Ajc. Sinke et al., EFFECTS OF A FLUCTUATING WATER-TABLE - COLUMN STUDY ON REDOX DYNAMICSAND FATE OF SOME ORGANIC POLLUTANTS, Journal of contaminant hydrology, 33(1-2), 1998, pp. 231-246
Citations number
31
Categorie Soggetti
Water Resources","Environmental Sciences","Geosciences, Interdisciplinary
The development of the redox conditions has been studied in an initial
ly aerobic column filled with quartz sand coated with ferrihydrite and
subjected to a fluctuating water table. The purpose of this study was
to evaluate the effect of water table fluctuations on the redox dynam
ics and the fate of selected organic pollutants. The column that was p
ercolated continuously with electron accepters (O-2, NO3, SO4) and ele
ctron donors (acetate and formate), was first operated under saturated
conditions resulting in the classical redox zonation. After 4 months
of operation, we started to fluctuate the water level and three draina
ge-imbibition cycles were run each with a total cycle length of 1 mont
h. The pulse of oxygen introduced by lowering the water table caused a
partial and temporal oxidation of previously reduced species. To inve
stigate the effect of the changing redox environment on the transport
and transformation of organic pollutants, breakthrough experiments wer
e performed with 4-nitrobenzoate and toluene as model pollutants repre
sentative for nitro-substituted and volatile aromatics, respectively.
The fate of 4-nitrobenzoate and toluene was studied under saturated co
nditions in short pulse breakthrough experiments and evaluated using t
he advection-dispersion model. 4-nitrobenzoate was transformed stoichi
ometrically into 4-aminobenzoate caused by the reduction of the nitrog
roup. The transformation rate varied with depth and with time, droppin
g from 15.3 nmol g(-1) h(-1) after the first drainage-imbibition cycle
to 1.5 nmol g(-1) h(-1) after 4 additional months of operation. Tolue
ne was not degraded during the first breakthrough experiment and showe
d a retardation factor of 2.06 which was ascribed to diffusion into en
trapped air, originating from drainage-imbibition cycles, and to sorpt
ion to biomass. After the 24-h pre-exposure to toluene, adaptation had
occurred and in later experiments toluene was degraded within the fir
st 6 cm. These data show that in an experiment that was well-described
in terms of water flow, gas flow, and initial mineral phase compositi
on, the microbial processes induced a chemical and physical heterogene
ity. An additional heterogeneity in space and time was introduced by t
he fluctuating water table. The 'history' of the column had consequenc
es for the fate of organic pollutants and resulted in an unpredictable
behaviour with respect to their transformation, transport and degrada
tion. (C) 1998 Elsevier Science B.V. All rights reserved.