Abstract

Microseismic monitoring is of importance for several geoscience research aspects and for applications in oil and gas industry. For signals generated by the ultra-weak microseismic events, conventional moving-coil geophone systems have reached their limit in detection sensitivity especially at high frequency range. Here we for the first time present a specially tailored fiber-optic sensing system targeting at downhole microseismic monitoring. The system contains 30 individual interferometric accelerometers and 2 reference sensors, which are time-division multiplexed into a 12-level vector seismic sensor array. The multiplexed accelerometers can achieve ~50 ng/ $\sqrt {\mathrm{Hz}} $ noise equivalent acceleration, which is superior to the commercial available moving-coil geophone systems at frequencies above 200 Hz. The measured sensitivity of the accelerometers can reach ~200 rad/g from 10 Hz to 1 kHz. The dynamic range is above 134 dB over the same frequency range and is higher than its electronic counterpart in the low frequency band. Moreover, the sensors can function properly under the harsh condition of 120 °C temperature and 40 MPa pressure over the 4-hour test duration. The sensor array along with the interrogator has been running uninterruptedly over 3 weeks in a multi-stage hydraulic fracturing stimulation field test. On-site results show that our system can clearly resolve the vector nature of both compressional and shear waves generated by the microseismic events.

Highlights

  • Microseismic monitoring has demonstrated as an efficient tool for both geophysical investigations and energy industry

  • Results show that the developed fiber sensor array can provide a lower NEA level compared to moving-coil geophone systems at high frequencies as well as an increased dynamic range for the low-frequency band

  • Our results show that via time-division multiplexing and heterodyne demodulation, the system can achieve a NEA

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Summary

INTRODUCTION

Microseismic monitoring has demonstrated as an efficient tool for both geophysical investigations and energy industry. Results show that the developed fiber sensor array can provide a lower NEA level compared to moving-coil geophone systems at high frequencies as well as an increased dynamic range for the low-frequency band. These characteristics make the system favorable for microseismic events detection. When external seismic signal induces acceleration (a(t)) onto the sensor unit, the mandrel moves upwards causing the inertial mass to push downwards against the cylinder. The phase variation φs(t) was extracted by the heterodyne interrogation method In this system, the sensitivity K depends on the seismic signal frequency f and the natural frequency f0 of the sensor unit. Given the accessible material of the compliant cylinder to survive in high temperature (>100◦C) for a long time, the natural frequency f0 is set as 1.6 kHz, resulting a designed sensitivity of ∼43 dB

THE INTERROGATOR
NEA AND DYNAMIC RANGE
CONCLUSIONS
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