Vapor Intrusion Assessments Performed During Site Investigations Petroleum Remediation Program I
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Products of OH + Furan Reactions and Some Implications for Aromatic Hydrocarbon Atmospheric Degradation
Products of OH + Furan Reactions and Some Implications for Aromatic Hydrocarbon Atmospheric Degradation Roger Atkinson, Air Pollution Research Center, University of California, Riverside Unsaturated 1,4-dicarbonyls are important products of the atmospheric degradations of aromatic hydrocarbons such as benzene, toluene, xylenes and trimethylbenzenes, which comprise 20% of the non- methane volatile organic compounds present in urban air masses in the USA. However, in many cases the measured formation yields of the unsaturated 1,4-dicarbonyls are significantly lower than those of these presumed co-product 1,2-dicarbonyls. These discrepancies could be due to analytical problems and/or rapid photolysis of unsaturated 1,4-keto-aldehydes and unsaturated 1,4-dialdehydes, or to incorrect reaction mechanisms for the OH radical-initiated reactions of aromatic hydrocarbons. Since unsaturated 1,4- dicarbonyls are major products of OH + furans, with apparently simpler product distributions and mechanisms, we have investigated the reactions of OH radicals with furan, 2- and 3-methylfuran, and 2,3- and 2,5- dimethylfuran, in the presence of NO. Using direct air sampling atmospheric pressure ionization tandem mass spectrometry and gas chromatography, the unsaturated 1,4-dicarbonyls were observed and quantified. The measured unsaturated 1,4-dicarbonyl formation yields ranged from 8 ± 2% from OH + 2,3-dimethylfuran to 75 ± 5% from OH + furan. Other products were also formed. These data will be presented and discussed and, time permitting, a brief discussion of in situ nitro-aromatic and nitro-PAH formation from the atmospheric degradations of aromatic hydrocarbons and PAHs will also be presented. Live cast on the link below: http://www.fin.ucar.edu/it/mms/fl-live.htm A recording will be available on ACD’s website for viewing at a later date. -
Formation of Highly Oxygenated Organic Molecules from Aromatic Compounds
Formation of highly oxygenated organic molecules from aromatic compounds. Ugo Molteni1, Federico Bianchi1-2, Felix Klein1, Imad El Haddad1, Carla Frege1, Michel J. Rossi1, Josef Dommen1, Urs Baltensperger1,* 5 1Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, CH-5232 Villigen, Switzerland 2Department of Physics, University of Helsinki, 00014 Helsinki, Finland Correspondence to: Urs Baltensperger ([email protected]) Abstract 10 Anthropogenic volatile organic compounds (AVOC) often dominate the urban atmosphere and consist to a large degree of aromatic hydrocarbons (ArHC), such as benzene, toluene, xylenes, and trimethylbenzenes, e.g. from handling and combustion of fuels. These compounds are important precursors for the formation of secondary organic aerosol. Despite their recognized importance as atmospheric reactants, the formation of highly oxygenated molecules (HOMs) in the gas phase leading to (extremely) low volatility compounds has not been studied in the past. Here we show that oxidation of 15 aromatics with OH leads to a subsequent autoxidation chain reaction forming HOMs with an O:C ratio of up to 1.09. This is exemplified for five single-ring ArHC (benzene, toluene, o-/m-/p-xylene, mesitylene (1,3,5-trimethylbenzene) and ethylbenzene), as well as two conjugated polycyclic ArHC (naphthalene and biphenyl). We present the identified compounds, differences in the observed oxidation patterns and discuss mechanistic pathways. We report the elemental composition of the HOMs and show the differences in the oxidation patterns of these ArHCs. A potential pathway for the 20 formation of these HOMs from aromatics is presented and discussed. We hypothesize that AVOC may contribute substantially to new particle formation events that have been detected in urban areas. -
User''s Guide for Evaluating Subsurface Vapor Intrusion Into Buildings
