TCE Fate and Transport, as Related to Vapor Intrusion

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TCE Fate and Transport, as Related to Vapor Intrusion Eric Suuberg School of Engineering, Brown University Providence, Rhode Island NEWMOA/Brown SRP Workshop on TCE Vapor Intrusion: State of the Science, Regulations and Technical Options April 2015 Vapor intrusion involves the migration of chemical vapors in the soil and groundwater to enter buildings through foundation cracks and joints. Sometimes vapor intrusion can result in long-term exposure of contaminants at harmful levels. Affects maybe 1/4 of the estimated inventory of 500,000 US brownfields sites. At present, no general EPA guidance, though draft guidance has been prepared. States regulate, but often very different standards in use. Also jurisdictional issues - who is in charge- OSHA? EPA? State? No agreement on site investigation practices. Limited use of quantitative modeling- very fieldwork based, empirical. 1

In environmental health risk assessment, for there to be a human health risk there must be a completed exposure pathway, involving identification of a - Source (Source strength variability? Where to measure?) - Migration Route (Temporal Effects? Preferential Pathways?) - Receptor (Backgrounds? Where to measure?) -Does depth to GW matter? -Does rain/ice make a difference? Other Seasonal/weather effects? -What about non- VI background? Is subslab sampling the answer? (Interstate Technology & Regulatory Council, 2007 What is wrong with this picture? Not appropriate for trichloroethylene (TCE), which is a DNAPL 2

Source characterization may be tricky with DNAPLs Also, there is Increasing understanding of the complexity of transport From a presentation by Larry Schnapf, Schnapf LLC, Cherry Hill, NJ. September 2014 - Other exposure routes can come into play (including resident-caused exposures) From NEWMOA- Improving Site Investigation Dose from drinking 2L/day of 5 µg/l TCE in water (EPA MCL) is same as from breathing 20m 3 /day of air containing 0.5 µg/m 3 - Second is harder to control 3

Background Sources The TCE issue has just exploded in the VI field more controversy on what is safe US EPA IRIS (2011) - RfC=2 µg/m 3, HQ (1) = 2.1µg/m 3, ELCR (10-6 ) = 0.48 µg/m 3, ELCR (10-5 ) = 4.8 µg/m 3 OSHA (PEL- 8 hr) = 537,000 µg/m 3, NIOSH (10 hr) = 134,000 µg/m 3 Now, risk based indoor air levels are shifting to non-cancer endpoints (e.g. developmental; FCM, thymus weight) New prompt or urgent action levels being based upon RfCmitigation may be required in weeks or days; may involve temporary relocation. But will the FCM RfC values stand? 4

Radon cancer risk @ 2 pci/l Non-smokers: 4 per 1000 risk (10-2.4 ) Smokers: 32 per 1000 risk (10-1.5 ) Important policy implications regarding being protective against VI risk One in four homes contain radon in excess of EPA action level of 4 pci/l In some towns 50% of homes are above this level. A patchwork of regulations 5

And it s a fluid situation From a Presentation by Laurent Levy, Gradient Corp. May 2014 What levels of TCE are used by regulators? From a Presentation by Laurent Levy, Gradient Corp. May 2014 6

Indoor air sample Foundation Slab Screening values- which to use? Levels? Groundwater (Henry s Law), soil gas Subslab, indoor air How many samples taken over what time? Subslab Soil Vapor Sample Location Groundwater sample location (convert to source strength using Henry s Law) U.S. EPA uses empirical attenuation factor approach for predicting indoor air concentrations Based upon many field measurements. Cindoor/Csubslab = 0.1 (resistance of slab) Cindoor/Cgroundwater source =0.001 Groundwater Sourcereflects resistance of soil plus slab 7

From Eklund, Folkes, Kabel, Farnum, in EM, 2007. Henry s Law relates expected soil vapor concentrations to Cgroundwater source Csoil gas= H CGW Washington, 1996 Shallow groundwater temperatures (Collins, 1925) If MCL for TCE in drinking water is 5 µg/l leads to about 1 mg/m 3 soil gas. EPA recommends non-cancer toxicity level inhalation conc. of 2 µg/m 3 (1.2 µg/m 3 cancer screening level at 10-6 ) 8

Higher GW Concentration Standards associated with higher assumed AFs. That is, you can afford to accept higher GW values the greater the assumed attenuation of vapors by soil. Data for CO, LA, CT, MA, NH, MI, PA. Henry s Law constants for benzene, TCE and PCE from EPA website, 25 C 9

Subslab Sample Reliability? Photos from O Brien and Gere But before discussing the simulations, consider what the EPA database shows about subslab samples and their relationship to indoor air samples. There is often great significance given to subslab values- but does this always make sense? Little dependence of indoor air concentration on subslab values, because indoor air values dominated by background sources 10

When do you really look to VI, as opposed to other sources (e.g., consumer products)? A 1000 m 3 volume house, 2 µg/m 3 indoor air contaminant level has an air inventory of 2 mg contaminant- can sorption processes contribute to the observed phenomena? Need to watch what values you assume for background levels- they have gone down over time Source: Background Indoor Air Concentrations of VOCs in North American Residences: A Compilation of Statistics and Implications for Vapor Intrusion by Helen Dawson (EPA) 11

