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www.jacobs.com | worldwide Innovation that provides sustainable solutions to complex challenges worldwide Quantifiable Lines of Evidence for Chemical Vapor Intrusion April 9 th , 2018, Eleventh International Conference on Remediation of Chlorinated and Recalcitrant Compounds CH2M is now Jacobs Chase Holton, PhD (Jacobs), Henry Schuver, DrPH (USEPA*), Chris Lutes (Jacobs), Jeff Kurtz, PhD (Geosyntec), and Robert Truesdale (RTI) *Personal Perspective & Presentation – Does not represent policy

Quantifiable Lines of Evidence for Chemical Vapor Intrusion

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Page 1: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

www.jacobs.com | worldwide

Innovation that provides sustainable solutions to

complex challenges worldwide

Quantifiable Lines of Evidence for Chemical Vapor IntrusionApril 9th, 2018, Eleventh International Conference on Remediation of Chlorinated and Recalcitrant Compounds

CH2M is now Jacobs

Chase Holton, PhD (Jacobs), Henry Schuver, DrPH (USEPA*), Chris Lutes (Jacobs), Jeff Kurtz, PhD (Geosyntec), and Robert Truesdale (RTI)

*Personal Perspective & Presentation – Does not represent policy

Page 2: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

Agenda

• Vapor Intrusion (VI) Assessment Challenges⎯ Sampling upper percentile of concentration distribution (e.g., 95th%) under natural conditions

• Indicators, Tracers, and Surrogates (ITS) for VI Assessment⎯ Definitions of ITS metrics

⎯ Evaluation of Data Rich VI Studies: Sun Devil Manor (SDM) and Indy

⎯ Temperature as an Indicator (SDM)

⎯ Radon as a Tracer/Surrogate (SDM)

• Summary and Looking Forward

Page 3: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

Vapor Intrusion – Assessment Challenges

• Indoor air sampling results subject to high variability⎯ Difficult to capture upper percentile of concentration

distribution with conventional sampling schemes

⎯ May result in false negative decisions

• Background sources can impact indoor air sampling results⎯ Sometimes difficult to identify through conventional

surveys

⎯ May result in false positive decisions

• Preferential vapor pathways are more common than we used to think⎯ May result in inadequate or unnecessary mitigation

Image sources: Holton et al.. (2013a) and photo by C. Holton

Page 4: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

Indicators, Tracers, and Surrogates for VI Assessment

• Indicators, Tracers, and Surrogates (ITS) – metrics and tools that can make VI assessment more informative, efficient , and cost-effective⎯ Indicators to narrow the assessment period (e.g., when are higher concentrations most

likely to occur?)

⎯ Tracers to enhance understanding of the CSM and/or prioritize sampling locations (e.g., how are VOCs entering the building?)

⎯ Surrogates to support or substitute for VOC results and improve the odds of a higher concentration sample.

• Select ITS are already included in VI guidance (e.g., seasonality, rainfall)

Page 5: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

Definition: Indicator

• Indicators are metrics that indicate the state or level of something, for example…⎯ In biology, an indicator can be a species that can be used to infer

habitat conditions, as amphibian population declines may indicate environmental stress

• For VI, indicators are metrics that indicate an elevated potential for CVOC exposure (e.g., temperature, pressure)

Image source: http://news.psu.edu/story/140702/2002/05/01/research/lessons‐toads

Page 6: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

Definition: Tracer

• Tracers are easily observable substances that move physically along with the targets of interest, for example…⎯ In hydrology, dyes can be followed through the course

of a physical process (water flow)

• For VI, radon is a naturally occurring tracer of the subslab soil gas to indoor air pathway and can be used to identify buildings more susceptible to VI.

