Oral Presentation NCGRT/IAH Australasian Groundwater Conference 2019

The canary or the coalmine? Isotopic evidence of drying climate versus groundwater outflow as the cause for recent losses from Thirlmere Lakes, NSW  (284)

Mark A. Peterson 1 , Dioni Cendón 1 , Catherine Hughes 1 , Jagoda Crawford 1 , Stuart Hankin 1 , Martin Krogh 2 , Kirsten L. Cowley 2 , Tim Cohen 3 , Martin S. Andersen 4 5 , Christian Anibas 4 5 , Will Glamore 6 , Shenyang Chen 6 , Wendy Timms 7 , Tim McMillan 4 8
  1. ANSTO, Lucas Heights, NSW, Australia
  2. Office of Environment and Heritage , Sydney, NSW, Australia
  3. GeoQuest Research Centre, School of Environmental Sciences, University of Wollongong, NSW, Australia
  4. Connected Waters Initiative, UNSW Sydney, NSW, Australia
  5. School of Civil and Environmental Engineering, UNSW Sydney, NSW, Australia
  6. Water Research Laboratory, School of Civil and Environmental Engineering, UNSW Sydney, NSW, Australia
  7. School of Engineering, Deakin University, Waurn Ponds, VIC, Australia
  8. School of Minerals and Resources Engineering, UNSW Sydney, NSW, Australia

The Thirlmere Lakes Research Program (TLRP) is a collaboration investigating water loss mechanisms in recent drying of five adjacent lakes, located 75 km south-west of Sydney. Some stakeholders and previous studies have perceived a correlation with local longwall coal mining history and suspect deep fracture outflow. Others suggest the lakes are simply responding to a drier climate, serving as the canary in the broader climate-change ‘coal mine’.

ANSTO has applied recurrent isotopic and chemical monitoring of the lakes and adjacent groundwater over two years to unravel some of the mystery of their recent water losses.  Each lake behaved uniquely, but they shared some common trends. Steady enrichment of stable water isotopes, 2H and 18O, indicates the dominance of evaporation, with minimal losses to groundwater or through transpiration. Lake Cl/Br ratios were very low and clustered in three groups, two trending away from initial ratios indicative of groundwater input. 3H and 14C show recent rainfall and/or runoff as the main contributors to lake waters, with apparent ages in the adjacent shallow groundwater up to several decades. High levels of 222Rn from shallow bores suggest a close association between the peats enclosing the lakes and 238 U from ancient erosion, or proximity of an underlying shale lens. The only deep piezometer (72-84 m) near the lakes showed negligible contributions from the lakes or recent surface water.

The trends in isotopic and chemical parameters infer that evaporation is sufficient to explain recent water losses from most of these perched lakes. Trends in some lakes hint that these had previous inputs from groundwater. While the historical variability of groundwater input to the lakes remains unknown, there is no current evidence of major losses to groundwater. Thirlmere Lakes will exist only intermittently under dry climate conditions.