Can we begin to do better by applying advanced engineering modeling tools? EPA Screening Model Approach Based upon a 1-dimensional (1-D) model developed by Paul Johnson and Robbie Ettinger in 1991, based on earlier Radon work of Nazaroff and others. Everything leaving the source enters the house- unrealistic, but a consequence of 1-D. Qbuilding LT Deff Attenuation factor depends upon Qbuilding Qck AB Ack=Lckwck dck D ck Cck 12

Many mathematical models of VI being developed worldwide. Differ based on where the main attenuation is assumed Source: Yao et al., Env. Sci. Tech., 47, 2457-2470 (2013). Brown University Modeling Approach A finite element computational package (Comsol) used to describe transport processes. Set finite element model domain. Typically assume a perimeter crack in the foundation. Assume Stack Effect creates an in-house negative pressure of 5 Pa. 13

3-D Modeling Approach- Finite Element Solver (COMSOL) 3-step solution method 1. Solve for gas advective flow through soil (Darcy s Law). 2. Solve for species transport via advection and diffusion. 3. Indoor air concentration is calculated using the species flow rate into the structure. Typically model 1 to 5 mm perimeter cracks Subslab sample reliability? Roughly same values, but 2 O.O.M. difference in indoor air soil 14

Soil gas and subslab Subslab still very intrusive, and can be misleading Soil gas often misunderstood. Open field soil gas of limited value in understanding what happens in the presence of buildings, paving, or even frozen ground surface. How far is far enough?? Solved simple 2-D Laplace Equation Lowell and Eklund, 2004 Echoed in various guidance documents, but challenged by Abreu and Johnson, 2005 for homogeneous soils. 15

How close should GW Source measurements be? Foundation to source depth Yao et al. Vadose Zone Journal,2013 Subslab to Source Concentration Unusually high source to slab attenuation can have an origin in GW sources that are Source edge to building distance/source depth not really that close Consider 2 m deep basement, 4 m deep source, sampling GW at r= 5 i.e., 20 m away, can lead to significant extra attenuation Also, at what depth to sample GW? Capillary zone resistance is very important From Shen et al., Env. Engineering Sci., 2013 Capillary Zone Shows extent to which open porosity filled with water; diffusion through water layer slow Shows how dramatically COC concentration drops through capillary zone- big part of AFsoil Relates to critical issue- the role of GW vertical concentration profiles 16

Indoor Air sampling Intrusive, expensive, and is it even reliable as an indication of risk? Typical TO- 15 with 6L summa Need a lot of care to avoid being misled by background. The Issue of Transients Sample data from a 2013 AEHS Conference Workshop by Schumacher et al. Samples from a duplex in Indianapolis. Note the wide variability over short sampling times. Correlation with Radon not particularly good. Seasonal variability in indoor air higher than in subslab. 17

Courtesy: Henry Schuver, EPA The majority of VI exposure could be unpredictable! One time assessments are increasingly unlikely to be considered satisfactory 18

Paul Johnson, and Henry Schuver * As for Radon From Henry Schuver, EPA 19

Summary There exists a large variation in Attenuation Factors, for reasons that are only partly understood. Essential to consider background concentrations (and to measure or at least use current estimates). How close should a GW monitoring well be, to be reliable? There needs to be the awareness of transients, some very short term, some seasonal, and some very long time scale. Resources United States Environmental Protection Agency (USEPA). Office of Solid Waste and Emergency Response (OSWER). EPA s vapor intrusion database: evaluation and characterization of attenuation factors for chlorinated volatile organic compounds and residential buildings (EPA 530-R-10-002). March 2012. United States Environmental Protection Agency (USEPA). Background Indoor Air Concentrations of Volatile Organic Compounds in North American Residences (1990 2005): A Compilation of Statistics for Assessing Vapor Intrusion. Office of Solid Waste and Emergency Response (OSWER). EPA 530-R-10-001, 2011. United States Environmental Protection Agency (USEPA). Superfund Vapor Intrusion FAQs. 2012. www.epa.gov/superfund/sites/npl/vapor_intrusion_faqs_feb2012.pdf United States Environmental Protection Agency (USEPA). Vapor Intrusion Screening Level (VISL) Calculator. Office of Solid Waste and Emergency Response (OSWER) and Office of Superfund Remediation and Technology Innovation (OSTRI), March 2012. 20

Resources (Cont d) United States Environmental Protection Agency (USEPA). Office of Solid Waste and Emergency Response (OSWER). EPA s conceptual model scenarios for the vapor intrusion pathway (EPA 530-R-10-003). February 2012 NYSDOH (New York State Department of Health). 2006. Guidance for Evaluating Soil Vapor Intrusion in the State of New York. Troy, N.Y.: Center for Environmental Health, Bureau of Environmental Exposure Investigation. (www.nyhealth.gov/environmental/indoors/vapor_intrusion/). Interstate Technology and Regulatory Council (ITRC). Vapor Intrusion Pathway: A Practical Guideline. Washington, D.C., 2007. Courtesy: Professor Kelly Pennell, UKY 21