PFAS migration in groundwater – hydrogeological assessment and long-term modelling of plume evolution to inform environmental management options ASLAN PERWICK – PATTLE DELAMORE PARTNERS LTD THANK YOU TO MANY OTHERS – NERENA RHODES, ANDREW RUMSBY, JAMES CONWAY, ALAN PATTLE, HAMISH WILSON, AMBER SIMMONDS, MANY MORE
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PFAS migration in groundwater –hydrogeological assessment and long-term modelling of plume evolutionto inform environmental management options
ASLAN PERWICK – PATTLE DELAMORE PARTNERS LTD
THANK YOU TO MANY OTHERS – NERENA RHODES, ANDREW RUMSBY, JAMES CONWAY, ALAN PATTLE, HAMISH WILSON, AMBER SIMMONDS, MANY MORE
Scope
• Understanding long-term fate & transport of key PFAS compounds in groundwater – why the need?
• Existing Plume – what is the situation?
• Plume predictions are needed - How could such a task be approached?
• The predictions and what do they mean?
• What are the learnings?
• What are the limitations?
PFAS Fate & Transport –Why the need to understand?
• PFAS compounds can have long residence times within the environment – risks could require long-term management.
• Leaching of source mass from the Source Zones (Soil) can continue for many decades – risk could require long-term management.
• Ultimately – a basis for Environmental Risk Management & decision making.
PFAS Fate & Transport –Present Situation
• PFAS use started on the site in the 1970s, continued for circa 35-yrs.
• Large existing PFOS+PFHxS Plume (the focus of this study)
• PFOS + PFHxS use has ceased within the last decade
• Area of PFOS + PFHxS >0.07 ug/L –likely greater than 1000 ha
PFAS Fate & Transport –How did we get here?
• Only 2-years of time-series data available –little data available for trend analysis
• Estimate that surface water system is a key migration method
• Plume estimated to have advanced quickly along key surface water routes, due to PFAS surface run-off.
• Gradual PFAS soil leaching to groundwater, and then advection and growth of a groundwater plume
• Highly dispersive hydrogeology, but layered, and numerous private groundwater takes
PFAS Fate & Transport – 3D Prediction of Plume Evolution: 1970s to Today
Prediction Summary:• The existing plume extent is large, and is likely to remain large for multiple
decades, before a gradual depletion over multiple more decades.
• Existing plume mass is likely to increase before a gradual depletion over multiple decades.
• Key receptors are interpreted to be surface water bodies, and these largely constrain the ultimate extent of the plume
• Shallow groundwater bores downgradient of the existing plume will likely require risk management measures in the future
Learnings:• Multi-disciplinary input needed when attempting a PFAS groundwater
assessment of this scale and complexity.
• Surface water transport route, and SW-GW pathway, a key migration method for this site (and likely others).
• Even with numerous uncertainties, 5D modelling (X,Y,Z, Time, Conc.) can still provide a useful basis to assist with decision making / risk management approach e.g. likelihood of risk or not?, understanding big-picture trends, null-hypothesis testing …
Limitations:
• For more certainty/refinement of predictions, some more field data would be needed e.g. Additional time-series, aerial delineation, and vertical delineation.
• PFAS compounds are tricky devils – behavior & chemical transformations in the sub-surface are not fully understood, could be significant.
• Soil source zone concentrations and depletion rates need to be estimated –underlying limitation
• Dealing with nanograms! PFAS sampling & analysis can show large variation between sampling rounds
• Many More!
Thank You & Questions
PFAS Fate & Transport – Predicted Plume Mass Evolution:
• 50-yr half-life source depletion predicted contaminant mass
PFAS Fate & Transport – 3D Geology Model:
• Constructed from Regional Council borehole database records