Manipulating the retention of unfrozen
water in freezing contaminated
soil to achieve prolonged bioremediation in cold climates remains
unformulated. This freezing-induced biodegradation experiment shows
how nutrient and zeolite amendments affect unfrozen water retention
and hydrocarbon biodegradation in field-aged, petroleum-contaminated
soils undergoing seasonal freezing. During soil freezing at a site-specific
rate (4 to −10 °C and −0.2 °C/d), the effect
of nutrients was predominant during early freezing (4 to −5
°C), alleviating the abrupt soil-freezing stress near the freezing-point
depressions, elevating alkB1 gene-harboring populations,
and enhancing hydrocarbon biodegradation. Subsequently, the effect
of increased unfrozen water retention associated with added zeolite
surface areas was critical in extending hydrocarbon biodegradation
to the frozen phase (−5 to −10 °C). A series of
soil-freezing characteristic curves with empirical α-values
(soil-freezing index) were constructed for the tested soils and shown
alongside representative curves for clays to sands, indicating correlations
between α-values and nutrient concentrations (soil electrical
conductivity), zeolite addition (surface area), and hydrocarbon biodegradation.
Heavier hydrocarbons (F3: C16–C34) notably biodegraded in all
treated soils (22–37% removal), as confirmed by biomarker-based
analyses (17α(H),21β(H)-hopane), whereas lighter hydrocarbons
were not biodegraded. Below 0 °C, finer-grained soils (high α-values)
can be biostimulated more readily than coarser-grained soils (low
α-values).