From organo-mineral nanocomposite to Australian basins; an integrated approach to unconventional gas exploration and development. Gas production from unconventional shale reservoirs is a potential major energy boom in Australia that will lower carbon emissions over comparable coal and oil use. The geological controls of shale are currently too poorly understood to direct effective exploration. This project will be the largest international effort to develop this knowledge.
Linkage Infrastructure, Equipment And Facilities - Grant ID: LE120100162
Funder
Australian Research Council
Funding Amount
$150,000.00
Summary
Integrated 2MHz Nuclear Magnetic Resonance high temperature tri-axial flow cell apparatus. The development of an integrated facility for petrophysical measurements allows the efficient use of expensive rock cores from gas or liquid reservoirs to develop reliable cross-correlations at conditions encountered in real reservoirs. The equipment is optimised for applications to unconventional reservoirs like Australia’s gas resources, in particular coal-bed methane reservoirs and gas reservoirs where ....Integrated 2MHz Nuclear Magnetic Resonance high temperature tri-axial flow cell apparatus. The development of an integrated facility for petrophysical measurements allows the efficient use of expensive rock cores from gas or liquid reservoirs to develop reliable cross-correlations at conditions encountered in real reservoirs. The equipment is optimised for applications to unconventional reservoirs like Australia’s gas resources, in particular coal-bed methane reservoirs and gas reservoirs where gas is difficult to extract.Read moreRead less
Carbon sequestration by mineral surface area as a feedback to climate warming in a greenhouse ocean. The project will investigate a previously unrecognised negative feedback to global warming resulting from sequestration of carbon to marine sediments by soil-formed clay minerals. By studying the past transitions to greenhouse periods, this project will assess the likely influence of this feedback in the present transition to a warmer climate.