Quantification of biodegradation for o-xylene and naphthalene using first
order decay models, Michaelis–Menten kinetics and stable carbon isotopes
Philipp Blum
a,
⁎, Daniel Hunkeler
b
, Matthias Weede
c
, Christof Beyer
a,d
, Peter Grathwohl
a
,
Barbara Morasch
b,e
a
University of Tübingen, Center for Applied Geoscience (ZAG), Sigwartstrasse 10, 72076 Tübingen, Germany
b
University of Neuchâtel, Centre for Hydrogeology, Rue Emile-Argand 11, 2009 Neuchâtel, Switzerland
c
URS Deutschland GmbH, Sutelstrasse 2, 30659 Hannover, Germany
d
University of Kiel, Institute of Geosciences, Ludewig-Meyn-Str.10, 24118 Kiel, Germany
e
Environmental Chemistry Laboratory (LCE), EPFL - ENAC - ISTE, Station 2, 1015 Lausanne, Switzerland
article info abstract
Article history:
Received 8 February 2008
Received in revised form 11 November 2008
Accepted 30 November 2008
Available online 14 December 2008
At a former wood preservation plant severely contaminated with coal tar oil, in situ bulk
attenuation and biodegradation rate constants for several monoaromatic (BTEX) and
polyaromatic hydrocarbons (PAH) were determined using (1) classical first order decay
models, (2) Michaelis–Menten degradation kinetics (MM), and (3) stable carbon isotopes, for o-
xylene and naphthalene. The first order bulk attenuation rate constant for o-xylene was
calculated to be 0.0025 d
- 1
and a novel stable isotope-based first order model, which also
accounted for the respective redox conditions, resulted in a slightly smaller biodegradation rate
constant of 0.0019 d
- 1
. Based on MM-kinetics, the o-xylene concentration decreased with a
maximum rate of k
max
=0.1 μg/L/d. The bulk attenuation rate constant of naphthalene retrieved
from the classical first order decay model was 0.0038 d
- 1
. The stable isotope-based
biodegradation rate constant of 0.0027 d
- 1
was smaller in the reduced zone, while residual
naphthalene in the oxic part of the plume further downgradient was degraded at a higher rate of
0.0038 d
- 1
. With MM-kinetics a maximum degradation rate of k
max
= 12 μg/L/d was determined.
Although best fits were obtained by MM-kinetics, we consider the carbon stable isotope-based
approach more appropriate as it is specific for biodegradation (not overall attenuation) and at
the same time accounts for the dominant electron-accepting process. For o-xylene a field based
isotope enrichment factor ε
field
of - 1.4 could be determined using the Rayleigh model, which
closely matched values from laboratory studies of o-xylene degradation under sulfate-reducing
conditions.
© 2008 Elsevier B.V. All rights reserved.
Keywords:
Natural attenuation
Redox zones
Contaminant Plume
Compound-specific isotope analysis (CSIA)
Rate constants
Polyaromatic hydrocarbons (PAH)
BTEX
1. Introduction
Active remediation techniques such as pump-and-treat or
excavation are economically not feasible for the large number
of soil and groundwater contaminations existing worldwide.
Monitored natural attenuation (MNA) as a passive remedia-
tion strategy is considered a worthwhile alternative. Numer-
ous studies have shown that natural attenuation (NA)
processes (e.g. dilution, sorption, dispersion, (bio-) degrada-
tion) have the potential to manage groundwater contamina-
tion at many sites (e.g. Rice et al., 1995; Mace et al., 1997;
Grathwohl et al., 2000), which becomes evident in the
observation that many dissolved contaminant plumes are
not expanding any more. In recent years, short and steady
state contaminant plumes are becoming increasingly toler-
ated and MNA is implemented as a remediation strategy in
the United States and in Europe when no receptor is at risk
(NRC, 1999; Rügner et al., 2006). (Bio-)Degradation deserves
special attention, because, out of all NA processes in ground-
water, it is the only one substantially effective in removing
contaminants from the environment for many compound
Journal of Contaminant Hydrology 105 (2009) 118–130
⁎ Corresponding author. Tel.: +49 7071 29 73170; fax: +49 70715059.
E-mail address: philipp.blum@uni-tuebingen.de (P. Blum).
0169-7722/$ – see front matter © 2008 Elsevier B.V. All rights reserved.
doi:10.1016/j.jconhyd.2008.11.009
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