
Chapter 2. System Overview
Thank-you for purchasing a Güralp Radian digital seismometer system.
This section describes the key components of a full Radian system. The Radian instrument is the main standard product in the system; other components and accessories can be purchased optionally. Please check your order confirmation to see which components were purchased by your organisation.
2.1 Key features
A slim-line, 55 mm diameter sonde with 750 mm length for rapid post-hole deployment.
Bluetooth communication via Android App (available for mobile phone and tablet) confirms integrity of the installation without physical disturbance of site.
State-of-the-art seismic sensor allows full operation over a full tilt range of ±180° by automatically centring the masses;.
Streaming and storage of instrument response and calibration parameters dramatically simplifies data management (RESP and Dataless SEED formats).
Instrument orientation and inclination are measured using an internal magnetometer and MEMS accelerometer to store and stream geographically-aligned waveforms.
Internal MEMS accelerometer extends the head-room (clip level) of the instrument to 4 g, to capture high-amplitude ground motion from local seismic events.
Triaxial orthogonal (ZNE) instrument with high cross-axis rejection ratio (> 65 dB).
Velocity and Acceleration responses available - selected at time of order.
Retractable, three-jaw, motorised hole-locks for optimal coupling to bore-hole casings.
Frequency response flat to either velocity or acceleration between 120 s and 200 Hz.
Low-latency outputs available (approx. 0.01 s data packets).
Robust and water-proof, encased in SAE 316 corrosion-resistant stainless steel to protect the instrument in extreme environments.
Accurate time-base provided by either surface GNSS, Precision Time Protocol (PTP), Network Timing Protocol (NTP), or internal clock (< 1 ms drift per day without GNSS).
No mass locking required; automatic mass centring.
Dual-redundant microSD card data storage.
Low power consumption (2.1 W): suitable for temporary deployments using batteries and solar panels.
2.2 Main benefits
2.2.1 Post-hole installations
Faster deployment reduces total field-work costs and/or allows greater station density for high-resolution seismic monitoring.
Reduced transportation costs compared to traditional instrumentation.
Can be drilled/cored into bed-rock for exceptional coupling and noise performance.
Reduced material costs and footprint compared to traditional seismic vault installations.
High performance in areas of high cultural noise.
Dramatically improved noise performance (20 dB reduction compared to vault installations - horizontal components; IRIS figures).
2.2.2 Bore-hole installations
Deep installations allow you to get closer to the source and farther from cultural noise, for better subsurface characterisation
Ultra-low noise performance at depth
Excellent coupling with bore-hole casing provided by three-jaw hole-locks
2.3 Typical applications
2.3.1 Post-hole deployments
Rapid deployment for volcanic unrest monitoring: recording of long-period tremor events and volcanic-tectonic earthquakes using a single instrument.
Ultra-dense recording arrays for microseismic monitoring in noisy environments.
Legislative compliance: Suitable for use in "traffic-light" systems for energy extraction or storage.
Accurate recordings of strong ground shaking caused by local events.
Fast installation for rapid-response aftershock deployments.
Permanent regional and global seismic networks.
Recording of ice-quakes in glaciers.
2.3.2 Bore-hole deployments
Passive microseismic monitoring.
Vertical seismic profiling (VSP).
Monitoring of moderate-strong teleseismic earthquakes.
Complement dense surface arrays.