Image source: http://newsroom.unl.edu/announce/files/file9957.png

Page 7: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

Definition: Surrogate

• Surrogates are metrics with a quantitative relationship to the target of interest that is sufficiently accurate to be a substitute, for example…⎯ Total coliform as surrogate for the pathogenic

organisms associated with sewage contamination

• For VI, total VOCs may be used in place of speciated VOC data to make decisions in the field

Image source: https://www.crcpress.com/The‐Coliform‐Index‐and‐Waterborne‐Disease‐Problems‐of‐microbial‐drinking/Gleeson‐Gray/p/book/9780419218708

Page 8: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

28

58

22

45

15

31

11

23

0

20

40

60

80

100

120

140

160

0.88 0.9 0.92 0.94 0.96 0.98 1

Requ

ired Num

ber o

f Sam

ples to

 Observee RM

E Once

Percentile Defined as RME =  Chance of Not Seeing RME With One Sample 

Required Number of Unguided Random Samples Per Location/Zone to Observe RME Once at Various Confidence Levels

5% Prob. Of Underestimating RME

10% Prob. Of Underestimating RME

20% Prob. Of Underestimating RME

30% Prob. Of Underestimating RME

This analysis is just the mathematics of probability. No assumptions about the distribution have been made, only the assumption of random independent sampling.  RME concentration defined as percentile. 

Reference: Kurtz et al., 2018, AEHS

Page 9: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

58

28

138

6 4 3 2 2 10

10

20

30

40

50

60

70

0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1Requ

ired Num

ber o

f Sam

ples to

 Observee RM

E Once

Guided True Positive Rate  = Chance of Seeing RME (Here defined as 95th Percentile with One Guided Sample)

Required Number of Guided Samples Per Location/Zone to Observe RME with 5% Probabilty of Underestimating

An indicator does not need to be perfect to be very helpful.  It just needs to “load the dice” by significantly increasing the odds of observing a sample toward the top of the VOC distribution.

Note the 0.05 “guided true positive” is a guide no better than chance

Reference: Kurtz et al., 2018, AEHS

Page 10: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

Evaluation of Data Rich VI Studies: SDM and Indy

• Sun Devil Manor (SDM) (Layton, UT)⎯ Studied by Arizona State University

⎯ 2.5+ year indoor air data set, also monitored weather and building dynamics

⎯ Known preferential pathway (land drain)

• Indy Duplex (Indianapolis, IN)⎯ Studied by USEPA/NERL

⎯ 1+ year indoor air data set, also monitored weather and building dynamics

⎯ Suspected preferential pathway (sewer)

SDM

Indy

Page 11: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

Source: GW plume with 10-50 μg/L TCE; GW deep gradient 0.23 ft/ft across property; Geology: silty clay with sand stringers

Sun Devil Manor[Layton, UT]

Page 12: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

SDM: Instrumentation and Monitoring Network

Page 13: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

Image source: Holton et al.. (2013a)

Page 14: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

0.01

0.1

1

10

-10

-5

0

5

10

15

20

25

30

35

0 100 200 300 400 500 600 700

Daily Average TC

E Concentration [ppbv]D

aily

Ave

rage

Indo

or-O

utdo

or T

empe

ratu

re [C

]

Time [d]

Indoor - Outdoor Temperature Difference Daily Average Concentration

Image source: Holton et al.. (2013b), AEHS Presentation

Page 15: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

0.01

0.1

1

10

100

-10 -5 0 5 10 15 20 25 30 35

TCE

Con

cent

ratio

n in

Indo

or A

ir [p

pbv]

∆Temperature (Indoor – Outdoor) [°C]

Thermal desorption tubes (4-h composite)

Portable GC/MS (1-min sample)

Page 16: Quantifiable Lines of Evidence for Chemical Vapor Intrusion
Page 17: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

SDM: What did we learn from early look at temperature data?

“Differential temperature monitoring may help narrow the assessment period – does not guarantee detection of higher concentrations”

“Diurnal changes in VI signal may be related to daily variation in differential temperature during periods of colder temperature”

Reference: Holton et al., 2013, AEHS (https://iavi.rti.org/index.cfm)

Page 18: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

34% Probability

66% Probability

Reference: Kurtz et al., 2018, AEHS

Page 19: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

0.0

0.2

0.4

0.6

0.8

1.0

1.2

1.4

1.6

0.01

0.1

1

360 390 420 450 480 510 540

24-h

r ave

. Rad

on in

Indo

or A

ir (p

Ci/L

)

24-h

r ave

. TC

E in

Indo

or A

ir (p

pbv)

Time (d)

Average Daily TCE and Radon in Indoor Air

TCERadon

Image source: Holton et al.. (2012)

Page 20: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

Radon as an Indicator of Preferential VI Pathways?

