1.2. PVI and Vapor Intrusion (VI)
The defining feature of PVI that distinguishes it as a unique subdivision of VI is the rapid rate of attenuation of PHCs because of aerobic biodegradation. With PVI, vapor concentrations generally decrease with increasing distance from a subsurface vapor source due to aerobic biodegradation, and eventually at some distance, the concentrations become negligible (USEPA, 2015a and 2015b). The extent and rate to which this natural biodegradation process occurs is strongly influenced by several factors cited by Lahvis and Baehr (1996), Suarez and Rifai (1999) and USEPA (2015a) and include: the concentration of the vapor source, the distance the vapors must travel to potential receptors, and the presence of O2. Petroleum vapors are not expected to migrate more than 15 feet (ft) from any source with most vapors being degraded within inches to a few feet.
Studies have documented the subsurface biodegradation of PHC vapors (McAlary et al., 2007; Ririe et al., 2002; Hers et al., 2000; Ostendorf et al., 2000; Lahvis et al., 1999). Recent evaluations of empirical soil gas data have demonstrated that biodegradation can limit the migration of PHC vapors from a subsurface vapor source (USEPA, 2013; Lahvis et al., 2013; Davis, 2009). These studies show that the potential for PVI is reduced because biodegradation minimizes the flux of PHC vapors in soil gas from a vapor source to overlying buildings.
General differences between PVI and VI for PHCs and CVOCs are discussed in Table 2-1 ITRC (2014) which is based on USEPA (2012a). These differences form the basis for the PVI-specific facility screening approach discussed and detailed in this volume.
1.3. Biodegradation
Aerobic biodegradation is the most important fate and transport mechanism for understanding PVI and is the basis for the screening strategy presented in Sections 4 and 5. The processes of partitioning, diffusion, advection, and mixing are the same for PHCs and other compounds, including CVOCs. Further details on these processes, its uniqueness to PVI, and the biogeochemical behavior of PHCs is discussed in Appendix C - Chemistry of Petroleum and Appendix M - Fate and Transport of Petroleum Vapors in ITRC (2014). A brief summary of the processes of biodegradation is provided below.
The Process of Biodegradation
PHC-degrading bacteria are found in biologically active soil in most environments (USEPA, 2015a) in Michigan. PHC-degrading bacteria can consume hydrocarbons rapidly in the presence of O2. This process limits the transport of PHC vapors. Although PHCs can be biodegraded in the absence of O2, the most rapid rates of biodegradation typically occur under aerobic conditions. The vadose zone above an area contaminated by a petroleum NAPL is normally an aerobic environment in which O2 can be readily replenished from the atmosphere. USEPA (2013 and 2015b) identified a total petroleum hydrocarbon (TPH) concentration of 250,000 micrograms per kilogram (µg/kg) as a metric for clean, biologically active soil absent of NAPL. EGLE uses a multiple lines of evidence approach for evaluation of when NAPL is absent (see EGLE’s Non-Aqueous Phase Liquid – Petroleum Releases Characterization, Remediation, and Management Guidance dated June 2023) to identify clean, biologically active soil. The rates of petroleum vapor biodegradation typically exceed the rates of petroleum vapor transport via diffusion; therefore, petroleum vapors are often fully attenuated by aerobic biodegradation processes in the vadose zone. This process is fundamental in understanding why unsaturated soil that does not contain NAPL does not pose a risk to the VIAP.
Environmental Effects on Biodegradation
While there is the general reliability of aerobic biodegradation in reducing the potential for an unacceptable risk for PVI, there are some environmental factors that can hinder this process, such as lack of soil moisture (USEPA, 2015a), which are not common in Michigan. The most significant factor in biodegradation is the availability of O2, which is a necessary electron acceptor and enzyme reactant in the aerobic biodegradation of PHCs. Roggemans et al. (2001) showed O2 concentrations of 2% by volume to be supportive of aerobic biodegradation. Other factors that can limit the biodegradation are described in ITRC (2014). In Michigan, these factors can often be found by the lack of O2 present in the subsurface.
1.4. PVI CSM
A CSM provides an iterative representation of the site data and information collected from the property or properties and guides the decision-making process. The CSM should be refined throughout the life of the project as new information is acquired. Because of the importance of biodegradation to PVI, the CSM for any petroleum release should incorporate biodegradation. Information to construct the CSM is acquired from historical research, facility characterization (e.g., sample collection), and an understanding of contaminant behavior, among other sources. Additional information on the development of a CSM can be found in ASTM International E1689-95 (2008) Standard Guide for Developing Conceptual Site Models for Contaminated Sites.
Vapor Source for a Petroleum Release
CSMs assist in defining and depicting the nature and extent of the vapor source and identifying where a potentially unacceptable risk for the VIAP may occur to guide further evaluation or response actions. Site data shows that when petroleum is most likely to pose a risk to the VIAP it is limited to NAPL being close to structures (e.g., less than 15 feet); dissolved phase PHCs or NAPL in direct contact with or entry into building foundations (e.g., basements, elevator pits, etc.); and NAPL entering into subsurface utilities (McHugh et al., 2010). The vapor source is key to understanding and identifying where potentially unacceptable risks for the VIAP may occur and is generally associated with the applicable unrestricted criterion. The applicable unrestricted VIAC can also be used to understand the full extent of a person’s obligations that exist under Part 201. See Volume 6 – Volatilization to the Indoor Air Criteria for more information.
For the risk evaluation of the VIAP associated with a petroleum release, only the applicable unrestricted groundwater VIAC and NAPL are used because of the aerobic biodegradation of PHC vapors in clean biologically active soil (soil without residual NAPL). Petroleum-contaminated soil in exceedance of appliable unrestricted residential soil VIAC that has been determined through multiple lines of evidence to be without NAPL will not be utilized in PVI risk evaluations.
NOTE: If an evaluation is made in accordance with Rule 299.14(5) and Rule 299.24(5) using more representative data such as soil gas, the soil gas data can be used to show compliance with the VIAC and that an unacceptable risk will not occur for a specific structure. The need for land or resource use restrictions will be highly dependent on site conditions, how or where the soil gas samples were collected in relation to the vapor source, and if future land uses can be evaluated with representative soil gas samples. See Section 6 and Attachment D.4 for more details.