robin davis-pvi workshop-25th aehs san diego march 2015
TRANSCRIPT
by Robin V. Davis, P.G. Project Manager Utah Department of Environmental Quality Leaking Underground Storage Tanks [email protected] 801-536-4177
Methods for Developing and Applying Screening Criteria for the
Petroleum Vapor Intrusion Pathway
Workshop 7 Tuesday March 24, 2015
6:30 pm – 9:30 pm
Association for Environmental Health & Sciences (AEHS) 25th Annual International Conference on Soil, Sediment, Water & Energy
San Diego, California
OBJECTIVES Understand why petroleum vapor intrusion (PVI) is
very rare despite so many petroleum LUST sites
Show mechanisms, characteristics, degree of vapor bioattenuation
Avoid unnecessary additional investigation, soil gas/air sampling
Show distances of vapor attenuation, apply as Screening Criteria, screen out low-risk sites
Understand causes of PVI
SCOPE Field studies published by work groups, individuals
Source strength: LNAPL in soil and GW, dissolved-phase
Associated soil gas measurements from 1000s of sample points at 100s of sites
Extensive peer review and quality control checks
Data compiled to an empirical database:
Some US States
Australia 2012
EPA draft PVI April 2013
ITRC October 2014
EPA ORD Issue Paper 2014
Guidance Documents Issued:
EPA Petroleum Vapor Database Jan. 2013
124/>1000
Perth Sydney
Tasmania
Australia
Davis, R.V., 2009-2011 McHugh et al, 2010 Peargin and Kolhatkar, 2011 Wright, J., 2011, 2012, Australian data Lahvis et al, 2013 EPA Jan 2013, 510-R-13-001
REFERENCES
4/13
70/816
Canada
United States
MAP KEY
# geographic locations evaluated
# paired concurrent measurements
of subsurface benzene soil vapor
& source strength
70
Petroleum Vapor Database of Empirical Studies EPA OUST Jan. 2013
Australian sites evaluated separately
816
CAPILLARY ZONE
a) LNAPL SOURCE
UNSATURATED ZONE
SATURATED ZONE
sharp reaction
front
O2
VOCs
b) DISSOLVED-PHASE SOURCE
CAPILLARY ZONE
UNSATURATED ZONE
SATURATED ZONE
high massflux
limited mass flux
sharp reaction
front
constituent distributions
O2
VOCs
constituent distributions
Conceptual Characteristics of Petroleum Vapor Transport and Biodegradation
After Lahvis et al 2013 GWMR
O2/Hydrocarbon
Vapor Profile
O2/Hydrocarbon
Vapor Profile
KEY POINTS
• Aerobic biodegradation of
vapors is rapid, occurs over
short distances
• LNAPL sources have high
mass flux, vapors attenuate
in longer distances than
dissolved sources
• Sufficient oxygen supply
relative to its demand,
function of source strength
0
1
0
1
>100 years of research proves rapid vapor biodegradation by 1000s of indigenous microbes
Studies show vapors biodegrade and attenuate within a few feet of sources
No cases of PVI from low-strength sources
Causes of PVI are well-known
Bioattenuation Study Results Subsurface Petroleum Vapor
Causes of Petroleum Vapor Intrusion
Preferential pathway: sumps, elevator shafts
High-strength source in direct contact with building (LNAPL, high dissolved, adsorbed)
Groundwater-Bearing Unit
BUILDING
Unsaturated Soil
Affected GW
LNAPL
LNAPL
4 1
3
LNAPL
High-strength source in close proximity to building, within GW fluctuation zone
2
Drawing after Todd Ririe, 2009
High-Strength Sources Direct contact or close proximity to buildings
Preferential pathways: engineered & natural
Preferential pathway: bad connections of utility lines; natural fractured and karstic rocks
UST system
Dissolved contamination
Clean Soil
High vapor concentrations, high mass flux
from LNAPL & soil sources
Low vapor concentrations, low
mass flux from dissolved sources