<C> <C> <C> <C> <C> <C>

sub-slab (6 ft BS) (indoor) (sub-slab) (soil gas) sub-slab (6 ft BS) (indoor) (sub-slab) (soil gas)

Year Season [ppbv] [ppbv] [ppbv] [unitless] [unitless] [pCi/L] [pCi/L] [pCi/L] [unitless] [unitless]

2011 Winter 0.81 122 0.33 0.41 0.0027 290 1600 0.50 <0.0017 <0.00031

2011 Spring 1.2 91 0.06 0.05 0.0007 310 1600 0.35 <0.0011 <0.00021

2011 Summer 0.36 93 0.0072 0.02 0.0001 370 1800 0.38 <0.001 <0.00021

2011 Fall 0.31 104 0.067 0.22 0.0006

2011 Overall 0.67 103 0.11 0.16 0.0011 323 1667 0.41 <0.0012 <0.00024

TCE Radon

Observations: Winter 2011 – Fall 2011

TCE varies by 100X - 1000X; Radon signal about 2X – 3X of baseline signal

Radon and TCE attenuation factors (ɑ=indoor air/soil gas at some depth) are different by 10X or more (especially at sub-slab depth)

10‐1 10‐3 <10‐3 <10‐4

“May need to think more about use of radon as a surrogate or VI tracer” Johnson et al., 2012

Page 21: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

Discovery of Land Drain VI Pathway

• Land drain VI pathway discovery initiated by odd soil gas profiles observed during long-term controlled depressurization testing

Page 22: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

Summary and Looking Forward

• Summary:⎯ Indicators, tracers, and surrogates related to VI-driving forces provide low cost data to

guide sampling and support VI assessment; some are already in guidance!

⎯ Differential temperature is an inexpensive indicator of when VI is more likely to occur at SDM

⎯ Differences in TCE and radon attenuation factors a potential indicator of land drain preferential pathway at SDM

• Looking forward:⎯ Seeking inputs (more sites, more data, experience with ITS) from VI community

⎯ Working toward multiple USEPA-supported publications and potentially a toolbox

• Part 1 of ITS review and evaluation submitted to Remediation Journal for publication; Part 2 currently being written

Page 23: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

Questions? Comments?

• Any experience using indicators, tracers, and/or surrogates in support of vapor intrusion assessment?⎯ How was the data collected (methods, frequency, duration)?

Page 24: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

www.jacobs.com | worldwideMay 8, 2018

© Copyright Jacobs

Thank you!Chase Holton, [email protected]

Page 25: Quantifiable Lines of Evidence for Chemical Vapor Intrusion

References• Kurtz, J. Outdoor Temperature and Differential Temperature as Indicators of VI Sampling

to Capture the RME. USEPA Vapor Intrusion Workshop at the 28th Annual International Conference on Soil, Water, Energy, and Air, San Diego, CA, March 20, 2018.

• Holton, C. Evaluation of Vapor Intrusion Pathway Assessment Through Long-Term Monitoring Studies, Doctoral Dissertation, Arizona State University, May 2015.

• Holton, C., Luo, H., Dahlen, P., Gorder, K., Dettenmaier, E., Johnson, P.C. Temporal Variability of Indoor Air Concentrations under Natural Conditions in a House Overlying a Dilute Chlorinated Solvent Groundwater Plume. Environmental Science & Technology, 2013a, 47, 13347-13354.

• Holton, C., Luo, H., Guo, Y. Dahlen, P., Gorder, K., Dettenmaier, E., Johnson, P. C. Evaluation of Selected Environmental Factors at a Vapor Intrusion Study Site. The 23rd Annual International Conference on Soil, Water, Energy, and Air, San Diego, CA, March 21, 2013b.

• Holton, C., Luo, H., Guo, Y., Gorder, K., Dettenmaier, E., Johnson, P. C. Long-Term and Short-Term Variation of Indoor Air Concentration at a Vapor Intrusion Study Site. The 22nd Annual International Conference on Soil, Water, Energy, and Air, San Diego, CA, March 19-22, 2012.