Applied numerical modeling of saturated / unsaturated flow and ...
Applied numerical modeling of saturated / unsaturated flow and ...
Applied numerical modeling of saturated / unsaturated flow and ...
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Uncertainty assessment <strong>of</strong> contaminant plume length<br />
estimates in heterogeneous aquifers<br />
Abstract<br />
Journal <strong>of</strong> Contaminant Hydrology 87 (2006) 73–95<br />
Christ<strong>of</strong> Beyer ⁎ , Sebastian Bauer, Olaf Kolditz<br />
www.elsevier.com/locate/jconhyd<br />
Center for <strong>Applied</strong> Geoscience, University <strong>of</strong> Tübingen, Sigwartstraße 10, D 72076 Tübingen, Germany<br />
Received 4 November 2005; received in revised form 14 April 2006; accepted 25 April 2006<br />
Available online 16 June 2006<br />
The Virtual Aquifer approach is used in this study to assess the uncertainty involved in the estimation <strong>of</strong><br />
contaminant plume lengths in heterogeneous aquifers. Contaminant plumes in heterogeneous twodimensional<br />
conductivity fields <strong>and</strong> subject to first order <strong>and</strong> Michaelis–Menten (MM) degradation kinetics<br />
are investigated by the center line method. First order degradation rates <strong>and</strong> plume lengths are estimated<br />
from point information obtained along the plume center line. Results from a Monte-Carlo investigation<br />
show that the estimated rate constant is highly uncertain <strong>and</strong> biased towards overly high values. Uncertainty<br />
<strong>and</strong> bias amplify with increasing heterogeneity up to maximum values <strong>of</strong> one order <strong>of</strong> magnitude.<br />
Calculated plume lengths reflect this uncertainty <strong>and</strong> bias. On average, plume lengths are estimated to about<br />
50% <strong>of</strong> the true plume length. When plumes subject to MM degradation kinetics are investigated by using a<br />
first order rate law, an additional error is introduced <strong>and</strong> uncertainty as well as bias increase, causing plume<br />
length estimates to be less than 40% <strong>of</strong> the true length. For plumes with MM degradation kinetics,<br />
therefore, a regression approach is used which allows the determination <strong>of</strong> the MM parameters from center<br />
line data. Rate parameters are overestimated by a factor <strong>of</strong> two on average, while plume length estimates are<br />
about 80% <strong>of</strong> the true length. Plume lengths calculated using the MM parameters are thus closer to the<br />
correct length, as compared to the first order approximation. This approach is therefore recommended if<br />
field data collected along the center line <strong>of</strong> a plume give evidence <strong>of</strong> MM kinetics.<br />
© 2006 Elsevier B.V. All rights reserved.<br />
Keywords: Natural Attenuation; Heterogeneity; Plume length; Center line method; Uncertainty analysis; Monte-Carlo;<br />
Numerical modelling<br />
⁎ Corresponding author. Tel.: +49 7071 29 73176; fax: +49 7071 5059.<br />
E-mail address: christ<strong>of</strong>.beyer@uni-tuebingen.de (C. Beyer).<br />
0169-7722/$ - see front matter © 2006 Elsevier B.V. All rights reserved.<br />
doi:10.1016/j.jconhyd.2006.04.006