PFAS are everywhere. More than 4,000 man-made chemicals, used since the 1940s, have found their way into soil, water and even the North Pole.
They are synthetic compounds found in everything from firefighting foam to non-stick cookware and water-proof fabrics. As outlined in the GHD Navigating PFAS Webinar Series - hosted by geochemist Mailyng Aviles - PFAS are valued in industrial and consumer applications for their unique water, oil and heat-resistant properties.
Their carbon-fluorine bonds are strong and the size of fluoride ion limits access to attack the bond, making them highly resistant to degradation and earning them the label “forever chemicals.” The most studied compounds - perfluorooctanoic acid (PFOA) and perfluorooctane sulfonate (PFOS) - have been linked to a range of environmental and human health concerns. Dietary intake is the primary exposure route for most people, as these compounds enter food chains through contaminated soil and water.
Managing PFAS is complex. Criteria for safe concentrations keep dropping, making compliance a moving target. In Australia, drinking water limits have fallen from 70 nanograms per litre to just 8 for PFOS, after the US EPA adjusted their criteria. While natural systems can slowly depurate PFAS, the key driver of risk remains the mass entering the environment.
Mass flux reframes the challenge. Instead of just measuring PFAS concentrations at a compliance point in a regulatory setting where the compliance criteria are evolving, it asks how much is moving, where it is going and how fast. Mass flux is the amount of contaminant passing through a unit area over time, expressed in grams per square metre per day. It helps to understand the rate of contaminant transport at specific locations. Mass discharge is the total mass flowing through a cross-section, measured in grams over a defined unit of time such as grams per day. It is important to understand both parameters as one provides information on the speed of response actions required and the other at how much mass has to be dealt with over the long term respectively.
In simple terms, mass flux (J) equals groundwater flux (Q) times contaminant concentration (C): J = Q × C. Mass discharge is mass flux multiplied by the cross-sectional area.
Understanding these concepts is the first step to tracking PFAS, targeting interventions and demonstrating real progress.