USER'S GUIDE FOR EVALUATING SUBSURFACE VAPOR INTRUSION INTO BUILDINGS Prepared By Environmental Quality Management, Inc. Cedar Terrace Office Park, Suite 250 3325 Durham-Chapel Hill Boulevard Durham, North Carolina 27707-2646 Prepared For Industrial Economics Incorporated 2667 Massachusetts Avenue Cambridge, Massachusetts 02140 EPA Contract Number: 68-W-02-33 Work Assignment No. 004 PN 030224.0002 For Submittal to Janine Dinan, Work Assignment Manager U.S. ENVIRONMENTAL PROTECTION AGENCY OFFICE OF EMERGENCY AND REMEDIAL RESPONSE ARIEL RIOS BUILDING, 5202G 1200 PENNSYLVANIA AVENUE, NW WASHINGTON, D.C. 20460 Revised February 22, 2004 DISCLAIMER This document presents technical and policy recommendations based on current understanding of the phenomenon of subsurface vapor intrusion. This guidance does not impose any requirements or obligations on the U.S. Environmental Protection Agency (EPA) or on the owner/operators of sites that may be contaminated with volatile and toxic compounds. The sources of authority and requirements for addressing subsurface vapor intrusion are the applicable and relevants statutes and regulations.. This guidance addresses the assumptions and limitations that need to be considered in the evaluation of the vapor intrusion pathway. This guidance provides instructions on the use of the vapor transport model that originally was developed by P. Johnson and R. Ettinger in 1991 and subsequently modified by EPA in 1998, 2001, and again in November 2002. On November 29, 2002 EPA published Draft Guidance for Evaluating the Vapor Intrusion to Indoor Air Pathway from Groundwater and Soils (Federal Register: November 29, 2002 Volume 67, Number 230 Page 71169-71172). This document is intended to be a companion for that guidance. -
Chapter 3 Equations of State
Chapter 3 Equations of State The simplest way to derive the Helmholtz function of a fluid is to directly integrate the equation of state with respect to volume (Sadus, 1992a, 1994). An equation of state can be applied to either vapour-liquid or supercritical phenomena without any conceptual difficulties. Therefore, in addition to liquid-liquid and vapour -liquid properties, it is also possible to determine transitions between these phenomena from the same inputs. All of the physical properties of the fluid except ideal gas are also simultaneously calculated. Many equations of state have been proposed in the literature with either an empirical, semi- empirical or theoretical basis. Comprehensive reviews can be found in the works of Martin (1979), Gubbins (1983), Anderko (1990), Sandler (1994), Economou and Donohue (1996), Wei and Sadus (2000) and Sengers et al. (2000). The van der Waals equation of state (1873) was the first equation to predict vapour-liquid coexistence. Later, the Redlich-Kwong equation of state (Redlich and Kwong, 1949) improved the accuracy of the van der Waals equation by proposing a temperature dependence for the attractive term. Soave (1972) and Peng and Robinson (1976) proposed additional modifications of the Redlich-Kwong equation to more accurately predict the vapour pressure, liquid density, and equilibria ratios. Guggenheim (1965) and Carnahan and Starling (1969) modified the repulsive term of van der Waals equation of state and obtained more accurate expressions for hard sphere systems. Christoforakos and Franck (1986) modified both the attractive and repulsive terms of van der Waals equation of state. Boublik (1981) extended the Carnahan-Starling hard sphere term to obtain an accurate equation for hard convex geometries. -
Trimethylbenzenes CAS Registry Numbers: 526-73-6 (1,2,3-TMB) 95-63-6 (1,2,4-TMB) 108-67-8 (1,3,5-TMB) 25551-13-7 (Mixed Isomers)
Development Support Document Final, September 4, 2015 Trimethylbenzenes CAS Registry Numbers: 526-73-6 (1,2,3-TMB) 95-63-6 (1,2,4-TMB) 108-67-8 (1,3,5-TMB) 25551-13-7 (Mixed Isomers) Prepared by Joseph T. Haney, Jr., M.S. Angela Curry, M.S. Toxicology Division Office of the Executive Director TEXAS COMMISSION ON ENVIRONMENTAL QUALITY Trimethylbenzenes Page i TABLE OF CONTENTS TABLE OF CONTENTS ............................................................................................................................................ I LIST OF TABLES ......................................................................................................................................................II ACRONYMS AND ABBREVIATIONS ................................................................................................................. III CHAPTER 1 SUMMARY TABLES .......................................................................................................................... 1 CHAPTER 2 MAJOR SOURCES AND USES ......................................................................................................... 4 CHAPTER 3 ACUTE EVALUATION ...................................................................................................................... 4 ACUTE 3.1 HEALTH-BASED ACUTE REV AND ESL ........................................................................................................ 4 3.1.1 Physical/Chemical Properties .................................................................................................................... -
