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.
Unlocking the anchors of soil organic carbon to manage climate change. Soil is the largest reservoir of terrestrial organic carbon. Most of the organic carbon in soils is preserved by association with minerals, however, the composition and stability of mineral-associated organic carbon remain poorly understood. The project will use novel and emerging techniques to discover the composition of organic carbon and stability of organic carbon present in mineral-organic associations in representative ....Unlocking the anchors of soil organic carbon to manage climate change. Soil is the largest reservoir of terrestrial organic carbon. Most of the organic carbon in soils is preserved by association with minerals, however, the composition and stability of mineral-associated organic carbon remain poorly understood. The project will use novel and emerging techniques to discover the composition of organic carbon and stability of organic carbon present in mineral-organic associations in representative Australian soils. Expected outcomes include new knowledge necessary for emerging global carbon cycling models and improve future climate projections. Read moreRead less
Drought effects on soil carbon and nitrogen cycling mediated by rhizosphere processes. There is much uncertainty about how drought caused by global warming will affect agricultural sustainability in Australia. This project will provide new knowledge about plant-soil interactions affecting carbon and nutrient cycling and will make predictions about long-term soil carbon storage and agricultural productivity in response to drought.