flux-based dnapl site - us epa · • linda abriola, tufts university • charles werth, university...
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1 Office of Research and DevelopmentNational Risk Management Research Laboratory, Ground Water and Ecosystems Restoration Division, Ada, Oklahoma
Flux-Based DNAPL SiteAssessment & Remediation:Overview of ConceptsSuresh Rao, School of Civil Engineering, Purdue University
Triad Conference – June 10, 2008
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Control Plane
z
y
x
nJ
q0
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Without Whom this Wouldn’t be Possible!
• Nandita Basu & Irene Poyer, Purdue University• Michael Annable, Kirk Hatfield & James Jawitz
University of Florida• Lynn Wood & Michael Brooks, US EPA-Ada• Ronald Falta, Clemson University• J. Christ, US Air Force Academy• Linda Abriola, Tufts University• Charles Werth, University of Illinois-Urbana/Champaign• Greg Davis, Colin Johnston & Brad Patterson,
CSIRO-Perth• Ravi Naidu, Megh Mallavarupu & Subhas Nandy
CRC-CARE & University of South Australia
Hill AFB 1994-1996; Dover AFB 1997-1999Rao et al. (WRR, 1997); Jawitz et al. (EST, 1998); McCray and Brusseau (EST, 1998); Falta et al. (WRR, 1999); Brooks et al. (JCH, 2004); Childs et al. (JCH, 2006)Sages (FL) 1998; Bachman Road (MI) 2000Jawitz et al. (EST, 2000); Mravik et al. (EST, 2003); Ramsburg et al. (EST, 2005)
Partial source removal debate: TheorySale and McWhorter (WRR, 2001); Rao and Jawitz (WRR, 2003); Parker and Park (WRR, 2004); Jawitz et al. (WRR, 2005)Partial source removal and flux: Lab and field dataFure et al. (JCH, 2006); Basu et al. (WRR, 2008 in press); Basu et al. (JCH, 2008 in press); Kaye et al. (JCH, 2008 in press); Chen and Jawitz (EST, in review 2007); Brooks et al. (In review, JCH, 2007)
A Decade+ of ProgressDNAPL Site Investigations
1995
1997
2005
2001
1999
2007
2003
2009
Can’t find it!
Can’t deplete it!
No benefit!
Back Diffusion!
Flux-based Assessment & Management?
Frequently Asked Questions• How much data needed before remediation?• What types of data best serve CSM & design?• Are high costs justified in terms of reduced
uncertainty?• What are the short-term benefits of source clean
up? • What is the likely plume response to source
clean up?• How to select target (interim) endpoints?• How to determine long-term stewardship needs?• Is there a simplified modeling & decision
framework?• How does all this fit into the TRIAD framework?
Pump & Treat Wells orInterception Trench or
Stream etc.E(t)
Source Control PlaneMd (t)
Source MassM0 and Mnow
Plume Mass(Parent + Products)
Mp (t) & λ(t)
DNAPL Site Monitoring:Enhancing Archived Site Data
PlumeControl Plane
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Contaminant Fluxes & Mass Discharge at Control Planes
Md = Σ Ji Ai
Ji = Local mass flux (ML2T-1)qi = Local Darcy flux (LT-1)Ci = Local conc. (ML-3)Ai = Area of element i (L2)Md = Source strength (MT-1)Ks = Satd. Hyd. Cond (LT-1)j = Hydraulic gradient (-)
Ji = qi Ciqi =-Ks j
i
Control Plane (CP)
Δx
Δz
Ai = Δx Δz
Control plane area should be just large enough to completely inscribe the dissolved plume width
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Cleanup to the Extent Necessary(CUTEN or Q10)
Source StrengthSource LongevityDegradation Rate Receptor Loading
⎟⎠⎞
⎜⎝⎛ −=
vxMM CPCP
λexp)1()2(
Measured mass fluxesat control cross-sectionsPumping tests
ResidualNAPL-phase
Q, C(t)
mass flux
C
t
C
t
Mea
sure
men
ts(f
ield
scal
e)Fi
eld
site
Q, C(t)
Comparisson andInterpretation
Control
Plane I
flux 1
Control
Plane II
flux 2
Key measures for:Site characterizationRemediation design &Performance Assessment
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Contaminant Mass Discharge Estimates
What We HaveTemporal Data
Concentration in select source zone monitoring wells over time
Spatial Data
1. Mass discharge at the source control plane at a point in time
2. Plume Mass
What We NeedSource Longevity (Source Strength Function)
- present source mass
- source depletion behavior
Source & Flux Distribution (Source Architecture)
- identification of hotspots, targeted treatment
Characterization of DNAPL Sources
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Source Depletion
First-Order
Linear
Constant
Newell et al., 2006, Jour. Env. Eng.Suarez et al., 2004, Remediation.
