Fiber optic internet cables could monitor earthquakes

A study provides new evidence that the same optical fibers that deliver high-speed internet and HD video to our homes could one day double as earthquake monitors.

“Fiber-optic cables are the backbone of modern telecommunications, and we have demonstrated that we can turn existing networks into extensive seismic arrays to assess ground motions during earthquakes,” says first author Zack Spica, an assistant professor in the earth and environmental sciences department at the University of Michigan.

Underground earthquake sensor system

Researchers conducted the study using a prototype array at Stanford University, where Spica was a postdoctoral fellow for several years.

“This is the first time that fiber-optic seismology has been used to derive a standard measure of subsurface properties that is used by earthquake engineers to anticipate the severity of shaking,” says coauthor Greg Beroza, professor in Stanford University’s School of Earth, Energy & Environmental Sciences.

To transform a fiber-optic cable into a seismic sensor, the researchers connect an instrument called a laser interrogator to one end of the cable. It shoots pulses of laser light down the fiber. The light bounces back when it encounters impurities along the fiber, creating a “backscatter signal” that is analyzed by a device called an interferometer.

Changes in the backscatter signal can reveal how the fiber stretches or compresses in response to passing disturbances, including seismic waves from earthquakes. The technique is called distributed acoustic sensing, or DAS, and has been used for years to monitor the health of pipelines and wells in the oil and gas industry.

The study extends previous work with the three-mile Stanford test loop by producing high-resolution maps of the shallow subsurface, which scientists can use to see which areas will undergo the strongest shaking in future earthquakes, Beroza says.

In addition, the study demonstrates that optical fibers can be used to sense seismic waves and obtain velocity models and resonance frequencies of the ground—two parameters that are essential for ground-motion prediction and seismic-hazard assessment. Spica and his colleagues say their results are in good agreement with an independent survey that used traditional techniques, thereby validating the methodology of fiber-optic seismology.

A good solution for big cities

This approach appears to have great potential for use in large, earthquake-threatened cities such as San Francisco, Los Angeles, Tokyo, and Mexico City, where thousands of miles of optical cables are buried beneath the surface.

“What’s great about using fiber for this is that cities already have it as part of their infrastructure, so all we have to do is tap into it,” Beroza says.

Many of these urban centers are built atop soft sediments that amplify and extend earthquake shaking. The near-surface geology can vary considerably from neighborhood to neighborhood, highlighting the need for detailed, site-specific information.

Yet getting that kind of information can be a challenge with traditional techniques, which involve the deployment of large seismometer arrays—thousands of such instruments in the Los Angeles area, for example.

“In urban areas, it is very difficult to find a place to install seismic stations because asphalt is everywhere,” Spica says. “In addition, many of these lands are private and not accessible, and you cannot always leave a seismic station standing alone because of the risk of theft.

“Fiber optics could someday mark the end of such large scale and expensive experiments. The cables are buried under the asphalt and crisscross the entire city, with none of the disadvantages of surface seismic stations.”

The technique would likely be fairly inexpensive, as well, Spica says. Typically, commercial fiber-optic cables contain unused fibers that can be leased for other purposes, including seismology.

For the moment, traditional seismometers provide better performance than prototype systems that use fiber-optic sensing. Also, seismometers sense ground movements in three directions, while optical fibers only sense along the direction of the fiber.

The next phase of the project involves a much larger test array. Scientists recently formed a 27-mile loop by linking optical fibers on Stanford’s historic campus with fibers at several other nearby locations.

The research appears in JGR Solid Earth. Additional coauthors are from Stanford, Universidad Nacional Autónoma de México, and Virginia Tech.

A collective effort from Stanford IT services, Stanford Geophysics, and OptaSense Ltd. made the three-mile Stanford fiber-optic array and data acquisition possible. Financial support for the work came from the Stanford Exploration Project, the US Department of Energy, and the Schlumberger Fellowship.

This news release includes information from Stanford University.

Source: University of Michigan

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