State of the art, challenges and upcoming...
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State of the art, challenges and upcoming techniques regarding investigation and
remediation of chlorinated solvents
Tom Heron, Executive Director Charlotte Riis, Expertise Director
NIRAS
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Source versus Plume
Governing Parametres
Distribution and Risk
• Contaminant Characteristics
• Geology
• Hydrogeology
• Soil/GW chemistry; redox
• Time
Source zone • Free Phase (DNAPL) and high
sorbed and dissolved concentrations • mg/l or mg/kg • >95% of the mass
Plume •Dissolved components • Low concentrations;
µg/l or µg/kg
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Challenges DNAPL and/in Low permeable Soil
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Backdiffusion and Scale
Few cm to decimetres
1 – 100 cm
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V = -k ∙ dh/dx
Challenges Permeability Contrasts
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Residual fri fase; 2 fase flow
V = -k ∙ dh/dx
Boks 2. Beregning af reduceret gennemstrømning som følge af residual fri fase.
F = 2 kr/(1 + kr) hvor
F er reduktionen af gennemstrømningen
kr er den relative permeabilitet i området med residual fri fase (kr =
1 ved uforurenede forhold)
Anderson, M. R. The dissolution and transport of dense non-aqueous phase liquids in saturated porous media, 1988. OHSU OGI School of Science & Engineering, Beaverton, OR
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Challenges
• Understand the system at the relevant scale - Characterization
• Extreme demands: 10.000 to 1 µg/l
• Ensure CONTACT (X-Y-Z, mass, time)
‐ Flow by-pass
‐ Diffusion in/out
‐ Reactions in water phase
‐ Incapsulation
‐ Density driven flow
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Understand the system at the relevant scale
Characterization
• Contaminant Composition and 3D Distribution
• Geology
• Hydrogeology
• Soil- and Water Chemistry; Redox
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Characterization
High quality sampling, depth specific; Coring
Non-/Less disruptive; Probing
Site specific combination of tools
Dynamic Approaches, Rapis SA; TRIAD
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Data presentation
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Source Zones Continous sampling with Dual-Tube system
• Continous sampling (1,25” cores) in 2,25” casing
• Ground Water Sampling in selected depths (SP22)
• Small diameter screened permanent sampling points for gas or water
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Source Zones DNAPL Detection using MIP, Coring and Sudan-IV Dye tests
76 1,4
6,6 0,03
21.000 79,0
250 0,78 270 0,42
450 2,70
Soil samples mg/kg TS PCE TCE Sand
Moraine clay
Sand
Moraine clay
M412 og K401 (80 cm apart)
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Source Zones MIP with GC/MS
• MIP-system and on-site GC/MS for detection of VOC’s in carrier gas. Appr. 1 sample/meter
Probing DK
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Source Zones FLUTe FACT liner, MIP and Coring (PCE)
MIP M5
PID [µV]
0
1
2
3
4
5
6
7
8
9
10
0,0E+0 2,0E+6 4,0E+6 6,0E+6
MIP M5
FID [µV]
0
1
2
3
4
5
6
7
8
9
10
0,0E+0 2,0E+6 4,0E+6 6,0E+6
MIP M5
XSD [µV]
0
1
2
3
4
5
6
7
8
9
10
0,0E+0 2,0E+6 4,0E+6 6,0E+6
Kerneprøve K3
Sum chlorerede
[mg/kg-Wv]
0
1
2
3
4
5
6
7
8
9
10
0 1 10 100 1000
Kerneprøve K3
PID
[ppm]
0
1
2
3
4
5
6
7
8
9
10
0 1 10 100 1000
FLUTe liner F3B
Sum chlorerede
0
1
2
3
4
5
6
7
8
9
10
0 2000 4000
Liner MIP Core
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Source Zones Laser Induced Fluorescens (LIF) for in-situ detection of LNAPL (UVOST system, Dakota)
• Aromatic components floures, Aliphats don’t
• Different respons from different UV-wave lengths
• Real time respons
• Used in combination with GeoProbe
• Detection level; 10-50 ppm in soil
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Source Zones Dye-LIF for detection of DNAPL (Dakota Tech.)
