Contamination of groundwater with pharmaceutical active
compounds
(PhACs) increased over the last decades. Potential pathways of PhACs
to groundwater include techniques such as irrigation, managed aquifer
recharge, or bank filtration as well as natural processes such as
losing streams of PhACs-loaded source waters. Usually, these systems
are characterized by redox-active zones, where microorganisms grow
and become immobilized by the formation of biofilms, structures that
colonize the pore space and decrease the infiltration capacities,
a phenomenon known as bioclogging. The goal of this work is to gain
a deeper understanding of the influence of soil biofilms on hydraulic
conductivity reduction and the fate of PhACs in the subsurface. For
this purpose, we selected three PhACs with different physicochemical
properties (carbamazepine, diclofenac, and metoprolol) and performed
batch and column experiments using a natural soil, as it is and with
the organic matter removed, under different biological conditions.
We observed enhanced sorption and biodegradation for all PhACs in
the system with higher biological activity. Bioclogging was more prevalent
in the absence of organic matter. Our results differ from works using
artificial porous media and thus reveal the importance of utilizing
natural soils with organic matter in studies designed to assess the
role of soil biofilms in bioclogging and the fate of PhACs in soils.