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Hobart, Australia
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HomeGeophysicsGeorradar GPR (Ground Penetrating Radar)

GPR (Ground Penetrating Radar) Survey in Hobart

Soils in Sandy Bay differ sharply from those in the city center. Sandy Bay sits on deep alluvial deposits with high clay content, while the CBD rests on weathered dolerite bedrock close to the surface. That contrast makes a GPR (Ground Penetrating Radar) survey essential in Hobart for locating buried pipes, cables, and old foundations before excavation. Without it, you risk hitting unknowns that halt work. The radar energy reflects differently off clay than rock, so we adjust frequencies accordingly. We pair this with calicatas exploratorias where the ground is too conductive for clear imaging, and with ensayo CPT when we need continuous soil profiles alongside the radar results.

Illustrative image of Georradar gpr in Hobart
In Hobart's variable geology, a GPR survey cuts excavation risk by revealing hidden pipes, voids, and bedrock depth before the first shovel hits ground.

Methodology and scope

In Hobart, many projects discover abandoned tram tracks or old sandstone sewers during excavation. We start every GPR (Ground Penetrating Radar) survey by checking the site history and existing utility plans. Then we deploy a 400 MHz antenna for general depth down to 4 meters, switching to 900 MHz for finer detail near the surface. Data processing removes noise from the conductive clay layers typical of Battery Point. For critical bore paths, we cross-reference radar results with ensayo SPT boreholes to confirm what the radar shows. The main parameters we record include signal velocity, two-way travel time, and reflection amplitude. We follow AS 1726 for field procedures and AS/NZS 1170.2 for load assumptions on buried structures.

Local considerations

Hobart's coastal humidity and frequent rainfall create conductive near-surface soils that can weaken radar signals. Wet clay in the Derwent estuary flats absorbs energy fast, reducing depth penetration. In the hilly suburbs like Mount Stuart, shallow bedrock creates multiple reflections that mask utilities. We mitigate this by using lower-frequency antennas and applying advanced gain filters during post-processing. Dense tree cover in areas like the Hobart Rivulet also interferes with surface coupling. We clear a small path when needed to maintain consistent antenna contact.

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Explanatory video

Applicable standards

AS 1726:2017 Geotechnical site investigations, AS/NZS 1170.2:2021 Structural design actions (wind actions), AS 1289.7.3 Standard guide for using the surface ground penetrating radar method

Associated technical services

01

Utility & Void Detection Survey

Locate buried water mains, electrical conduits, gas lines, and old foundations in Hobart's urban zones. We scan on a 0.5 m grid and mark findings directly on the pavement or ground surface. Suitable for depths down to 3 m in typical Hobart soils. Deliverable includes geo-referenced site plan.

02

Bedrock & Groundwater Table Mapping

Map the depth to weathered dolerite bedrock in Hobart's hillside suburbs like Lenah Valley and Tolmans Hill. We use a 200 MHz antenna for deeper penetration (up to 6 m in dry conditions). Results help foundation designers choose between shallow footings and deep piles. Report includes depth contour maps.

Typical parameters

ParameterTypical value
Antenna frequency range400 MHz to 900 MHz
Maximum effective depth4 m in dry soils, 1.5 m in clay
Signal velocity in soil0.10–0.15 m/ns (typical)
Two-way travel time resolution0.5 ns
Data grid spacing0.5 m x 0.5 m (standard)
Output formatRadargrams with depth-calibrated markers

Frequently asked questions

How deep can GPR penetrate in Hobart's clay soils?

In the wet alluvial clays common near the Derwent River, maximum depth is about 1.5 m with a 400 MHz antenna. In sandy or gravelly soils on higher ground, penetration can reach 4 m. We adjust antenna frequency based on site-specific conditions.

What is the typical cost of a GPR survey in Hobart?

A standard utility detection survey for a 500 m² lot in Hobart ranges from AU$1.940 to AU$3.680 depending on access conditions and required grid density. Larger sites or deeper bedrock mapping cost more. We provide a fixed quote after a site visit.

Can GPR detect plastic pipes or fibreglass tanks?

Yes, but the contrast between plastic and surrounding soil is lower than for metal. In Hobart's clay soils, plastic pipes down to 1.2 m depth are reliably detected with a 900 MHz antenna. We verify ambiguous signals with a potholing test pit.

Do you need site plans before the survey?

Yes. We request any existing utility plans, building drawings, or previous geotechnical borehole logs for the site. This helps us calibrate the radar velocity and interpret reflections. For heritage sites in Hobart, we also check the council's historic infrastructure records.

Location and service area

We serve projects across Hobart.

Location and service area