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This project addressed potential connection between aquifers in an area where groundwater extraction for both agriculture and coal seam gas occur. The analysis of water chemistry and isotopes, and new mathematical techniques were employed. Overall, there was no evidence of significant solute or gas transfer between aquifers. Methane gas was found to be generated within all aquifers via microbial activity. As a result, stable and radioactive isotopes results are complex. In contrast, hydrochemistry, and the analysis of very low concentrations of the lithium ion and its stable isotopes were found to be effective indicators of coal-seam gas bearing groundwater

Hydrochemical and isotopic indicators of hydrological processes within coal seam gas formations and adjacent aquifers, Condamine River catchment, QLD