Development of a laboratory monitoring system for elastic waves transmitted through sand under dry and nearly saturated conditions

Abstract Laboratory experiments with seismic measurements have the potential to be highly useful for understanding the physical process of water-induced landslides, and fundamental experiments are helpful for the appropriate interpretation of recorded seismograms. We developed a laboratory measureme...

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Main Authors: Masayuki Nakayama, Hironori Kawakata, Shiro Hirano, Issei Doi
Format: Article
Language:English
Published: SpringerOpen 2021-01-01
Series:Earth, Planets and Space
Subjects:
Online Access:https://doi.org/10.1186/s40623-020-01346-4
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spelling doaj-457e4b155f064ad08e7588ae9c59c8302021-01-24T12:43:20ZengSpringerOpenEarth, Planets and Space1880-59812021-01-0173111210.1186/s40623-020-01346-4Development of a laboratory monitoring system for elastic waves transmitted through sand under dry and nearly saturated conditionsMasayuki Nakayama0Hironori Kawakata1Shiro Hirano2Issei Doi3Graduate School of Science and Engineering, Ritsumeikan UniversityCollege of Science and Engineering, Ritsumeikan UniversityCollege of Science and Engineering, Ritsumeikan UniversityDisaster Prevention Research Institute, Kyoto UniversityAbstract Laboratory experiments with seismic measurements have the potential to be highly useful for understanding the physical process of water-induced landslides, and fundamental experiments are helpful for the appropriate interpretation of recorded seismograms. We developed a laboratory measurement system to investigate the relationships between wave propagation and water saturation in sand. We considered that the wavelength should be comparable to or sufficiently shorter than the sensing intervals. Furthermore, we embedded a wave source that can repeatedly emit an arbitrary and identical signal in an octave frequency band under both dry and nearly saturated conditions. We measured the transmitted waves by embedded accelerometers over 24 h under dry and nearly saturated conditions. The difference in the slowness between the two conditions was one-thousand-fold larger than the fluctuations in slowness over 24 h for each condition. Also, the difference in amplitude between the two conditions was about double the fluctuations in amplitude over 24 h for each condition. These results suggested that our system can monitor the water content change in sand via the change in spectral amplitude and phase slowness.https://doi.org/10.1186/s40623-020-01346-4Wave propagationSandFluid saturationGeohazardLaboratory experimentsPorous materials
collection DOAJ
language English
format Article
sources DOAJ
author Masayuki Nakayama
Hironori Kawakata
Shiro Hirano
Issei Doi
spellingShingle Masayuki Nakayama
Hironori Kawakata
Shiro Hirano
Issei Doi
Development of a laboratory monitoring system for elastic waves transmitted through sand under dry and nearly saturated conditions
Earth, Planets and Space
Wave propagation
Sand
Fluid saturation
Geohazard
Laboratory experiments
Porous materials
author_facet Masayuki Nakayama
Hironori Kawakata
Shiro Hirano
Issei Doi
author_sort Masayuki Nakayama
title Development of a laboratory monitoring system for elastic waves transmitted through sand under dry and nearly saturated conditions
title_short Development of a laboratory monitoring system for elastic waves transmitted through sand under dry and nearly saturated conditions
title_full Development of a laboratory monitoring system for elastic waves transmitted through sand under dry and nearly saturated conditions
title_fullStr Development of a laboratory monitoring system for elastic waves transmitted through sand under dry and nearly saturated conditions
title_full_unstemmed Development of a laboratory monitoring system for elastic waves transmitted through sand under dry and nearly saturated conditions
title_sort development of a laboratory monitoring system for elastic waves transmitted through sand under dry and nearly saturated conditions
publisher SpringerOpen
series Earth, Planets and Space
issn 1880-5981
publishDate 2021-01-01
description Abstract Laboratory experiments with seismic measurements have the potential to be highly useful for understanding the physical process of water-induced landslides, and fundamental experiments are helpful for the appropriate interpretation of recorded seismograms. We developed a laboratory measurement system to investigate the relationships between wave propagation and water saturation in sand. We considered that the wavelength should be comparable to or sufficiently shorter than the sensing intervals. Furthermore, we embedded a wave source that can repeatedly emit an arbitrary and identical signal in an octave frequency band under both dry and nearly saturated conditions. We measured the transmitted waves by embedded accelerometers over 24 h under dry and nearly saturated conditions. The difference in the slowness between the two conditions was one-thousand-fold larger than the fluctuations in slowness over 24 h for each condition. Also, the difference in amplitude between the two conditions was about double the fluctuations in amplitude over 24 h for each condition. These results suggested that our system can monitor the water content change in sand via the change in spectral amplitude and phase slowness.
topic Wave propagation
Sand
Fluid saturation
Geohazard
Laboratory experiments
Porous materials
url https://doi.org/10.1186/s40623-020-01346-4
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