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Calculation and Use of First-Order Rate Constants for Monitored ...

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Appendix I. Uncertainty in <strong>Rate</strong> <strong>Calculation</strong>sUsing Statistics to Estimate the Time Frame toAchieve Remediation ObjectivesAs with any remediation method, one <strong>of</strong> the fundamental questionsthat arises is “How much time will be required be<strong>for</strong>e remediationobjectives are achieved?” At the current state <strong>of</strong> practice, theonly practical approach available uses a statistical analysis <strong>of</strong>long-term monitoring data from wells in the source area <strong>of</strong> thecontaminant plume. Many practitioners will calculate the Pearsonproduct moment correlation coefficient (R 2 ) <strong>for</strong> the regression usedto extract the Point Decay <strong>Rate</strong> constant (k point). If the coefficientis near one (e.g., greater than 0.9 or 0.95), the regression isaccepted as being useful in a qualitative way. There are twoproblems with this approach; it does not allow the user to select alevel <strong>of</strong> confidence <strong>for</strong> the comparison, <strong>and</strong> it does not give morevalidity to regressions with many points compared to regressionswith only a few points.The slope <strong>of</strong> the regression is the rate constant. A better approachis to calculate a confidence interval on the slope <strong>of</strong> the regression.The following data from Kolhatkar et al., 2000 will be used toillustrate this approach. They collected long-term ground-watermonitoring data from three wells at a gasoline release site in NewJersey. Their original data displayed extreme oscillations withconcentrations bouncing from a high value down to the analyticaldetection limit <strong>of</strong> 1µg/L, <strong>and</strong> then back to a high value oversequential sampling intervals. Although the scatter in the dataset is typical <strong>of</strong> the variation seen at many other sites, the influence<strong>of</strong> these outliers on the statistical estimate <strong>of</strong> the rate <strong>of</strong> attenuationwas removed by editing the data set to remove those points wherethe concentration <strong>of</strong> MTBE was less than the detection limit.Table I-1. Sources <strong>of</strong> Uncertainty in Calculated <strong>Rate</strong> <strong>Constants</strong>Type <strong>of</strong> Uncertainty Applies to Type <strong>of</strong> Effect Ways to ManageMonitoring WellLocation(horizontal <strong>and</strong>vertical location)Seasonal EffectsSeepage VelocityEstimatePoint Decay <strong>Rate</strong> (k point)Bulk Attenuation <strong>Rate</strong>Constant (k )Biodegradation <strong>Rate</strong>Constant (λ)Point Decay <strong>Rate</strong> (k point)Bulk Attenuation <strong>Rate</strong>Constant (k )Biodegradation <strong>Rate</strong>Constant (λ)Bulk Attenuation <strong>Rate</strong>Constant (k )Wells not in strongest source area maynot give repres entative indication <strong>of</strong> howlong entire plume will persist.Wells not on centerline <strong>of</strong> plume can givemis leading indications aboutconcentration pr<strong>of</strong>ile in plume.A poorly des igned monitoring wellnetwork may give misleading in<strong>for</strong>mationabout source s trength, source size, <strong>and</strong>centerline plume concentrations used <strong>for</strong>calibration.Can introduce additional s catter in dataus ed to develop k pointrate c ons tant.Ty pically not a problem as all data arecollected at the same time.Can be a problem if seas onal effects aresignificant <strong>and</strong> the data used <strong>for</strong>calibration are not c ollec ted(concentration vs. distance) at the sametime.Increases ov erall uncertainty incalculation.Characterize source with several wells.Estimate <strong>and</strong> report uncertainty in final result(estimated time to reach clean-up s t<strong>and</strong>ards ).Us e a well-designed monitoring well networkwith transects <strong>of</strong> wells in rows across theplume rather than one set <strong>of</strong> wells down theinferred centerline. Estimate <strong>and</strong> reportunc ertainty in final res ult (es timated plumelength).The source <strong>and</strong> plume need to be wellc haracterized to ensure representativemodeling res ults . Per<strong>for</strong>m sensitivity analysison model.Addres s as part <strong>of</strong> an uncertainty calculation(s ee below). For s trong seasonal effects, use<strong>of</strong> data from the same season c an bec onsidered.Not applicable.For strong seasonal effects, use data froms ame s eas on to help ensure representativ emodeling res ults . Per<strong>for</strong>m sensitivity analysison model.Average results from multiple seepageestimates along plume centerline. Improv eseepage velocity estimate. Estimate <strong>and</strong>report uncertainty in final result (estimatedplume length).PlumeHeterogeneityAll rate constantc alc ulationsIncreases apparent uncertainty.<strong>Use</strong> worst-case data. <strong>Use</strong> transects toc apture plume heterogeneity. For regressionbased rate cons tants (k <strong>and</strong> k point), estimate<strong>and</strong> report uncertainty in final result. Formodeling studies designed to determine λ,per<strong>for</strong>m sensitivity analy sis on model byc hanging k ey variables to their upper <strong>and</strong>lower expected range <strong>and</strong> evaluate howmodeling res ults c hange.12

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