論文

査読有り
2004年10月

A 100 m laser strainmeter system installed in a 1 km deep tunnel at Kamioka, Gifu, Japan

JOURNAL OF GEODYNAMICS
  • S Takemoto
  • ,
  • A Araya
  • ,
  • J Akamatsu
  • ,
  • W Morii
  • ,
  • H Momose
  • ,
  • M Ohashi
  • ,
  • Kawasaki, I
  • ,
  • T Higashi
  • ,
  • Y Fukuda
  • ,
  • S Miyoki
  • ,
  • T Uchiyama
  • ,
  • D Tatsumi
  • ,
  • H Hanada
  • ,
  • Naito, I
  • ,
  • S Telada
  • ,
  • N Ichikawa
  • ,
  • K Onoue
  • ,
  • Y Wada

38
3-5
開始ページ
477
終了ページ
488
記述言語
英語
掲載種別
研究論文(学術雑誌)
DOI
10.1016/j.jog.2004.07.008
出版者・発行元
PERGAMON-ELSEVIER SCIENCE LTD

We have installed a laser strainmeter system in a deep tunnel about 1,000 m below the ground surface at Kamioka, Gifu, Japan. The system consists of three types of independent interferometers: (1) an EW linear strainmeter of the Michelson type with unequal arms, (2) an NS-EW differential strainmeter of the Michelson type with equal arms and (3) a NS absolute strainmeter of the Fabry-Perot type. These are configured in L-shaped vacuum pipes, each of which has a length of 100 m. (1) and (2) are highly sensitive (order of 10(-13) strain) and have wide dynamical range (10(-13) - 10(-6)). Observations with strainmeters (1) and (2) started on June 11, 2003. (3) is a new device for absolute-length measurements of the order of 10(-9) of a long-baseline (100 m) Fabry-Perot cavity by the use of phase-modulated light. This third strainmeter will be ready for operation before the end of 2004. The laser source of strainmeters (1) and (2) is a frequency-doubled YAG laser with a wavelength of 532 nm. The laser frequency is locked onto an iodine absorption line and a stability of 2 x 10(-13) is attained. The light paths of the laser strainmeter system are enclosed in SUS304 stainless steel pipes. The inside pressure is kept to be 10(-4) Pa. Consequently, quantitative measurement of crustal strains of the order of 10(-13) can be attained by employing the laser strainmeter system of (1) and (2) at Kamioka. This resolving power corresponds to that of a superconducting gravimeter. Using the laser strainmeter system, we expect to determine parameters related to fluid core resonance, core modes and core undertone as well as other geodynamic signals such as slow strain changes caused by silent earthquakes or slow earthquakes. (C) 2004 Elsevier Ltd. All rights reserved.

Web of Science ® 被引用回数 : 30

リンク情報
DOI
https://doi.org/10.1016/j.jog.2004.07.008
Web of Science
https://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=JSTA_CEL&SrcApp=J_Gate_JST&DestLinkType=FullRecord&KeyUT=WOS:000225869300018&DestApp=WOS_CPL
ID情報
  • DOI : 10.1016/j.jog.2004.07.008
  • ISSN : 0264-3707
  • Web of Science ID : WOS:000225869300018

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