Define extent & degree of contamination
Apply Screening Criteria Building
Collect Basic Data, Characterize Site, Construct Conceptual Site Model
LNAPL in soil
LNAPL in soil & GW
Soil Boring/MW Soil Boring/MW
Utility line
1.E+00 1.E+02 1.E+04 1.E+06 1.E+08
0
5
10
15
0 5 10 15 20
Benzene (ug/m3)
O2 & CO2 (% V/V)
Coachella, CA COA-2 (Ririe, et al 2002)
1.E+001.E+021.E+041.E+061.E+08
-5
0
5
10
15
20
0 5 10 15 20 25
Benzene (ug/m3)
Salina Cash Saver VMW-1 (UDEQ 7/27/07)
OA
IA
LNAPL
LNAPL
1.E+00 1.E+02 1.E+04 1.E+06 1.E+08
0
5
10
15
0 5 10 15 20 25
Benzene (ug/m3)
Dep
th,
fee
t b
elo
w g
rad
e
O2 & CO2 (% V/V)
Beaufort, SC NJ-VW2 (Lahvis, et al., 1999)
Oxygen
Carbon Dioxide
Benzene
Benzene in GW
16,000 ug/L
Signature Characteristics of Aerobic Biodegradation of Subsurface Petroleum Vapors
• Vapors aerobically biodegraded by oxygen-consuming microbes, waste product carbon dioxide
• Vapors attenuate in short distances
Vapor Bioattenuation Limited by Contaminated Soil
1.E+00 1.E+02 1.E+04 1.E+06 1.E+08
0
5
10
15
0 5 10 15 20
Benzene (ug/m3)
De
pth
, fe
et
be
low
gra
de
O2 & CO2 (% V/V)
Conneaut, OH VMP-1
(Roggemans, 1998; Roggemans et al., 2001)
Oxygen
Carbon Dioxide
Benzene
LNAPL in Soil (sand, silty sand)
8/26/06 6/27/07
Importance of Shallow Vapor Completion Points
Shallower point confirms attenuation above contaminated soil zone
Shallow completion too deep
Example of apparent non-attenuation until shallow vapor point installed in non-contaminated soil
VW-11 Hal’s, Green River, Utah
No attenuation within contaminated soil zone
EPA OUST Jan. 2013
Results of Empirical Studies
http://www.epa.gov/oust/cat/pvi/PVI_Database_Report.pdf
• Thickness of clean soil required to attenuate vapors
associated with LNAPL and dissolved sources
• Screening Criteria
1.E+00 1.E+02 1.E+04 1.E+06 1.E+08
0
5
10
15
0 5 10 15 20 25
Benzene (ug/m3)
O2 & CO2 (% V/V)
Santa Clara, UT VW-4 1/19/2009
4 feet Benzene in GW
3180/ ug/L
1.E+00 1.E+01 1.E+02 1.E+03 1.E+04 1.E+05 1.E+06
0
2
4
6
8
10
0 5 10 15 20 25
Benzene (ug/m3)
De
pth
, fe
et
bg
s
O2 & CO2 (% v/v)
Jackson’s, UT VMW-4 9/29/08
Oxygen, %
Carbon Dioxide, %
Benzene, ug/m3
Benzene in GW
12,000 ug/L
4.94 feet
Dissolved Sources
= Distance between top of source and deepest clean vapor point
Thickness of clean soil needed to attenuate vapors
1.E+00 1.E+02 1.E+04 1.E+06 1.E+08
0
5
10
15
0 5 10 15 20
Benzene (ug/m3)
O2 & CO2 (% V/V)
Coachella, CA COA-2 Ririe, et al 2002
9.5 feet
1.E+00 1.E+02 1.E+04 1.E+06 1.E+08
0
5
10
15
0 5 10 15 20 25
Benzene (ug/m3)
De
pth
, fe
et
be
low
gra
de
O2 & CO2 (% V/V)
Beaufort, SC NJ-VW2 Lahvis, et al., 1999
Oxygen
Carbon Dioxide
Benzene
Benzene in GW
16,000 ug/L
8 feet
LNAPL Sources
= Distance between top of LNAPL and deepest clean vapor point
Thickness of clean soil needed to attenuate vapors
Screening Distances
95%-100% Confidence
Dissolved Sources Benzene Vapors vs. Distance of Attenuation
LNAPL Sources (small sites) Benzene Vapors vs. Distance of Attenuation
5 ft 15 ft
13 feet, 95% Confidence
Lahvis et al 2013 Results of Vapor Attenuation from LNAPL Sources
• Different analysis, similar results
• 13 ft vertical
separation attenuates LNAPL source vapors
LNAPL Indicators
17
LNAPL INDICATOR MEASUREMENTS
Current or historic presence of LNAPL
in groundwater or soil
Visual evidence:
Sheen on groundwater or soil, soil staining, measurable thickness
Groundwater, dissolved-phase
PHCs >0.2 times effective solubilities
(Bruce et al. 1991)
Benzene >3-5 mg/L
TPH-gro >20-30 mg/L
TPH-dro >5 mg/L
Soil, adsorbed-phase