Γ = 0
Γ=1
Γ = 0.5
where,
Cs(t) and C0 =
flux-avg. conc. at source CP at time = t; and t=0
M0 = initial source mass
Vd = Darcy flux
A = Source CP Area
Γ = empirical constant
Simple Cases
0( )sC t C=
Falta et al. 2005a
Source Mass Estimation
( ) ,0,0
0
exp DD D
MM t M t
M⎛ ⎞
= −⎜ ⎟⎝ ⎠
First-Order
Γ=1
Fit monitoring well data to standard functions to estimate a value of Γ
( ) ,0,0
00
expt
DP D
MM t M t dt
M⎛ ⎞
= −⎜ ⎟⎝ ⎠
∫
Two equations and two unknowns –solve for MD,0 and M0
Estimate present source mass using
,00
0
exp Dt now
MM M t
M=
⎛ ⎞= −⎜ ⎟
⎝ ⎠
Method A: Requires only MW data
1. Monitoring well data over time fitted with an exponential to estimate k.
2. Now,
3. Here, a = time from which sampling data available
4. Thus:
/t a d t aM V AC k= ==
Method B: Requires mass discharge (MD) and plume mass (MP)
( )expt now t a dM M kt= == −
Source Mass Reduction
Dover AFB Florida Study
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Sages Drycleaner
Site
Hill AFB OU-2
Dover AFBClemson Study
Dover AFB OU
Sour
ce F
lux
Red
uctio
n0 0.2 0.4 0.6 0.8 1
Falta et al., 2005
Exponent Γ is a function of DNAPL source architecture, hydrogeologic heterogeneity & correlation between the two.
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Source Mass Reduction
Sour
ce F
lux
Red
uctio
n
2ln 0.1kσ =
2ln 1kσ =2ln 3kσ =
Brusseau et al. 2008
Basu et al. 2008
UTCHEM Simulations
Source Mass & Source Strength
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Source Zone ArchitectureEulerian Approach
Reactive Travel Times
•Source zone conceptualized as a network of stream tubes, each characterized by velocity (travel time) and NAPL saturation.
•The domain described by mean and variance of travel time and NAPL saturation distribution, measured by non-reactive and reactive tracers, respectively.
•The measured parameters are used to predict change in the mean contaminant flux in time over the source control plane
Source Zone ArchitectureLagrangian Approach
Source Depletion Dynamics:
Decreasing GTP
Increasing Dissolution
Suchomel & Pennell, ES&T, 2006
Surfactant Flushing in 2-D Flow Chambers
M0 = Initial Mass of NAPL, κ0
β2 = Mass Depletion ExponentDamkohler
Model(Parker and Park 2005)
M0 – Initial Mass of NAPLβ - Variability Index
Power Law Model
(Zhu and Sykes 2005)
μlnτ= Mean of Hydrodynamic Field and DNAPL Architectureσlnτ= Variability of Hydrodynamic Field and DNAPL Architecture
Streamtube Model
(Jawitz et al. 2005)
Simplified Source Depletion Models
Basu et al., 2006, JCH
ln
ln
( ) ln1 1 erf2 2 2
f
c s
C T Tf C
τ
τ
μσ
⎡ ⎤−= − ⎢ ⎥
⎣ ⎦
( ) ( )
s o
f
c
C T M Tf C M
β⎡ ⎤
= ⎢ ⎥⎣ ⎦
2( ) ( )1 exp o
s o
f
s
C T L M TC K M
βκ⎡ ⎤⎛ ⎞⎛ ⎞
⎢ ⎥= − −⎜ ⎟⎜ ⎟⎢ ⎥⎝ ⎠⎝ ⎠⎣ ⎦
Cf(T) = f (HS, DS)Cf(T) = Flux-avg. Concentration
at Source Control PlaneHS = Hydrodynamic StructureDS = DNAPL Structure
Dissolution Profile Fitted to Source Depletion Models
ConclusionAll source depletion models fitdissolution behavior effectively
BUT, can we estimate parameters of any of these models independently and predict the dissolution profile apriori?
- YES, the streamtube model can be parameterized using tracer tests –
Power Function Model
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pore volumes
Cf/C
s
αNRMSD = 0.015
Damkohler Model
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0.25
0.5
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pore volumes
Cf/C
s
κ0, β2NRMSD = 0.017
Basu et al., JCH, 2008
Streamtube Model
0
0.25
0.5
0 5 10 15 20 25 30
pore volumes
Cf/C
s
UTCHEM output
Model Fit
μlnτ, σlnτNRMSD = 0.007
Predicting Source Depletion:Simplified Models
GTP can be measured in lab. Field methods need to be developed.Tracer tests for calibrating stream-tube modeling demonstrated at lab & field scales.Eulerian vs. Lagrangian approaches, $$$!!!Γ=1 may be an adequate approximation??
Basu et al., WRR 2008
A
Sn (x,y,z; t)
Spatially Distributed vs. Integrated Parameters
Transition from local parameters (Sn, K, C) to integrated system behavior [J(g/m2/day); MD (g/day)]
J = contaminant mass flux (g/m2/day)q = groundwater flux (cm/day)C = dissolved concentration (mg/L)
J (y,z;t) =
q(y,z;t) C(z,y;t)
MD (g/day)= mass discharge = J d A∫
Relationship between mean values:
Total DNAPL mass [m(t)] & Source Strength [MD(t)]
Source Mass & Flux Distributions
• How does source mass change with time? • How does the flux distribution change?
