Independent report into safety of Building 23 at ANSTO
The final report on the safety of Building 23 by the independent expert review team has been completed.
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The final report on the safety of Building 23 by the independent expert review team has been completed.
How to prepare samples for analysis on the Powder Diffraction beamline.
You are invited to submit to the various awards from ANSTO, User Advisory Committee (UAC) and Australian Neutron Beam User Group (ANBUG).
nandin member, SVSR, report on their proof-of-concept for a reusable Graphene Oxide (GO) membrane to capture waste water vapours from ageing sewerage systems.
The high-energy heavy-ion microprobe is used for the characterisation or modification of material properties at depths from approximately 1 micrometre to maximum depths of up to 500 micrometres from the material surface.
The need for a smaller, more transportable version of ANSTO’s 1500-litre atmospheric radon-222 monitor, and with a calibration traceable to the International System of Units, prompted the team to develop a 200-litre radon monitor that would meet those needs.
This scholarship recognises outstanding ability and promise in the field of nuclear science and technology, specifically as it applies to nuclear energy. Successful applicants will demonstrate a history of interest in nuclear energy and a desire to continue this interest.
ANSTO is one of the world's leading providers of irradiation services for silicon ingots, which are used by the multimillion dollar electronics industry across Europe and Asia. Each year, ANSTO irradiates more than 50 tonnes of silicon.
Read about an ANSTO scientist and their work to prepare for a school project or interview.
Role at ANSTO
Dr Inna Karatchevtseva undertakes work at ANSTO in two main areas: defence industry research and fundamental materials research.
The QUOKKA instrument provides the powerful technique of small-angle neutron scattering which can look at sizes and structures of objects on the nanoscale including soft matter.
Research elucidates how in situ cosmogenic radiocarbon is produced, retained and lost in the top layer of compacting snow (the ‘firn layer’) and the shallow ice below at an ice accumulation site in Greenland.