi ni okeru kuchu denjiho chosa kekka

Abstract

For the study of a landslide that occurred at Hachimantai Sumikawa, Akita Prefecture, an airborne electromagnetic survey is conducted for the examination of the relationship between the spot of landslide and solfataric clay (bluish gray clay). The location is a cap block type structure with a Neogene green tuff overlain by accumulated lava flow, where hot water is very active. The system used in this study is capable of measurement across a very wide frequency range, and measurements are made simultaneously at five frequencies of 220Hz, 1100Hz, 5500Hz, 27,500Hz, and 137,500Hz, these frequencies meaning depth levels 5m-70m explored. It is found that the spot of landslide matches a region where resistivity is so low as to be not higher than 10ohm/m. It is also found, in the resistivity cross section analysis for the middle part of the spot of landslide, that the mass of soil that moved on the upper part of the spot is relatively high in resistivity while the part below the slide surface is low in resistivity. There is agreement between the results reported above and the results of on-site investigations. 4 refs., 6 figs.
Authors:
Konishi, N; Nakamura, N; Miyamoto, T [1] 
  1. Nippon Engineering Consultant Co. Ltd., Tokyo (Japan)
Publication Date:
Oct 22, 1997
Product Type:
Conference
Report Number:
ETDE/JP-98751022; CONF-9710214-
Reference Number:
SCA: 440700; 580000; PA: JP-97:0G4554; EDB-98:075723; SN: 98001944490
Resource Relation:
Conference: 97. SEGJ conference, Butsuri tansa gakkai dai 97 kai (1997 nendo shuki) gakujutsu koenkai, Sapporo (Japan), 22-24 Oct 1997; Other Information: PBD: 22 Oct 1997; Related Information: Is Part Of Proceeding of the 97th (Fall, Fiscal 1997) SEGJ Conference; PB: 371 p.; Butsuri tansa gakkai dai 97 kai (1997 nendo shuki) gakujutsu koenkai koen ronbunshu
Subject:
44 INSTRUMENTATION, INCLUDING NUCLEAR AND PARTICLE DETECTORS; 58 GEOSCIENCES; ELECTROMAGNETIC SURVEYS; AERIAL SURVEYING; LANDSLIDES; MEASURING INSTRUMENTS; HOT SPRINGS; CLAYS; FREQUENCY RANGE; ELECTRIC CONDUCTIVITY; TERTIARY PERIOD; TUFF; VOLCANIC ROCKS
OSTI ID:
622723
Research Organizations:
Society of Exploration Geophysicists of Japan, Tokyo (Japan)
Country of Origin:
Japan
Language:
Japanese
Other Identifying Numbers:
Other: ON: DE98751022; TRN: JN97G4554
Availability:
Available from Society of Exploration Geophysicists of Japan, 2-18, Nakamagome 2-chome, Ota-ku, Tokyo, (Japan); OSTI as DE98751022
Submitting Site:
NEDO
Size:
pp. 188-192
Announcement Date:
Jul 24, 1998

Citation Formats

Konishi, N, Nakamura, N, and Miyamoto, T. Survey result of airborne electromagnetic survey in the Hachimantai Sumikawa landslide area; Hachimantai Sumikawa jisuberi ni okeru kuchu denjiho chosa kekka. Japan: N. p., 1997. Web.
Konishi, N, Nakamura, N, & Miyamoto, T. Survey result of airborne electromagnetic survey in the Hachimantai Sumikawa landslide area; Hachimantai Sumikawa jisuberi ni okeru kuchu denjiho chosa kekka. Japan.
Konishi, N, Nakamura, N, and Miyamoto, T. 1997. "Survey result of airborne electromagnetic survey in the Hachimantai Sumikawa landslide area; Hachimantai Sumikawa jisuberi ni okeru kuchu denjiho chosa kekka." Japan.
@misc{etde_622723,
title = {Survey result of airborne electromagnetic survey in the Hachimantai Sumikawa landslide area; Hachimantai Sumikawa jisuberi ni okeru kuchu denjiho chosa kekka}
author = {Konishi, N, Nakamura, N, and Miyamoto, T}
abstractNote = {For the study of a landslide that occurred at Hachimantai Sumikawa, Akita Prefecture, an airborne electromagnetic survey is conducted for the examination of the relationship between the spot of landslide and solfataric clay (bluish gray clay). The location is a cap block type structure with a Neogene green tuff overlain by accumulated lava flow, where hot water is very active. The system used in this study is capable of measurement across a very wide frequency range, and measurements are made simultaneously at five frequencies of 220Hz, 1100Hz, 5500Hz, 27,500Hz, and 137,500Hz, these frequencies meaning depth levels 5m-70m explored. It is found that the spot of landslide matches a region where resistivity is so low as to be not higher than 10ohm/m. It is also found, in the resistivity cross section analysis for the middle part of the spot of landslide, that the mass of soil that moved on the upper part of the spot is relatively high in resistivity while the part below the slide surface is low in resistivity. There is agreement between the results reported above and the results of on-site investigations. 4 refs., 6 figs.}
place = {Japan}
year = {1997}
month = {Oct}
}