• Injection of hydrophobic dye 30 cm ’in front’ of UV-Source/detector
• Induces Flourescens from DNAPL by preferential dissolution of dye into the DNAPL
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Ground Water Plumes Dissolved Concentrations
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Ground Water Plumes Depth specific sampling using Geoprobe
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Ground Water Plumes EnISSA system (Belgium)
• In-Situ measurements; MIP & GC-MS; detection of 14 VOC pr. 30 cm (1 min./analyses)
• Detektion limit for VOC i ground water ~ 20 µg/l
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Ground Water Plumes Waterloo profiler with Geoprobe
• Waterloo profiler modified (Stone Environmental)
• Water sampling, hydraulic head and K estimation
• Continuous extraction from probe and on-line analyses of redox-parametres
PCE TCE TCA 1,2-DCE Head K
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Ground Water Plumes Low detection limit MIP
• Sensitivity enhanced > 10 times, using XSD detector
Responstest with 0,5 ppm TCE
Standard system
New system
Standard
New
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Geology and Hydrogeology
Coring, depth specific, detailed sampling
Probing, Non-/Less disruptive
• Physical
• Electrical
• Optical
• Chemical
Less permanent piezometres
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Geology and Hydrogeology Estimation of K and vertical gradient by HPT
• HPT pressure yields trustworthy hydraulic conductivity data. Values from 10-4 -10-6 m/s
• Conductivity log for indication of geological composition
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Hydrogeology Pneumatic slugtest for estimating K-values and simultaneous water sampling
• K-values validated by HPT
• Basis for flux estimates (M=A*v*C)
0
1
2
3
4
5
6
7
0 10 20 30
De
pth
(m
ete
rs)
Hydraulic Conductivity [K] (m/day)
Est. K (m/day)
Slug Test K (m/day)
24.16 m/day
18.06 m/day
0.43 m/day
0.90 m/day
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Geology and Hydrogeology CPT, Electrical Conductivity-logs & Photos
• CPT (Tip & Sleeve, Hydraulic Head)
• Electrical Conductivity, tracing ZVI/Guar injektion with tracer
• Optical log
0,3
0,8
1,3
1,8
2,3
2,8
3,3
3,8
4,3
4,8
5,3
5,8
6,3
6,8
7,3
0 200 400 600 800 1000 1200
Dyd
be (
m u
.t.]
EC [mS/m]
E314
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Summary
• High Resolution data on
Contaminant Distribution
Geology
Hydrogeology
Redox Conditions
• In Situ measurements
• High Quality On-Site, On-line, Real-time data
• Supplementary Accredited Analyses
• Dynamic Approach for Rapid Site Assessment
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Remediation
• Choose the right technology/-ies
‐ Contact / Non-contact issues
‐ Flow by-pass
‐ Density driven flow
‐ Stoichiometric delivery
‐ Incapsulation issues
‐ Diffusion in/out
‐ Reactions in water phase
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Flow bypass,
dilution & dispersion kinetics
Desorption, diffusion
Contact sport
• Air Sparging
• Soil Vapor Extraction
• In Situ Chemical Oxidation
• Biological methods
• Flushing
• Pump and Treat
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Courtesy of Gorm Heron, TerraTherm
Non-Contact
• Excavation
• Mixing
• Thermal Enhanced
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Technologies and key parametres
ERD ISCO SVE IAS Ther-mal
DPE, etc
Smolde-ring
Mixing
Surfac-tants
Fracturing
EK
Contact dependent √ √ √ √ % √ % % √ √*
Sufficient mass deliv. √ √ % % % % √ √ √ √
Specific concentration √ √ % % % % √ (√) √ √
Contact time requirements
√ √ √ √ √ √ % √ √ √
Extr. pathways require. % % √ √ √ √ % % √ %
Risk of spreading √ √ √ √ √ % % (%) √ √
Soil structure changes % (%) % % (%) % (%) √ % %
Enhancement methods So
il V
apo
r E
xtra
ctio
n
En
han
ced
Red
uct
ive
Deh
alo
gen
atio
n
Slo
w In
Sit
u C
om
bu
stio
n
In S
itu
Air
Sp
arg
ing
Th
erm
ally
En
han
ced
Te
chn
olo
gie
s
Du
al P
has
e/M
ult
i Ph
ase
Ext
ract
ion
In S
itu
Ch
emic
al O
xid
atio
n
Hyd
rau
lic o
r p
neu
mat
ic
Ele
ctro
Kin
etic
Tra
nsp
ort
Ph
ysic
al m
ixin
g o
f so
il et
c.
En
han
ced
Dis
solu
tio
n b
y su
rfac
e ac
tive
am
men
dm
ents
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Fighting the contact challenge
• Slow Release; Chelated Iron, fast/slow substrates
• Mixing
• Fracturing
• Circulation
• Surfactants
• Pulsed injection
• Changing injection pressure and re-injection
• Installation/over-injection
• Osmosis/ion-migration/foreses (EK-Bio)
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Sand
Volatile/semi-volatile
components: Light oils,
chlorinated solvents etc.
‘Homogenous’ sand
> 95 %
Thermal: Steam, ISTD, ERH, RF
Radical oxidation: Fentons, persulfate, Regen-Ox
ZVI-Clay/Soil Mixing
Smoldering
(Direct Ox/ERD/S-ISCO/S-ERD)
< 25 % Pump & Treat
50 – 75%
Oxidation: KMnO4, Persulfate, ozone, H2O2
Enhanced biological degradation
(Air Sparging/SVE)
Surfactant Flushing
< 50 %
Air Sparging/SVE
Free phase pumping, DPE
(Surfactant flushing)
Realistic removal
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? ?? ?
Clay and silt
> 95 %
< 25 %
Air Sparging/SVE
Free phase pumping, DPE
Smoldering
Pump & Treat
Phytoremediation
Natural attenuation
50 – 75% Radical oxidation: Fentons, persulfate, Regen-Ox etc.
< 50 % Direct Ox/ERD/S-ISCO/S-ERD
Enhanced biological degradation
Volatile/semi-volatile
componenter: Light oil
products, chlorinated solvents
etc.
Realistic removal Excavation
Thermal: ISTD, ERH, SEE, RF
ZVI-Clay/Soil Mixing
EK-Bio ?
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That’s it!