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Coherent Optical Time Domain Reflectometry aka Optical Fiber Distributed Acoustic Sensing PDF

19 Pages·2015·29.98 MB·English
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Preview Coherent Optical Time Domain Reflectometry aka Optical Fiber Distributed Acoustic Sensing

Coherent  Optical  Time   Domain  Reflectometry            a.k.a.   Optical  Fiber  Distributed   Acoustic  Sensing Mark  Zumberge Scripps  Institution  of  Oceanography Phase mode: Two Pulse Rayleigh “Virtual Interferometer” à true strain measurement 10 m between pulse centers defines spatial resolution = Gauge length, L Two Pulses f1 f2 “Mirror 1” “Mirror 2” 10 µs delay for 1km phase I (amp) Rect cos Δf amplitude sin Q Polar phase strain, εL Range gate f1 -f2 = Δf optical carrier Demodulated Phase • Linear, • Quantitative • High dynamic range Courtesy  of  OptaSense,  a  Qinetiq  company Summary Logistically  inexpensive  means  to  deploy  a     permanent  seismic  array:  just  an  armored  cable   on  seafloor Electronics:  a  box  w/  laser,  photo-­‐‑detector     aPached  to  OOI  cable  for  power  and  data  and   to  a  passive  optical  fiber  cable Creates  permanent  seismic  array  w/  hundreds     of  stations Low  cost,  long  lifetime,  useful  for  4D  seismic     studies Gravity  Observations  to   Investigate  Volcano  Structure   and  Its  Evolution Mark  Zumberge Glenn  Sasagawa Jeff  Ridgway Gerald  D’Spain Scripps  Institution  of  Oceanography Time  lapse   gravity ROV  deployable  gravity  meters   Observations  of  CO  sequestration     2 Precision  of  a  few  µμGal   Potential  for  detection  of  magma     body  inflation Scintrex  CG5s  in  gimbal  frames •  Shock mounted frame •  Underway tilt control Shock mounts •  On-deck cold bath

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a ached to OOI cable for power and data and to a passive optical fiber cable. Creates permanent seismic array w/ hundreds of stations. Low cost, long lifetime, useful for 4D seismic studies. Summary. Page 7. Mark Zumberge. Glenn Sasagawa. Jeff Ridgway. Gerald D'Spain. Scripps Institution of
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