PHCs >effective soil saturation (Csat)
Benzene >10 mg/kg
TPH-gro >250-500 mg/kg
Soil field measurements
Organic vapor analyzer/PID/OVA of
soil cores
Gasoline-contaminated soil: >500 ppm-v
Diesel-contaminated soil: >10 ppm-v
Soil Gas measurements
- O2 shows no increase and CO2 shows no decrease with
increasing distance from source
- Elevated aliphatic soil gas concentrations, eg Hexane >100,000 ug/m3
(after EPA 2013; Lahvis et al 2013)
Results of Empirical Studies for Developing Screening Criteria
Various methods of data analysis yield similar results
Dissolved Sources require 5 feet separation distance: • Benzene <5 mg/L • TPH <30mg/L
LNAPL Sources require 15 feet separation distance: • Benzene >5 mg/L, >10 mg/kg • TPH >30mg/L, >250-500 mg/kg • 18 feet separation required for large industrial sites
Soil within separation distance: • LNAPL-free soil contains sufficient oxygen to bioattenuate vapors
• “Clean” (non-source), biologically active, sufficient oxygen and moisture
• EPA: <100 mg/kg TPH “clean” soil
Field Example:
Deep SV Benzene, ug/m3
Shallow SV Benzene, ug/m3
= AF
~7,000,000x contaminant reduction
~1 ug/m3
145,000 ug/m3 AF = = 7E-06
Measuring Magnitude of Subsurface
Vapor Attenuation
Subsurface Attenuation Factor (AF)
= Ratio of shallow to deep vapor concentration
Beaufort, SC NJ-VW2
(Lahvis, et al., 1999)
0
5
10
15
0 5 10 15 20 25
O2 & CO2 (% V/V)
1.E+00 1.E+02 1.E+04 1.E+06 1.E+08
Benzene (ug/m3)
Oxygen
Carbon Dioxide
Benzene
Benzene in GW
16,000 ug/L
0
20
40
60
80
100
1.E-021.E-03<1.E-04
Subsurface Vapor Attenuation Factors
Nu
mb
er
of
So
il V
ap
or
Sa
mp
le E
ve
nts
Benzene TPH
0
30
60
90
120
150
Reason 1: No
Clean
Overlying Soil
Reason 2: Low
Source
Strength
Reason 3:
Rapid
Attenuation
Near High-
Strength
Source
Nu
mb
er
of
So
il V
ap
or
Sa
mp
le E
ve
nts Benzene TPH
3 Reasons for
Insignificant
AFs 10x-100x
0
40
80
120
160
200
>1.E-011.E-011.E-021.E-03<1.E-04
Subsurface Vapor Attenuation Factors
Nu
mb
er
of
So
il V
ap
or
Sa
mp
le E
ve
nts
Benzene TPH
Distribution of Magnitude of Subsurface
Petroleum Vapor Attenuation Factors
Screen these out Reasonable Screening
AF 100x-1000x
Most events
exhibit Significant
AFs >10,000x
http://www.epa.gov/oswer/vaporintrusion/documents/vi-cms-v11final-2-24-2012.pdf
EPA Modeling Studies Vertical and Lateral Attenuation Distances
Lateral Distance, meters
Ve
rtic
al
Dis
tan
ce B
elo
w G
rad
e,
mete
rs
10 20 30 40 80 90 50 60 70
0
2
4
6
8
0
2
4
6
8
LNAPL Vapor Source
200,000,000 ug/m3
8 m deep (26 ft)
Lateral
Attenuation
5m (16 ft)
Building with
Basement
Vertical
Attenuation
6m (20 ft)
Oxygen
Model:
20 ft vertical 16 ft lateral Field Data:
15 ft vertical
8 ft lateral
Conclusions: - Models under-predict
attenuation
- Vapors attenuate in
shorter distances
laterally than vertically
Reference
Screening
Distance
(feet)
Screening
Concentration
Benzene, TPH (ug/L)
Other
Criteria
EPA OUST Petroleum
Database Report
5
15
<5000, <30,000
LNAPL
LNAPL UST sites. 18 ft for large sites.
Clean soil <250 mg/kg TPH
Wright, J., Australia,
2011 5 <1000 Includes large industrial sites
30 LNAPL
California 5 <100 SG Oxygen not required
5 <1000 SG Oxygen required >4%
10 <1000 SG Oxygen not required
30 LNAPL
Indiana
5 <1000 SG Oxygen not required
Distances apply vertically & horizontally
AFs for GW & SG 30 LNAPL
New Jersey 5 <100 SG Oxygen not required
5 <1000 SG Oxygen required >2%
10 <1000 SG Oxygen not required
100 LNAPL Distances apply vertically & horizontally
Wisconsin 5 <1000 Distances apply vertically & horizontally
20 >1000
30 LNAPL