Greenhouse Gas Fluxes from Soils of Different Land-Use Types in a Hilly
Available online at www.sciencedirect.com Agriculture, Ecosystems and Environment 124 (2008) 125–135 www.elsevier.com/locate/agee Greenhouse gas fluxes from soils of different land-use types in a hilly area of South China Hui Liu a,b, Ping Zhao a,*, Ping Lu c, Yue-Si Wang d, Yong-Biao Lin a, Xing-Quan Rao a a South China Botanic Garden, Chinese Academy of Sciences, Guangzhou 510650, PR China b School of Tourism and Environment, Guangdong University of Business Studies, Guangzhou 510320, PR China c EWL Sciences, P.O. Box 39443, Winnellie, Northern Territory 0821, Australia d Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, PR China Received 15 October 2006; received in revised form 3 September 2007; accepted 11 September 2007 Available online 24 October 2007 Abstract The magnitude, temporal, and spatial patterns of greenhouse gas (hereafter referred to as GHG) fluxes from soils of plantation in the subtropical area of China are still highly uncertain. To contribute towards an improvement of actual estimates, soil CO2,CH4, and N2O fluxes were measured in two different land-use types in a hilly area of South China. This study showed 2 years continuous measurements (twice a week) of GHG fluxes from soils of a pine plantation and a longan orchard system. Impacts of environmental drivers (soil temperature and soil moisture), litter exclusion and land-use (vegetation versus orchard) were presented. Our results suggested that the plantation and orchard soils were weak sinks of atmospheric CH4 and significant sources of atmospheric CO2 and N2O. Annual mean GHG fluxes from soils of plantation À1 À1 À1 À1 and orchard were: CO2 fluxes of 4.70 and 14.72 Mg CO2–C ha year ,CH4 fluxes of À2.57 and À2.61 kg CH4–C ha year ,N2O fluxes À1 À1 of 3.03 and 8.64 kg N2O–N ha year , respectively. -
Using Respiration Quotients to Track Changing Sources of Soil Respiration Seasonally and with Experimental Warming
Biogeosciences, 17, 3045–3055, 2020 https://doi.org/10.5194/bg-17-3045-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Using respiration quotients to track changing sources of soil respiration seasonally and with experimental warming Caitlin Hicks Pries1,2, Alon Angert3, Cristina Castanha2, Boaz Hilman3,a, and Margaret S. Torn2 1Department of Biological Sciences, Dartmouth College, Hanover, NH 03755, USA 2Climate and Ecosystem Science Division, Earth and Environmental Science Area, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA 3Institute of Earth Sciences, the Hebrew University of Jerusalem, Givat Ram, Jerusalem 91904, Israel acurrently at: Department of Biogeochemical Processes, Max Planck Institute for Biogeochemistry, Jena 07745, Germany Correspondence: Caitlin Hicks Pries ([email protected]) Received: 7 June 2019 – Discussion started: 28 June 2019 Revised: 9 March 2020 – Accepted: 28 April 2020 – Published: 17 June 2020 Abstract. Developing a more mechanistic understanding of activity that may have utilized oxidized carbon substrates, soil respiration is hampered by the difficulty in determin- while growing-season values were lower in heated plots. Ex- ing the contribution of different organic substrates to respi- perimental warming and phenology change the sources of ration and in disentangling autotrophic-versus-heterotrophic soil respiration throughout the soil profile. The sensitivity of and aerobic-versus-anaerobic processes. Here, we use a rel- ARQ to these changes demonstrates its potential as a tool atively novel tool for better understanding soil respiration: for disentangling the biological sources contributing to soil the apparent respiration quotient (ARQ). The ARQ is the respiration. amount of CO2 produced in the soil divided by the amount of O2 consumed, and it changes according to which or- ganic substrates are being consumed and whether oxygen is being used as an electron acceptor. -
