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Distributed Acoustic Sensing (DAS) of Strain at Earth Tide Frequencies: Laboratory Tests
The solid Earth strains in response to the gravitational pull from the Moon, Sun, and other planetary bodies. Measuring the flexure of geologic material in response to these Earth tides provides information about the geomechanical properties of rock and sediment. Such measurements are particularly useful for understanding dilation of faults and fractures in competent rock. A new approach to measuring earth tides using fiber optic distributed acoustic sensing (DAS) is presented here. DAS was originally designed to record acoustic vibration through the measurement of dynamic strain on a fiber optic cable. Here, laboratory experiments demonstrate that oscillating strain can be measured with DAS in the microHertz frequency range, corresponding to half-day (M2) lunar tidal cycles. Although the magnitude of strain measured in the laboratory is larger than what would be expected due to earth tides, a clear signal at half-day period was extracted from the data. With the increased signal-to-noise expected from quiet field applications and improvements to DAS using engineered fiber, earth tides could potentially be measured in deep boreholes with DAS. Because of the distributed nature of the sensor (0.25 m measurement interval over kilometers), fractures could be simultaneously located and evaluated. Such measurements would provide valuable information regarding the placement and stiffness of open fractures in bedrock. Characterization of bedrock fractures is an important goal for multiple subsurface operations such as petroleum extraction, geothermal energy recovery, and geologic carbon sequestration.
Complete Metadata
| @type | dcat:Dataset |
|---|---|
| accessLevel | public |
| bureauCode |
[
"019:20"
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| contactPoint |
{
"fn": "Matthew W Becker",
"@type": "vcard:Contact",
"hasEmail": "mailto:matt.becker@csulb.edu"
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| description | The solid Earth strains in response to the gravitational pull from the Moon, Sun, and other planetary bodies. Measuring the flexure of geologic material in response to these Earth tides provides information about the geomechanical properties of rock and sediment. Such measurements are particularly useful for understanding dilation of faults and fractures in competent rock. A new approach to measuring earth tides using fiber optic distributed acoustic sensing (DAS) is presented here. DAS was originally designed to record acoustic vibration through the measurement of dynamic strain on a fiber optic cable. Here, laboratory experiments demonstrate that oscillating strain can be measured with DAS in the microHertz frequency range, corresponding to half-day (M2) lunar tidal cycles. Although the magnitude of strain measured in the laboratory is larger than what would be expected due to earth tides, a clear signal at half-day period was extracted from the data. With the increased signal-to-noise expected from quiet field applications and improvements to DAS using engineered fiber, earth tides could potentially be measured in deep boreholes with DAS. Because of the distributed nature of the sensor (0.25 m measurement interval over kilometers), fractures could be simultaneously located and evaluated. Such measurements would provide valuable information regarding the placement and stiffness of open fractures in bedrock. Characterization of bedrock fractures is an important goal for multiple subsurface operations such as petroleum extraction, geothermal energy recovery, and geologic carbon sequestration. |
| distribution |
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{
"@type": "dcat:Distribution",
"title": "Distributed Acoustic Sensing of Strain at Earth Tide Frequencies Journal Sensors",
"format": "HTML",
"accessURL": "https://doi.org/10.3390/s19091975",
"mediaType": "text/html",
"description": "The data is based on this paper submitted into the Journal "Sensors" : "Distributed Acoustic Sensing of Strain at Earth Tide Frequencies" by Matthew W Becker and Thomas I Coleman, Vol. 19, 2019."
},
{
"@type": "dcat:Distribution",
"title": "Oscillating Strain Data using DAS.mat",
"format": "mat",
"accessURL": "https://gdr.openei.org/files/1129/CSULB_T13_EarthTide_earthtide_mean_360_519.mat",
"mediaType": "application/octet-stream",
"description": "These data are associated with the article published in the Journal "Sensors" : "Distributed Acoustic Sensing of Strain at Earth Tide Frequencies" by Matthew W Becker and Thomas I Coleman, Vol. 19, 2019.
Data are in matlab format and are the mean strain rate in nm/s over channels 360-519 as described in the article. "
}
]
|
| DOI | 10.15121/1512085 |
| identifier | https://data.openei.org/submissions/8444 |
| issued | 2018-01-24T07:00:00Z |
| keyword |
[
"DAS",
"EGS",
"Lab Tests",
"Matlab",
"characterization",
"distributed acoustic sensing",
"earth tide",
"energy",
"fiber optics sensors",
"fracture",
"geomechanics",
"geothermal",
"hydraulic",
"low frequency strain",
"measurement",
"stimulation strain"
]
|
| landingPage | https://gdr.openei.org/submissions/1129 |
| license | https://creativecommons.org/licenses/by/4.0/ |
| modified | 2025-07-07T16:48:24Z |
| programCode |
[
"019:006"
]
|
| projectLead | William Vandermeer |
| projectNumber | EE0006763 |
| projectTitle | Phase I Project: Fiber Optic Distributed Acoustic Sensing for Periodic Hydraulic Tests |
| publisher |
{
"name": "California State University",
"@type": "org:Organization"
}
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|
| title | Distributed Acoustic Sensing (DAS) of Strain at Earth Tide Frequencies: Laboratory Tests |
