Subsurface & utility

Industry

Subsurface & utility

Find it before you dig. Record it before you backfill. Radar for what is under, LiDAR for what is open.

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Collection Subsurface & utility

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This job

Mapping what you cannot see

Subsurface investigation is the work of finding buried features before someone puts a machine through them, and recording what is actually there before it disappears again.

Two distinct jobs sit under that. Locating: finding services, voids, foundations, ordnance or fill across an area, non-destructively. And recording: capturing what was laid, where, while the trench is still open.

The first prevents strikes. The second prevents the next generation having the same problem you just had.

What makes subsurface work difficult

You cannot verify what you did not dig up. Every subsurface method returns an interpretation, not a measurement, and the interpretation carries uncertainty that the deliverable has to be honest about.

Ground conditions dominate. Radar penetration depends on soil conductivity, moisture and material. Clay is difficult. Wet clay is worse. The same equipment performs very differently across one site.

And records are usually wrong. As-laid drawings, where they exist at all, were often drawn from memory after the fact. The record you inherit is a hypothesis, not a fact.

How the day actually runs

Establish what you are looking for and how deep. Antenna frequency is a trade between depth and resolution, and you cannot have both. A 500 MHz unit resolves shallow detail; a low frequency unit reaches deeper and sees less.

Grid the survey area properly. Radar returns a cross-section along a line, so coverage is a function of line spacing. Wide spacing means you can walk a linear service straight past it.

Fly the radar and the magnetometer as separate passes if both are in scope. They detect different things: radar returns interfaces, magnetometry returns ferrous anomalies.

Capture the surface with LiDAR or photogrammetry at the same time, so the subsurface interpretation sits on real topography.

Walk open trenches before backfill. That is the only moment the truth is visible.

What to fly, what to walk

What you needCapture withWhy
Buried services, voids, interfacesZond Aero 500 or 1000Higher frequency, shallower, better resolution
Deeper features, geology, fillZond Aero LFLower frequency reaches further
Ferrous objects, ordnance, drumsSensys MagDrone R3Magnetic anomaly, not radar reflection
Surface topography for contextZenmuse L3 or Matrice 4ESubsurface data needs a real surface under it
Open trench before backfillSHARE C10-32 or C1 ProRecords exactly what was laid, where
Pits, chambers, culverts, cable tunnelsSHARE C10-32Enclosed, no sky view

Radar tells you what is under the ground. A scanner records the surface and every accessible void. Together that is a complete utility model.

What you can and cannot claim

Depth from radar is calculated from signal velocity, and velocity varies with ground conditions. Calibrate against a known target on site where you can, and state the assumption where you cannot.

Position in plan is generally more reliable than depth. Say so in the deliverable.

Every subsurface finding is an interpretation. The professional standard is to state confidence, state method, and state coverage, rather than present anomalies as located services. A drawing that shows a line without a confidence statement invites someone to dig on it.

Where the consequence of being wrong is high, verify with potholing.

What gets handed over

A plan of interpreted features with confidence levels, a statement of method and coverage, and the raw radar sections so someone can check the interpretation.

Recipients are civil contractors, utility locators, geotechs and archaeologists, all of whom will act on it with machinery. They need to know what is confident and what is indicative.

What gets it questioned: anomalies presented as identified services, depths quoted without a velocity assumption, and coverage claims that do not match the line spacing actually walked or flown.

The common miss

Line spacing too wide. A service running parallel to your survey lines can sit between them and never appear. Grid tighter than feels necessary, and grid in two directions where it matters.

The other one is over-claiming. An anomaly is an anomaly. Calling it a 150 mm water main because that is what the drawing says is how strikes happen.

And the missed opportunity: the trench that gets backfilled without anyone recording it. Ten minutes with a scanner would have produced a permanent record, and instead the next crew inherits the same uncertainty you did.

Start with these

One or two kits that fit this job. Family pages cover the rest of the line.

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Collection Subsurface & utility

Questions for this job

Choosing a model

Which Zond Aero antenna do I need?
Depth versus resolution. The 500 MHz unit gives the best resolution on shallow targets, typically services and near-surface features. The 1000 resolves finer detail shallower still. The LF unit trades resolution for depth and suits geology, deeper fill and larger buried structures. If you mainly locate services, start at 500. If your briefs are geotechnical or archaeological, the LF is the one.
Do I need a magnetometer as well as GPR?
They detect fundamentally different things. Radar returns interfaces between materials, so it finds pipes, voids and layer changes regardless of material. Magnetometry finds ferrous objects specifically, which makes it the right tool for ordnance, steel drums, buried tanks and iron pipework. Sites with a UXO or contamination question need both. Sites with a service-locating question usually need radar alone.

Buying & price

Why fly GPR instead of pushing a cart?
Coverage rate and access. A pushed unit is slower and limited to ground you can walk with a cart, which excludes rough terrain, vegetation, water margins and contaminated sites. Airborne radar covers large areas quickly and reaches places a cart cannot. For tight urban service locating a pushed unit is often still the right tool, so this is an addition to the toolkit rather than a replacement.

Accuracy

How deep will it actually see?
Ground dependent, and any supplier quoting a single figure is oversimplifying. Dry sandy soil gives good penetration. Clay, particularly wet clay, attenuates the signal severely and can cut usable depth to a fraction of the published range. Saline groundwater is worse again. Expect to characterise the site early and set client expectations from a test line rather than from the brochure.
Can I say I have located a service, or only an anomaly?
An anomaly, unless you have verified it. This matters legally and practically. Radar returns a reflection from an interface; identifying what caused it is interpretation. Present findings with confidence levels, state your method and coverage, and recommend potholing where the consequence of being wrong is high. Presenting anomalies as located services is how strikes happen.

Workflow & data

Why scan an open trench if we already have the design?
Because the design is not what got laid. Alignments shift around obstructions, depths change with ground conditions, and nobody updates the drawing. Ten minutes with a scanner before backfill produces a permanent, measured record of what is actually there. Utilities are increasingly asking for it, and it is the cheapest data you will ever collect on that asset.
Next step

Bring a real site

Start with a call. If it looks like a fit, we bring the kit to your site and capture the section that usually causes trouble. You keep the data.

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Collection Subsurface & utility