Liquid-Vapor Equilibrium in a Binary System
Liquid-Vapor Equilibria in Binary Systems1 Purpose The purpose of this experiment is to study a binary liquid-vapor equilibrium of chloroform and acetone. Measurements of liquid and vapor compositions will be made by refractometry. The data will be treated according to equilibrium thermodynamic considerations, which are developed in the theory section. Theory Consider a liquid-gas equilibrium involving more than one species. By definition, an ideal solution is one in which the vapor pressure of a particular component is proportional to the mole fraction of that component in the liquid phase over the entire range of mole fractions. Note that no distinction is made between solute and solvent. The proportionality constant is the vapor pressure of the pure material. Empirically it has been found that in very dilute solutions the vapor pressure of solvent (major component) is proportional to the mole fraction X of the solvent. The proportionality constant is the vapor pressure, po, of the pure solvent. This rule is called Raoult's law: o (1) psolvent = p solvent Xsolvent for Xsolvent = 1 For a truly ideal solution, this law should apply over the entire range of compositions. However, as Xsolvent decreases, a point will generally be reached where the vapor pressure no longer follows the ideal relationship. Similarly, if we consider the solute in an ideal solution, then Eq.(1) should be valid. Experimentally, it is generally found that for dilute real solutions the following relationship is obeyed: psolute=K Xsolute for Xsolute<< 1 (2) where K is a constant but not equal to the vapor pressure of pure solute. -
An Investigation of a Soil Gas Sampling Technique and Its Applicability for Detecting Gaseous PCE and TCA Over an Unconfined Granular Aquifer
Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 6-1988 An Investigation of a Soil Gas Sampling Technique and Its Applicability for Detecting Gaseous PCE and TCA Over an Unconfined Granular Aquifer Timothy J. Mayotte Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons, and the Hydrology Commons Recommended Citation Mayotte, Timothy J., "An Investigation of a Soil Gas Sampling Technique and Its Applicability for Detecting Gaseous PCE and TCA Over an Unconfined Granular Aquifer" (1988). Master's Theses. 1201. https://scholarworks.wmich.edu/masters_theses/1201 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. AN INVESTIGATION OF A SOIL GAS SAMPLING TECHNIQUE AND ITS APPLICABILITY FOR DETECTING GASEOUS PCE AND TCA OVER AN UNCONFINED GRANULAR AQUIFER by Timothy J. Mayotte A Thesis Submitted to the Faculty of The Graduate College in partial fulfillment of the requirements for the Degree of Master of Science Department of Geology Western Michigan University Kalamazoo, Michigan June 1983 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. AN INVESTIGATION OF A SOIL GAS SAMPLING TECHNIQUE AND ITS APPLICABILITY FOR DETECTING GASEOUS PCE AND TCA OVER AN UNCONFINED GRANULAR AQUIFER Timothy J. Mayotte, M.S. Western Michigan University, 1988 A soil gas sampling and analytical technique was investigated to evaluate its ability and versatility for detecting chlorinated hydrocarbons in unconfined aquifers. -
Estimation of Soil Respiration: Techniques for Measurement of Soil Gas
Estimation of soil respiration: Techniques for measurement of soil gas Mark Blonquist Apogee Instruments Bruce Bugbee Utah State University Scott Jones Utah State University Two methods for soil respiration measurement Soil surface flux Gradient flux (chambers): (buried sensors): • widely used • not commercially available • commercially available ($3,000-$15,000) ($15,000-60,000) • provides subsurface data • must account for altered boundary • requires diffusion coefficient layer • challenging to measure sub- • doesn’t need diffusion coefficient surface gas concentration Photo from LI-COR Biosciences Photo from Turcu et al. (2003) Respiration: CH2O + O2 CO2 + H2O 20.95% 0.04% Advantage of O2 = 20.95% = 520 x CO = 0.04% measuring CO2 2 Advantage of 1 – No bicarbonate effects measuring O2 2 – Low cost (approx. $300 vs. $900) Once physical effects are accounted for, relationship between C flux and C metabolized (respiration) is 1:1 Respiratory quotient: CO2 / O2 Carbohydrate RQ = 1.0 Protein RQ = 0.8 Fat RQ = 0.6 Lignin RQ = 0.2 Nitrification: RQ = 0.0 + NH4 + 2O2 NO3 + 2H + H2O Two ways to express gas concentration Absolute Units Relative Units • partial pressure • percent gas in air [kPa] [%] • moles of gas per unit volume • mole fraction [mol m-3] [kPa kPa-1 air] • mass of gas per unit volume • parts per million [g m-3] [ppm] Gas sensors respond to absolute concentration, but are generally calibrated to read relative units Factors affecting gas concentration in soil • Barometric Pressure Factors affecting gas concentration in soil • Barometric -
