Vibration & seismic monitoring — Calgary, Alberta

Measuring what
moves the ground.

PPV monitoring for quarry blasts, pipelines and construction. Induced seismicity monitoring for fracking and wastewater injection. Seismic arrays for natural earthquakes.

  • Peak Particle Velocity
  • Quarry blasting
  • Pipeline construction
  • Construction vibration
  • Induced seismicity
  • Hydraulic fracturing
  • Wastewater injection
  • Earthquake seismic arrays
  • Natural seismicity
  • Earthquake early warning
  • Canada
01 — Services

Three ways the ground moves.

Vibration and seismic monitoring for blasting, construction and energy projects.

Schematic — not to scale

01 — PPV

Vibration monitoring

Peak Particle Velocity monitoring for quarry blasts, pipeline construction and construction sites.

  • Quarry blasts
  • Pipelines
  • Construction
02 — ISM

Induced seismicity monitoring

Monitoring of seismicity induced by hydraulic fracturing and wastewater injection.

  • Hydraulic fracturing
  • Wastewater injection
03 — Arrays

Earthquake seismic arrays

Seismic arrays recording natural seismicity.

  • Natural seismicity
  • Seismic arrays
02 — Examples

Monitoring,
in practice.

Examples of the work: vibration limits on construction and traffic sites, induced events around wells, regional earthquakes and early warning.

PPV · Vibration monitoringCalgary, Alberta

Scale and table: City of Calgary Roads, “What are Traffic Vibrations”

Fig. 01Peak Particle Velocity (PPV) monitoringA seismograph records ground vibration; readings are compared with how people feel it, from not noticeable to unpleasant.
ISM · Event monitorExample · Nov 2015
Fig. 02Induced seismicity monitoring (ISM)Located events with time, depth, magnitude and focal mechanism, plus live station status. Microseismic events map the fractures along a stimulated well; raised fluid pressure can push a nearby fault to slip.
Natural seismicity · Regional eventExample · Sept 2019
Fig. 03Natural seismicityA regional earthquake recorded across an array: station triggers, epicentre and distance from the stations, and the recorded waveforms with P and S arrivals picked.
FaultEpicentreS-waveDamaging wavesP-waveFirst felt waveSensors≈ 10–20 km apartAlert centreCity — warnedEach station+DigitiserGüralp MinimusAccelerometerGüralp FortisAdapted from USGS

Tap the diagram to open it full screen

Fig. 04Earthquake early warning (EEW)Sensors detect the faster P-wave and send an alert ahead of the slower, damaging S-waves.
03 — In the field

From the field.

04 — Contact

Planning a blast, a build
or a well program?

Tell us about the site and what needs monitoring.

Contact
Rob Kendall, MSc, PGeophPresident
Office
440 Brunswick Ave SW
Calgary, Alberta T2S 1N8