Radiometrics

A perspective view of a ternary radiometric image derived from the Radiometric Map of Australia which shows the relative concentrations of the radioelements potassium, thorium and uranium. The image was derived by clipping out a small area of the map and enhancing it by draping the ternary image over the topography, giving a three dimensional effect.

Perspective view of a ternary
radiometric image draped over
topography

A stylised view of a low-flying aircraft flying over the landscape while recording the radioactive response of the earth.

The radioactivity of the Earth
can be measured using low-flying
aircraft

The ternary radiometric image of the Radiometric Map of Australia which shows relative concentrations of the radioelements potassium, thorium and  uranium for the whole of Australia.

Ternary image of the Radiometric
Map of Australia

The radiometric, or gamma-ray spectrometric method is a geophysical process used to estimate concentrations of the radioelements potassium, uranium and thorium by measuring the gamma-rays which the radioactive isotopes of these elements emit during radioactive decay. Airborne gamma-ray spectrometric surveys estimate the concentrations of the radioelements at the Earth’s surface by measuring the gamma radiation above the ground from low-flying aircraft or helicopters

All rocks and soils contain radioactive isotopes, and almost all the gamma-rays detected near the Earth’s surface are the result of the natural radioactive decay of potassium, uranium and thorium. The gamma-rays are packets of electromagnetic radiation characterised by their high frequency and energy. They are quite penetrating, and can travel about 35 centimetres through rock and several hundred metres through the air. Each gamma ray has a characteristic energy, and measurement of this energy allows the specific potassium, uranium and thorium radiation to be diagnosed.

The gamma-ray spectrometric method has many applications but is used primarily as a geological mapping tool. Changes in lithology, or soil type, are often accompanied by changes in the concentrations of the radioelements. The method is capable of directly detecting mineral deposits. Potassium alteration, which is often associated with hydrothermal ore deposits, can be detected using the gamma-ray spectrometric method. It is also used for uranium and thorium exploration, heat flow studies and environmental mapping.

Geoscience Australia and the State and Northern Territory Geological Surveys have systematically surveyed most of Australia over the past 40 years using airborne gamma-ray spectrometry. These surveys have been combined into a Radiometric Map of Australia, consisting of potassium, uranium and thorium grids of the continent at 100 metre resolution. The data are available for free download through the Geophysical Archive Data Delivery System (GADDS) External site link.

Topic contact: minerals@ga.gov.au Last updated: October 4, 2013