Bundaberg Au
Bundaberg, Australia

HVSR Microtremor Survey in Bundaberg: Passive Seismic for Soil Resonance

The alluvial flats around the Burnett River in Bundaberg behave very differently from the volcanic-derived soils near the town centre. In the river corridor, soft Holocene clays can amplify ground motion at low frequencies, whereas the older basalt profiles closer to Woongarra show much stiffer responses. An HVSR microtremor survey in Bundaberg captures that natural resonance directly, measuring the H/V spectral ratio from ambient vibrations. It is a quick, non-invasive way to identify fundamental site frequency without drilling. For projects on the coastal plain, we often pair the HVSR results with a subrasante vial assessment to understand how the subgrade will behave under cyclic loading.

Illustrative image of HVSR microtremor survey (Nakamura method) in Bundaberg
The HVSR microtremor survey in Bundaberg captures natural soil resonance directly, revealing the fundamental frequency that governs seismic site response.

Methodology applied in Bundaberg

Bundaberg sits on a complex mix of Quaternary alluvium, coastal sands, and Tertiary basalt flows, which means the depth to bedrock can vary from 5 metres near Kalkie to over 30 metres around the airport. The Nakamura method works by deploying a three-component seismometer on the ground for 30 to 60 minutes, recording microtremors generated by wind, ocean waves, and distant traffic.

Key parameters derived from the survey include:
  • Fundamental resonance frequency (f0) in Hz
  • Peak H/V amplitude (amplification factor)
  • Estimated depth to seismic impedance contrast
  • Site class correlation per AS 1170.4
For deeper basin zones, we combine the microtremor data with a factor-seguridad evaluation to check whether the amplified motion could trigger slope instability in cuttings. The whole survey is non-destructive and causes zero traffic disruption, which is important on busy roads like Bourbong Street.
HVSR Microtremor Survey in Bundaberg: Passive Seismic for Soil Resonance
ParameterTypical value
Recording duration30-60 minutes per station
Frequency range0.2 – 20 Hz
Sensor typeThree-component broadband seismometer (2 Hz corner)
H/V processingKonno-Ohmachi smoothing, 40 band-width constant
Depth estimatef0 = Vs / (4H) approximation using regional Vs profiles
AS 1170.4 site classClass Aa to De based on f0 and amplification

Typical technical challenges in Bundaberg

In Bundaberg, many times we see that the main risk is not the peak ground acceleration itself, but the resonance coupling between a soft soil layer and a medium-rise building. A 3-storey structure has a natural period around 0.3–0.5 seconds, and if the soil resonates at 2–3 Hz, the amplification can double the seismic demand. An HVSR microtremor survey in Bundaberg identifies those critical frequencies before design. Without it, engineers may under-design for low-frequency shaking and over-design for high-frequency motion, leading to either unsafe or uneconomic structures.

This service complements our laboratory testing work for a complete project analysis.

Need a geotechnical assessment?

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Email: contact@geotechnicalengineering1.xyz
Applicable standards: AS 1170.4-2007 (Earthquake actions), SESMWG Guidelines for HVSR Measurement (2016), SESMWG Guidelines for HVSR Interpretation (2018)

Our services


We offer three complementary HVSR survey scales to match different project budgets and site conditions in Bundaberg.

Single-station HVSR survey

A rapid 60-minute measurement at one location to determine the fundamental frequency and site class. Ideal for small residential projects or a quick check before a geotechnical borehole program.

Multi-station array survey

Five to ten stations deployed along a profile or grid to map lateral variations in resonance frequency. Suitable for subdivisions, road corridors, and medium-rise developments where soil conditions change across the site.

Integrated HVSR + MASW survey

Combining microtremor measurements with active MASW to obtain both the resonance frequency and a Vs30 profile. This is the preferred approach for AS 1170.4 site classification on complex ground.

Frequently asked questions

What is the HVSR microtremor survey method?

The HVSR (horizontal-to-vertical spectral ratio) method, also known as the Nakamura technique, records ambient ground vibrations using a three-component seismometer. The ratio of horizontal to vertical spectra reveals the fundamental resonance frequency of the soil column. It is a passive seismic method that requires no artificial energy source.

How much does an HVSR survey in Bundaberg cost?

For a standard single-station survey in Bundaberg, the cost typically ranges between AU$2,120 and AU$3,570. Multi-station arrays or integrated surveys with MASW are higher due to additional field time and processing. Contact us for a quote tailored to your specific project scope and number of stations.

How is HVSR different from MASW or ReMi?

HVSR measures the natural resonance frequency of the soil using passive ambient vibrations only. MASW and ReMi require an active seismic source (sledgehammer or weight drop) to generate surface waves. HVSR is faster and less intrusive, but it does not provide a direct Vs30 value. MASW or ReMi are needed when a shear-wave velocity profile is required for site classification.

Do I need an HVSR survey for a single residential house in Bundaberg?

For a standard single-storey house on stiff ground, an HVSR survey is usually not mandatory. However, if the site is on soft alluvium near the Burnett River or if you are building a two-storey or three-storey structure, the survey helps identify potential resonance issues. Local council may request it for developments in known liquefaction-prone zones.

Coverage in Bundaberg


Visual overview