Glyphosate, an ionizable organic herbicide, is frequently
detected
in soils and groundwater globally despite its strong retention via
sorption. Understanding its apparent mobility hinges on our ability
to quantify its system-specific sorption behavior, hindered by its
affinity to adsorb onto sediments, yielding very low aqueous concentrations.
Here, we present findings from a saturated flow-through column experiment
in which we monitored glyphosate sorption onto a natural calcareous
aquifer sediment, using the noninvasive geophysical method spectral
induced polarization (SIP). Our kinetic sorption reactive transport
model predicted the strong nonlinear reversible retention of glyphosate
and reproduced the spatial profile of retained glyphosate in the sediment,
with a measured maximum of 0.06 mg g–1. The strong
contribution of sorption to pore fluid conduction masked the expected
variations in imaginary conductivity, σ″. However, time
constants derived from a Cole–Cole model matched the timing
and spatial distribution of model-predicted sorbed concentration changes,
increasing from 0.8 × 10–3 to 1.7 × 10–3 s with an increase in sorbed glyphosate of 0.1 mg
g–1. Thus, glyphosate sorption modified the surface
charging properties of the sediment proportional to the solid-bound
concentrations. Our findings link SIP signal variations to sorption
dynamics and provide a framework for improved monitoring of charged
organic contaminants in natural sediments.