Australia’s OPAL multi-purpose reactor prepares for new milestone
Routine transport of spent nuclear fuel
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Routine transport of spent nuclear fuel
Micro-Particle Induced X-ray Emission (µPIXE) is used to construct elemental maps that show variations of an element's concentration across the sample surface.
Early research at ANSTO has contributed to development of innovative submicron particle encapsulation technology.
Collaboration finds that old carbon reservoirs are unlikely to cause a massive greenhouse gas release in a warming world.
New material shows enhanced conductivity for solid oxide fuel cells used in satellites, spacecraft, transport vehicles and as power source
New high energy ion microprobe beamline supports space research on the effects of radiation on astronauts.
ANSTO and the Australian Radiation Protection and Nuclear Safety Agency (ARPANSA) have been recognised for their valuable contributions to the search and recovery efforts for a missing 8mm-long radioactive capsule in the Western Australian outback.
Cyclotek and ANSTO have announced the launch of a Joint Venture (JV), to establish Australia’s first GMP (Good Manufacturing Practice) theranostics facility starting in Melbourne, Australia.
Billions of tonnes of iron ore tailings are generated each year from the mining industry. Converting these toxic tailings into soil-like materials which can develop and sustain plant and microbial communities is critical for mine site remediation and improved environmental outcomes.
You may be confident about the major crystallographic phases of your ore body – but what about those minor phases that can affect processing or cause long-term problems with remediation?
ITRAX has now analysed more than a kilometre of cores since it became operational in 2012.
A new radiocarbon dating facility opened at the University of New South Wales (UNSW) will complement the extensive radiocarbon facilities at ANSTO’s world-leading Centre for Accelerator Science
Insights into the formation of deep river canyons mountain ranges in intra-tectonic plate areas by SAAFE Scholarship recipient and collaborators.