Open AccessFossil and contemporary fine particulate carbon fractions at 12 rural and urban sites in the United States
Author(s) -
Schichtel Bret A.,
Malm William C.,
Bench Graham,
Fallon Stewart,
McDade Charles E.,
Chow Judith C.,
Watson John G.
Publication year - 2008
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2007jd008605
Subject(s) - radiocarbon dating , carbon fibers , particulates , total organic carbon , environmental science , carbon cycle , geography , physical geography , environmental chemistry , chemistry , archaeology , ecology , materials science , organic chemistry , ecosystem , composite number , composite material , biology
Fine particulate matter collected at two urban, four near‐urban, and six remote sites throughout the United States were analyzed for total carbon (TC) and radiocarbon ( 14 C). Samples were collected at most sites for both a summer and winter season. The radiocarbon was used to partition the TC into fossil and contemporary fractions. On average, contemporary carbon composed about half of the carbon at the urban, ∼70–97% at near‐urban, and 82–100% at remote sites. At Phoenix, Arizona, and Seattle, Washington, one monitor was located within the urban center and one outside to assess the urban excess over background concentrations. During the summer the urban and rural sites had similar contemporary carbon concentrations. However, during the winter the urban sites had more than twice the contemporary carbon measured at the neighboring sites, indicating anthropogenic contributions to the contemporary carbon. The urban fossil carbon was 4–20 times larger than the neighboring rural sites for both seasons. Organic (OC) and elemental carbon (EC) from TOR analysis were available. These and the radiocarbon data were used to estimate characteristic fossil and contemporary EC/TC ratios for the winter and summer seasons. These ratios were applied to carbon data from the Interagency Monitoring of Protected Visual Environments network to estimate the fraction of contemporary carbon at mostly rural sites throughout the United States. In addition, the ratios were used to develop a semiquantitative, lower bound estimate of secondary organic carbon (SOC) contribution to fossil and contemporary carbon. SOC accounted for more than one‐third of the fossil and contemporary carbon.