Strain Meters
The Gravity Group also uses fiber optic instruments to build strain meters in boreholes and on the seafloor. Following are some examples of our work in geodesy.
Strain in an ice sheet borehole -- Siple Dome Antarctica
One example of applying fiber optics to strain problems is our development of A Time-of-Flight Fiber Optic Borehole Strain Sensor in Antarctica.
Borehole optical fiber strainmeter -- Long Vall ey exploratory well
We have deployed an optical fiber strainmeter similar to the one
used at Siple Dome to monitor strain in the Long Valley exploratory
well near Mammoth Mountain, California. It is located over the resurgent
dome in the Long Valley Caldera, a site of current volcanic unrest
with great societal relevance due to a high potential for an eruptive
event.
Seafloor strainmeter (see FOSS)
We developed an optical fiber strainmeter intended for measuring
tectonic strains on the seafloor. In this instrument, an optical
fiber is stretched between two points fixed to the ocean bottom;
relative displacement of these points causes a change in the elongation
of the fiber. This associated change in optical path length is monitored
by an electronic distance meter. The dominant sources of noise in
determining the optical path length of the fiber stem from the dependence
of the fiber's index of refraction on both wavelength and temperature.
In a 50 day long experiment performed in the shallow ocean, a test
fiber was installed along a 210 m long baseline on the bottom. The
RMS variation in length was 5 mm except for two displacements of
order 10 cm caused by known effects.
People
Mark Zumberge
John Blum
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