0
5
1 0
1 5
z
5
1 0
1 5
2 0
2 5
x1 0
2 0
y
XY
Zp e rm1 .0 E -1 04 .6 E -1 12 .2 E -1 11 .0 E -1 14 .6 E -1 22 .2 E -1 21 .0 E -1 24 .6 E -1 32 .2 E -1 31 .0 E -1 3
x
5
10
15
20
25
y
5
10
15
20
25
z
0
5
10
15
XY
ZSn
0.160.140.120.100.080.060.040.02
T2VOC Numerical Simulations
Basu et al. JCH, 2008
Flux Statistics at Source Control Plane
0
0.5
1
1.5
2
2.5
3
0 10 20 30 40 50
Time (years)
Flux
Mea
n an
d St
anda
rd D
evia
tion
(g/m
2/da
y) Mean Flux (Positive Correlation)
Mean Flux (Negative Correlation)
Sigma Flux (Positive Correlation)
Sigma Flux (Negative Correlation)
Both mean and standard deviation of contaminant flux distribution decrease with mass depletion from DNAPL source
Basu et al. JCH, 2008
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Flux Statistics at Source Control Plane
Numerical simulations are for emplaced NAPL.
Will this be also valid for spills?
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0.2
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1
0 0.2 0.4 0.6 0.8 1
Reduction in Flux Mean
Red
uctio
n in
Flu
x St
d. D
evia
tion
Domain 1 (Case 1) - variance(ln k) = 1Domain 1 (Case 2) - variance(ln k) = 2.45Domain 1 (Case 3) - variance (ln k) = 1Domain 2 (Case 1) - variance (ln k) = 2.45Domain 2 (Case 2) - variance (ln k) = 2.45Hill AFB, Utah
coefficient of variation = σ/μ = constant
Basu et al. JCH 2008
DNAPL Spill & Dissolution Simulations:Evolution of Source Architecture
Simulation data provided courtesy of:
J A Christ (USAFCE) &
L M Abriola (Tufts University)
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0.2
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1
0 0.2 0.4 0.6 0.8 1
Reduction in Flux Mean
Red
uct
ion
in F
lux
Sta
nd
ard
Dev
iati
on
Red lines represent variance ln k =1Black lines represent variance ln k = 0.29
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0.8
1
0 0.2 0.4 0.6 0.8 1
Reduction in Sn mean
Red
uct
ion
in S
n s
tan
dard
dev
iati
on Red lines represent variance ln k =1Black lines represent variance ln k = 0.29
DNAPL Mass Contaminant FluxBasu et al. JCH 2009?
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Temporal Evolution OfSource & Flux Centroids
Flux Center of Mass
0
1
2
3
4
5
6
7
0 20 40 60 80 100
Mass Removed (%)
Cen
ter
of M
ass
(m
)
y_barz_bar
Saturation Center of Mass
0
1
2
3
4
5
6
7
0 20 40 60 80 100
Mass Removed (%)
Ce
nte
r of M
ass
(m
)
z_bar
x_bary_bar
Source Mass Contaminant FluxBasu et al. JCH 2009?
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Lab Data: Flux Architecture Dynamics
Flow-cell top
Inlet chamber flush port
Water outlets
Water inlet
Brass screen
Inlet chamber
Outlet chamber
NAPL injection port
B1B2
B3M1
M2M3
T1T2
T3
Heterogeneous permeability field
x
yz
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
0 0.2 0.4 0.6 0.8 1
reduction in flux mean
redu
ctio
n in
flux
sta
ndar
d de
viat
ion
Exp1Exp2Exp3Exp4
Zhang et al. 2008, JCH
Implication of Results•Flux distribution is an important metric that can be used for design of optimal remedial system that targets “hotspots”
• Flux distribution more stable over time than source distribution
•The observed stability of flux distribution is an unexpected andinteresting result that warrants further investigation
•Stability of flux distribution suggests the ability to characterize flux distributions in time once initial distribution is known.
A
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FLUX Characterization
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TRIAD BenefitsImproved Site Decision Making:• Integration of archived site monitoring data with new data
collection for enhanced conceptual site model• Mass discharge at source & plume control planes enables
estimation of source mass, source longevity, and natural attenuationcapacity
• Mass discharge serves as a metric for site prioritization, remediation performance, and helps in setting interim cleanup goals
• Groundwater & contaminant flux distribution measured at source control planes allows targeted source treatment & helps formulate cost-effective of site monitoring strategies
Questions• How much data needed before remediation?• What types of data best serve CSM & design?• Are high costs justified in terms of reduced
uncertainty?• What are the short-term benefits of source clean
up? • What is the likely plume response to source
clean up?• How to select target (interim) endpoints?• How to determine long-term stewardship needs?• Is there a simplified modeling & decision
framework?• How does all this fit into the TRIAD framework?
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Answers?