WHAT

LeNS-UK is a NERC funded instrument facility that was established in September 2025 and aims to provide seismic nodes to the UK science community for a wide variety of applications.

Traditional broadband seismometers have been used for decades to advance our knowledge of the Earth’s internal structure and processes. However… read more… 

… while traditional seismometers typically have good long period response, low noise floors and extensive recording durations (months-years), they are bulky and require significant power infrastructure (solar panels, large batteries etc) in order to operate. This limits the number that can be deployed and the choice of locations that are suitable for installation. In contrast, seismic nodes are compact instruments that incorporate the sensor, power supply, digitiser, recording media and GPS into a single package. Consequently, they can be readily deployed in large numbers with little effort. While the fidelity of their recordings are inferior to broadband instruments, particularly at longer periods, and their recording durations are limited (30-50 days), they provide an opportunity to record many aspects of the seismic wavefield that were previously out of reach. Typical seismic node deployments can involve 100s, 1000s or even 10s of thousands of instruments in dense arrays that could span urban areas, areas of dense vegetation, or remote regions that are only accessible on foot. Consequently nodal deployments have revolutionised modern seismology with applications in energy resources (e.g. geothermal), environmental monitoring (e.g. soil moisture) and natural hazards (e.g. landslides, volcanoes). 

SPECS

LeNS-UK hosts two types of seismic node in order to offer the flexibility for a wide range of experiments. The Stryde node is a small, compact instrument that contains a single component accelerometer. It is ideal for deployments that involve large numbers closely spaced nodes. The second type of instrument is a SmartSolo node, which contains a 3-component geophone. While much more bulky than the Stryde node, it is capable of recording all three components of ground motion and has superior long period response. In addition to these nodes, LeNS-UK has a variety of supporting equipment to facilitate charging, data download and storage. The table below provides a summary of what is available.

SmartSolo

  • 200x SmartSolo IGU-16HR sensors with 3-component, 5Hz Geophone, 64Gb, 2.4kg, 30 days recording duration
  • 25x IGU-16HR-EB battery packs that permit the use of any external power source
  • 3x battery charger units with 16 slots each, mobile
  • 3x data harvesting units with 16 slots each, mobile

Stryde

  • 1980x Stryde node Range+ single component accelerometers, 8Gb, 150g, 50 days recording duration
  • 1x Nimble Next case to charge and download up to 90 nodes simultaneously
  • 2x Nest Kits to charge or download two nodes at a time in the field

In addition to the above, the facility also has various peripheral equipment including initialisation devices, laptops, hand-held devices and tools to help operate the equipment.

HOW TO

Deploying a node is relatively simple – just stick it into the ground and walk away. However, some things to consider include:

Accurately record its location … 

If you mark the location by a stick or some other protruding object, then standard GPS locations may be sufficient. However, if you bury it, then you may need to use a differential GPS or some other highly accurate location method, otherwise you run the risk of losing the instrument. Furthermore, if you use very dense node deployments, then standard GPS locations may not be accurate enough to make the recorded data as useful as you might have hoped.

To bury or not to bury …

In general, you get much better signal to noise ratios if you bury the node, since it reduces wind noise and noise caused by temperature variations. So where possible, this is strongly recommended. However, the on-board GPS has limitations, so you cannot bury it too deeply, although this depends on soil type. Wet clay is the worst, while dry sand is the best.

Is anywhere ok …

One nice thing about nodes is that they can be easily hidden and the presence of vegetation that would rule out the use of solar panels is unlikely to be an issue. However, they are still subject to noise sources such as nearby roads, and their deployment in saturated ground or areas subject to flooding is not recommended. Furthermore, if deploying in urban environments or places with significant population densities, then give careful consideration to the possibility that some curious person might dig up the node and throw it in the bin (which has happened before!).

ABOUT

LeNS-UK is managed by Professor Nicholas Rawlinson and seven Co-Investigators from other institutions around the UK. A brief summary of what they do and how they will use the nodes is listed below.

Nick

Prof Nicholas Rawlinson, McKenzie Professor of Earth Sciences and head of Bullard Labs, University of Cambridge

Nick uses seismic nodes to track melt migration beneath active volcanic regions in Iceland. As magma pushes it way through the crust, it generates very small earthquakes called microseisms, which are best detected and characterised by very dense seismic deployments. Outcomes of this research include a better understanding of precusory signals prior to eruptions, and a new insights into the operation of volcanic plumbing systems.

Alex

Dr Alex Brisbourne, Ice Dynamics and Palaeoclimate, British Antarctic Survey, Cambridge

Dr Alex Brisbourne is a Glacier Geophysicist at the British Antarctic Survey. To investigate the ice sheets and what lies beneath them, Alex uses seismic nodes to record both naturally occurring icequakes and human made seismic sources. Analysis of these signals helps us understand how the icesheets will evolve, and how they will contribute to sea level rise in the future.

Karen

Dr Karen Lythgoe, School of Geosciences, University of Edinburgh

Nodes have made high-resolution imaging of fault zones feasible, with a short recording time and in remote areas, allowing better characterisation of fault zones at seismogenic depths. I have deployed and analysed nodal arrays above the Sumatran Fault in Indonesia,  allowing microseismicity detection that delineates fault geometry and changes in mechanical behaviour. I’ve also used nodal arrays to investigate volcano-tectonic interactions, subsurface structure in urban areas, and most recently for environmental seismology applications.

Paula

Dr Paula Koelemeijer, Department of Earth Sciences, University of Oxford

Through the use of seismic nodes, we aim to characterise anthropogenic seismic noise in urban environments. This noises typically hinders our ability to detect natural seismicity. We are also interested in studying the impact of this noise due to human activities on animals and their behaviour. 

James

Prof James Hammond, School of Natural Sciences, Birkbeck, University of London

I plan to use seismic nodes to study the critical zone, in particular to understand how passive seismology can be used to monitor changes in the shallow soil. I will also use the equipment to densely instrument volcanic and tectonic areas, to improve earthquake location and seismic imaging.

Jess

Dr Jessica Johnson, School of Environmental Sciences, University of East Anglia

Jess uses seismology to explore how fluids move underground and how stress builds up around hazardous natural phenomena. Her research spans tracking tiny earthquakes on the crumbling cliffs of North Norfolk to studying explosive volcanic transitions in the Caribbean. Recently, Jess has been combining dense seismic arrays with machine learning to uncover the hidden processes that trigger seismic activity.

Tom

Dr Tom Kettlety, Department of Earth Sciences, University of Oxford

I use nodal data to better understand and mitigate induced seismicity and earthquakes that could affect industrial activities.  This includes using local microseismic networks for monitoring fluid injection operations of geothermal sites, using nodes for mining-induced seismicity monitoring, or dense array beamforming for regional earthquake detection near prospective CO2 storage operations.

Mark

Dr Mark Ireland, School of Natural and Environmental Sciences, Newcastle University

At Newcastle University, we have leveraged nodal seismometers to advance near-surface imaging for geotechnical projects and geothermal energy exploration. Nodes offer deployment flexibility and cost-effectiveness over traditional methods; we’ve explored these large-N deployments for ambient noise tomography deployments at site-specific scales. We have experience in deploying from several hundred up to 3000!

APPLY

Members of the LeNS-UK management committee have priority use of the node pool. However, we anticipate having some spare capacity, so welcome applications from UK-based researchers who would like to use the nodes, provided they are available. Alternatively, external users may also wish to collaborate with one or more members of the management committee on their project, in which case they are welcome to email them directly. If you would like to use the node pool, then please complete and submit the form below. 

LeNS-UK Application
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