CONTAMINATION of SOIL, SOIL GAS, and GROUND WATER by HYDROCARBON COMPOUNDS NEAR GREEAR, MORGAN COUNTY, KENTUCKY by A. Gilliam Al
CONTAMINATION OF SOIL, SOIL GAS, AND GROUND WATER BY HYDROCARBON COMPOUNDS NEAR GREEAR, MORGAN COUNTY, KENTUCKY By A. Gilliam Alexander, Douglas D. Zettwoch, and Michael D. Unthank, U.S. Geological Survey, and Robert B. Burns, Kentucky Natural Resources and Environmental Protection Cabinet, Division of Waste Management U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 92-4138 Prepared in cooperation with the KENTUCKY NATURAL RESOURCES AND ENVIRONMENTAL PROTECTION CABINET, DIVISION OF WASTE MANAGEMENT Louisville, Kentucky 1992 U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. Geological Survey Dallas L. Peck, Director For additional information Copies of this report can be write to: purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Books and Open-File Reports Section 2301 Bradley Avenue Federal Center, Box 25425 Louisville, KY 40217 Denver, CO 80225 CONTENTS Abstract............................................................ 1 Introduction........................................................ 1 Purpose and scope.............................................. 3 Description of the study area.................................. 3 History of ground-water contamination.......................... 4 Hydrogeologic framework............................................. 5 Alluvium....................................................... 5 Breathitt Formation............................................ 7 Lee Formation.................................................. 7 Study Approach..................................................... -
Understanding Vapor Diffusion and Condensation
uilding enclosure assemblies temperature is the temperature at which the moisture content, age, temperature, and serve a variety of functions RH of the air would be 100%. This is also other factors. Vapor resistance is commonly to deliver long-lasting sepa- the temperature at which condensation will expressed using the inverse term “vapor ration of the interior building begin to occur. permeance,” which is the relative ease of environment from the exteri- The direction of vapor diffusion flow vapor diffusion through a material. or, one of which is the control through an assembly is always from the Vapor-retarding materials are often Bof vapor diffusion. Resistance to vapor diffu- high vapor pressure side to the low vapor grouped into classes (Classes I, II, III) sion is part of the environmental separation; pressure side, which is often also from the depending on their vapor permeance values. however, vapor diffusion control is often warm side to the cold side, because warm Class I (<0.1 US perm) and Class II (0.1 to primarily provided to avoid potentially dam- air can hold more water than cold air (see 1.0 US perm) vapor retarder materials are aging moisture accumulation within build- Figure 2). Importantly, this means it is not considered impermeable to near-imperme- ing enclosure assemblies. While resistance always from the higher RH side to the lower able, respectively, and are known within to vapor diffusion in wall assemblies has RH side. the industry as “vapor barriers.” Some long been understood, ever-increasing ener- The direction of the vapor drive has materials that fall into this category include gy code requirements have led to increased important ramifications with respect to the polyethylene sheet, sheet metal, aluminum insulation levels, which in turn have altered placement of materials within an assembly, foil, some foam plastic insulations (depend- the way assemblies perform with respect to and what works in one climate may not work ing on thickness), and self-adhered (peel- vapor diffusion and condensation control.