Reducing 3D geological uncertainty via improved data interpretation methods. The integrity of 3D geological models heavily relies on robust and consistent data interpretation. This project proposes an innovative workflow for 3D modelling to minimise geological uncertainty. Advanced visualisation and intelligent decision support methods will be combined to assist geological interpretation. Feedback on interpretation will be provided based on data evidence and consistency with expert knowledge and ....Reducing 3D geological uncertainty via improved data interpretation methods. The integrity of 3D geological models heavily relies on robust and consistent data interpretation. This project proposes an innovative workflow for 3D modelling to minimise geological uncertainty. Advanced visualisation and intelligent decision support methods will be combined to assist geological interpretation. Feedback on interpretation will be provided based on data evidence and consistency with expert knowledge and previous interpretations. The process can be considered as a spelling and grammar checker for geological interpretation. The outcome of this study aims to achieve an improved workflow that reduces model uncertainty, resulting in a broad and significant impact on the management of Australian mineral, energy and water resources.Read moreRead less
Engineering planetary habitability: Earth’s first billion years. This project aims to establish the critical physical-chemical factors in the early surface environment and tectonic regime that supported early life and continuing habitability. Life was established on Earth within the first billion years of its 4.56-billion-year history. This project’s integrated geological and geochemical study will investigate this period’s rare sedimentary and volcanic record, including the oldest fossiliferous ....Engineering planetary habitability: Earth’s first billion years. This project aims to establish the critical physical-chemical factors in the early surface environment and tectonic regime that supported early life and continuing habitability. Life was established on Earth within the first billion years of its 4.56-billion-year history. This project’s integrated geological and geochemical study will investigate this period’s rare sedimentary and volcanic record, including the oldest fossiliferous sequences discovered recently, to show how the early Earth’s chemistry supported life and evolution. The project expects to enhance understanding of why life prospers on some habitable zone planets but not on others.Read moreRead less
Carbon dioxide sequestration more than 3.7 billion years ago and the oldest climate cycles. More than 3.7 billion years ago atmospheric greenhouse CO2 was sequestered into limestone sedimentary rocks deposited in ice-free oceans. Why then, with the 30-25 per cent cooler sun in those times, was our earth not frozen over? Solving this oldest climate problem, will give the deepest-time perspective to the earth's changing climate feedback loops.
Multiscale and multiphase modelling of deformable porous media. The physics of our Nation's most pressing engineering problems involve simultaneous processes on multiple scales. Our research conducts massive computer simulations of processes involving fluid flow in rock on a broad range of scales. Simulations of this kind make future technologies such as CO2 sequestration more predictable and manageable.
Banded iron formations: life, oxygen and ocean chemistry. This project aims to investigate the co-evolution of life and environments during Earth’s first two billion years using iron-rich chemical sediments deposited from global oceans. The project expects to generate knowledge of Earth’s transition into a planet habitable for complex life by combining nanoscale characterisation techniques, with laboratory experiments and theoretical modelling. Expected outcomes include transformative ideas abou ....Banded iron formations: life, oxygen and ocean chemistry. This project aims to investigate the co-evolution of life and environments during Earth’s first two billion years using iron-rich chemical sediments deposited from global oceans. The project expects to generate knowledge of Earth’s transition into a planet habitable for complex life by combining nanoscale characterisation techniques, with laboratory experiments and theoretical modelling. Expected outcomes include transformative ideas about the role of life in iron and phosphorus cycles, the chemistry of the early ocean, ancient biological productivity, the antiquity of oxygenic photosynthesis and the rise of oxygen. The project will also deliver new conceptual models for the formation of the host-rocks for most of the world’s iron resources, improving how we explore for iron in the Earth’s crust. This should provide benefits to understanding geobiology on Earth and other planets.Read moreRead less