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. 2015 May 7;8(3):243–263. doi: 10.1007/s11869-015-0338-3

Table 3.

Examples of OM/OC ratio determined in various studies at urban and remote locations

Study Particle size Method/descriptiona OM/OC (ratio) Location Season (sampling period)
Urban/sub-urban Remote
Krivacsy et al. (2001) PM2.5 Used total organic carbon (TOC) analyzer to determine TC and WSOC 1.9 High alpine research station, Jungfraujoch, Switzerland (in the Swiss alps; elevation 3580 m above sea level (asl)) July to August 1998
Used solid-phase extraction on a copolymer sorbent
Analyzed C, H, N, and S of OM by elemental analyzer with estimated O
Determined OM mass by gravimetry
Kisset al. (2002) PM1.5 Used total organic carbon (TOC) analyzer to determine TC and WSOC 1.93 ± 0.038 (ranged from 1.9 to 2.0) Rural K-puszta site with mixed forest, Hungary January to September 2000
Used solid-phase extraction on a copolymer sorbent
Analyzed C, H, N, and S of OM by elemental analyzer with estimated O
Determined OM mass by gravimetry
Maria et al. (2002, 2003) PM1 Calculated OC and OM from FTIR and compare with thermal/optical OC 1.27 ± 0.02 to 1.49 ± 0.28 Aircraft sampling over northeast Asia during the ACE-Asia Campaign April and May 2001
A 4-solvent rinsing procedure was used to separate functional groups into fractions of increasing hygroscopicity
Used carbon monoxide (CO) vs. FTIR OC ratios to classify back trajectory clusters into 10 groups
Russell (2003) Submicron PM FTIR, estimated OC from the number of carbon bonds and OM from the molecular mass of each functional group 1.36 ± 0.13 (1.2–1.6) Aircraft and ship-based sampling in the Caribbean and northeastern Asiab March to April and July 2001
El-Zanan et al. (2005) PM2.5 After sequential solvent extraction with dichloromethane, acetone, and water, the dried residue was weighed for OM and analyzed for OC by TOR OC. The water extracts were also analyzed for ions (Cl-, NO3 -, SO4 =, Na+, K+, and NH4 +) to subtract inorganic ion mass. 1.92 ± 0.40 (1.58–2.58) 2.07 by mass balance U.S. National Parks (5 sites)c Annual (1988–2003)
Zhang et al. (2005) PM1 Inorganic ions (e.g., sulfates, nitrates, ammonium) and organics by AMS, followed by deconvolution of AMS mass spectrum to identify HOAs and OOAs. Averaged 1.8 with 1.2 for HOA and 2.2 for OOA Pittsburgh, PA September 2002
Yu et al. (2005a, b) PM1.5 Used water and solvent extraction followed by GC/MS analysis for WSOC and solvent-soluble OC Daytime 2.0 ± 0.3 (1.4–2.5). Nighttime 1.8 ± 0.2 (1.3–2.0) Great Smoky Mountains National Park, TN July to August 2005
Chen and Yu (2007) PM2.5 Determined OM by combining heating, gravimetric, and chemical constituents 2.1 ± 0.3 Sub-urban site at Clearwater, Hong Kong October 2003 to June 2005
Gilardoni et al. (2007) PM1 FTIR and comparison with IC-PILS for speciated carboxylic acids 1.4 ± 0.12 Aircraft sampling of Ohio power plant emissions and regional background (12 flights) Summer 2004
1.6 ± 0.4 Ship sampling in the Gulf of Maine
1.5 ± 0.16 Appldore Island, ME
1.6 ± 0.14 Chebogue Point, Nova Scotia, Canada
Reff et al. (2007) PM2.5 FTIR for aliphatic (CH) and carbonyl (C=O and [(C=O)−OH] by partial least squares (PLS) equation Outdoor 1.7–2.6 219 non-smoking homes in LA county, CA, Elizabeth, NJ, and Houston, TX Summer 1999 to Spring 2001
Indoor 1.3–1.7 (average 1.45 ± 0.17)
Personal 1.3–1.6 (average 1.4 ± 0.11)
Aiken et al. (2008) PM1 Elemental analysis by AMS Average 1.71 with 1.2–1.3 for HOA, 1.85–2.45 for OOA; and 1.6–1.7 for BBOA Mexico City, Mexicod March 2006
Cozic et al. (2008) PM1 OM by Q-AMS, normalized to OC by OC/EC TOT carbon analyzer 1.84 Jungfraujoch, Switzerland February and March 2005
Polidori et al. (2008) PM2.5 Used a combination of polarity-based extraction/fractionation method, determine OM by gravimetry and OC by thermal/optical analysis (polarity generally increases as organic oxygen content increases) OM/OC ratios increase with increasing polarity: 1.37 for hexane, 1.66 for dichloromethane, 1.89 for ethyl acetate, 2.11 for acetone, and 2.25 for methanol extractions. Annual average ratios with (OM/OCtotal) and without (OM/OCextract) non-extractable material were 2.05 ± 0.18 and 1.91 ± 0.24, respectively Pittsburgh, PA Annual (July 2001–July 2002)
Gilardoni et al. (2009) PM1 FTIR 1.8 Mexico City, Mexico March 2006
2.0 Altzomoni (60 km SE of Mexico City, Mexico)
Day et al. (2010) PM1 FTIR and comparison of OM with Q-AMS 1.66e La Jolla, CA February and March 2009
Hawkins and Russell (2010) PM1 FTIR and comparison with Q-AMS 1.55 ± 0.17 La Jolla, CA June to September 2008
Takahama et al. (2011) Submicron PM FTIR and comparison with ACSM 2.0–2.2 Whistler Mountain, BC, Canada March and April 2009
1.6–1.8 Aircraft sampling over Mexico and the Gulf of Mexico coast (12 flights) May to September 2009
Ruthenburg et al. (2014) PM2.5 FTIR 1.83 Mesa Verde, CO Annual (2011) at seven IMPROVE sites
1.79 Olympia, WA
1.78 Proctor Maple R.F., VT
1.71 St. Marks, FL
1.73 Trapper Creek, AK
1.56 Phoenix, AZ

PM particulate matter, PM x PM with diameter smaller than x micrometers at 50 % cut-point, HOA hydrocarbon-like organic aerosol (represent gasoline and diesel engine exhaust emissions), OOA oxygenated organic aerosol (contains more oxygen atoms than HOAs, resemble humic-like substance, and have been associated with secondary organic aerosol), BBOA biomass burning organic aerosol

aMeasurement methods include aerosol chemical speciation monitor (ACSM), aerodyne aerosol mass spectrometer (AMS), quadrupole-aerosol mass spectrometer (Q-AMS), ion chromatography-particle into liquid sampler (IC-PILS), Fourier transform infrared analysis (FTIR), total carbon (TC), thermal/optical reflectance (TOR), thermal/optical transmittance (TOT), water-soluble organic carbon (WSOC), water-soluble organic matter (WSOM)

bDuring the aerosol characterization experiment (ACE)-Asia study in the western Pacific and the Passing Efficiency of the Low Turbulence Inlet Experiment (PELTI) study in the Caribbean

cSites are Acadia, ME; Great Smoky Mountains, TN; Big Bend, TN; Indian Gardens, Grand Canyon, AZ; and Mount Rainier, WA

dDuring the Megacity Initiative: Local and Global Research Observations (MILAGRO) field campaign, ground-based sampling was done at the T0 Supersite at the Instituto Mexicano del Petróleo (IMP) and aircraft data were collected aboard the NCAR C-130 aircraft over the city

eEstimated based on the sum of carbon mass in the functional groups (Russel 2003)