Per- and polyfluoroalkyl substances,
and other chemicals in aqueous
fire-fighting foam (AFFF), accumulate at air–water interfaces
in the vadose zone, reducing interfacial tension and potentially causing
tension-driven flow (TDF). This study investigates the importance
of TDF on AFFF lateral spreading in the vadose zone using bench-scale
column experiments and numerical modeling. Understanding AFFF spreading
beyond an original spill footprint would enhance site conceptual models,
wherein understanding the contaminant source zone is critical. Our
experiments demonstrate that AFFF exhibits noteworthy TDF, characterized
by substantial lateral water flow and AFFF spreading, causing variations
in moisture content, which alters capillary pressure and hydraulic
conductivity. The modified HYDRUS model accurately simulated experiments
and was then used to simulate site-scale AFFF source zone dynamics.
The numerical investigation demonstrated that TDF could lead to a
significant increase in the surface footprint of an AFFF source zone,
where wetter conditions yield a 6-fold increase compared to an initial
spill, while drier soils exhibit a 4-fold expansion. The footprint
expansion occurs over decades, which is highly relevant for our conceptual
understanding of both historic and relatively new AFFF spills. This
study highlights that the lateral flow of AFFF due to TDF is an important
transport mechanism that controls the AFFF source zone.