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  4. Laboratory-scale strain and temperature response of a distributed optical fiber sensor

Laboratory-scale strain and temperature response of a distributed optical fiber sensor

Author(s)
Madjdabadi, B.
Valley, Benoît  
Laboratoire de géothermie et géomécanique des réservoirs  
Siczkar, L.
Dusseault, M.B.
Kaiser, P.K.
Publisher
American Rock Mechanics Association
Date issued
June 23, 2013
In
ARMA
Vol
347
From page
264
To page
271
Subjects
DOFS Smart Profile DiTeSt Spatial resolution Brillouin frequency strain
Abstract
Distributed optical fiber sensors (DOFSs), used initially in structural health monitoring for high-rise buildings and bridges, are attracting attention in the field of underground structures, including mining. Designed for long-term study of deformations, DOFSs are more efficient when installed away from excavation damaged zone (EDZ) in a borehole filled with a grout mixture to measure elastic strain field responses to excavations. The DOFS sensing cable, as a component of a complex compliance system, i.e. rockmass and grout, is being assessed through laboratory work.
A test program is underway to observe DOFS response to various perturbations including strain and joint displacement. Initially, tests on unstrained sensors are performed in order to assess measurement repeatability and noise-to-signal ratio at both local and global scales. Then, the various lengths of the cable, from 1 m down to 1 cm, will be stretched up to 0.5% strain. In other tests, the same lengths of the cable will be exposed to shear displacement, such as might occur in the vicinity of a joint or fault that experiences shear.
The results from these tests will answer uncertainties and questions regarding the scaling factor between straining sections over a full sampling window, i.e. spatial resolution, and a partial sampling window, i.e. validity of calibration factors provided by the supplier, and assessing effects of coating and plastic protective layers of the sensor. Issues such as shear deformation responses of cable and bending direction of the cable are being evaluated.

Initial results on unstrained cable to assess measurement repeatability showed variability in length assessment between successive readings. This variability particularly impacts the data interpretation from the strain sensors since these sensors present locally large Brillouin frequency gradients which results in locally large variability in differential readings. Our detailed experimental results will be presented in the paper.
Notes
Paper presented at the 47th U.S. Rock Mechanics/Geomechanics Symposium, San Francisco, California, June 2013
Event name
Rock Mechanics/Geomechanics Symposium
Location
San Francisco, CA, USA
Publication type
conference paper
Identifiers
https://libra.unine.ch/handle/20.500.14713/21534
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2022-03-18_110_7648.pdf

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