Seismometer Network
Broadband Seismometer Array Subsystem
Distributed network of broadband and short-period seismometers detecting moonquakes, meteorite impacts, and artificial vibrations across the Ark site.
Purpose
Provide comprehensive seismic monitoring of the Ark environment to characterize ground motion, detect potentially damaging seismic events, and supply data for structural response analysis.
Context
Lunar seismicity differs fundamentally from Earth: deep moonquakes originate at 700-1100 km depth from tidal stresses, shallow moonquakes are rare but powerful, thermal moonquakes occur at the terminator, and meteorite impacts produce seismic signals. This network must detect all types to protect the Ark.
Principles
- ▸Broadband seismometry covering 0.001-50 Hz frequency range for all moonquake types
- ▸Three-component sensing (vertical + two horizontal) at each station
- ▸Array configuration enabling source localization through triangulation
- ▸Ultra-low noise floor required due to absence of oceanic and atmospheric noise on Moon
Typical implementations
- ▸CNES/IPGP SEIS-type very broadband seismometers (InSight heritage)
- ▸Apollo Lunar Surface Experiment Package (ALSEP) passive seismic experiment legacy
- ▸Molecular electronic transfer (MET) seismometers for high sensitivity
- ▸MEMS accelerometers for strong-motion recording close to structure
- ▸Geophones for short-period, high-frequency detection
Lunar considerations
- ▸Extreme thermal cycling requires oven-controlled or deep-buried sensor installations
- ▸Lunar seismic Q factor is very high causing prolonged signal ringing (scattering in regolith)
- ▸No atmospheric noise floor enables detection of extremely small events
- ▸Vacuum environment eliminates convection-based thermal noise but complicates thermal management
- ▸Regolith coupling requires careful installation technique (burial or pier mounting)
- ▸200+ deep moonquake nests identified from Apollo data can inform monitoring strategy
Specifications
Functional
| primary function | Detect and characterize all seismic events in the vicinity of the Lunar Ark |
| inputs | Ground motion (velocity and acceleration), Calibration signals from internal calibration coils, Timing signals from master clock |
| outputs | Continuous seismic waveform data (three components per station), Event detection triggers, Ground motion parameters (PGA, PGV, spectral acceleration) |
| frequency range hz | 0.001-50 |
| sensitivity m per s2 | 1e-10 |
| dynamic range db | 180 |
| number of stations | 8 |
| sample rate hz | 100 |
| timing accuracy ms | 1 |
Physical
| mass kg | 120 |
| dimensions | Each station: 30cm diameter x 25cm height; array spans 500m radius |
| materials | Titanium housings, Fused silica suspension elements, Mu-metal magnetic shielding, Radiation-hardened electronics, Thermal insulation (MLI blankets) |
| installation depth m | 1.0 |
| burial in regolith | True |
| thermal stabilization | passive burial plus active oven control |
Operational
| power consumption w | 40 |
| thermal range c | -173, 127 |
| lifetime years | 100 |
| mtbf hours | 600000 |
Interfaces
Provides
- Three-component broadband seismic data from all stations at 100 sps
- Free-field ground motion data for comparison with structural response measurements
Requires
- 40W continuous power distributed to 8 stations via buried cabling
- Digitization, timestamping, and data collection from sensor array
Decomposes into
Cite this entry
Lunar Ark Codex. "Seismometer Network" (L2-SSM-SEIS). Retrieved 10 September 2026, from https://lunarark.com/entry/L2-SSM-SEIS
Licensed CC-BY-SA 4.0. You may reuse and adapt this entry with attribution, under the same licence.