MEASUREMENT OF TOTAL NONMETHANE ORGANIC-CARBON (C-Y) - DEVELOPMENT AND APPLICATION AT CHEBOGUE POINT, NOVA-SCOTIA, DURING THE 1993 NORTH-ATLANTIC REGIONAL EXPERIMENT CAMPAIGN
Jm. Roberts et al., MEASUREMENT OF TOTAL NONMETHANE ORGANIC-CARBON (C-Y) - DEVELOPMENT AND APPLICATION AT CHEBOGUE POINT, NOVA-SCOTIA, DURING THE 1993 NORTH-ATLANTIC REGIONAL EXPERIMENT CAMPAIGN, J GEO RES-A, 103(D11), 1998, pp. 13581-13592
A technique was developed for the measurement of total nonmethane orga
nic carbon (C-y) in the gas phase based on cryogenic collection, prese
paration of CO, CH4, and CO2, conversion of all carbon to CH4, and mea
surement by flame ionization detector. Collection and recovery efficie
ncies were found to be essentially quantitative for C-2-C-7 hydrocarbo
ns and better than 95 and 93% for methanol and formaldehyde, respectiv
ely. CO2 prevented the measurement of the C-2 hydrocarbons in atmosphe
ric samples, and system response to ambient water vapor limited the pr
ecision of the measurement at very low C-y. The measurement system had
an estimated uncertainty of 10% at ambient mixing ratios of 100 ppb C
, and a detection limit of between 5 and 7 ppb C. C-y was measured in
Boulder, Colorado, during June of 1993 and at Chebogue Point, Nova Sco
tia, during the North Atlantic Regional Experiment intensive campaign,
August to September 1993. C-y values ranged from several hundred ppb
C to 11 ppb C in Boulder, and from 177 to below 5 ppb C at Chebogue Po
int, with medians of 55 and 11 ppbC, respectively. C-y was found to co
rrelate with both CO and O-3 at higher levels of those two pollutants.
The sum of C-y and the C-2 hydrocarbons was virtually always equal to
or greater than the sum of the hydrocarbons. Several exceptions to th
is occurred when high HC values were observed in cannister samples but
not C-y measurements. These instances were attributed to short-term p
erturbations from local sources. There was a net difference between to
tal nonmethane organic carbon and the sum of hydrocarbons and carbonyl
s of 3.5 +/- 7.8 ppb C overall. This difference appears to be broadly
correlated with anthropogenic pollution. There does not appear to be a
significantly large reservoir of reactive carbon unaccounted for by h
ydrocarbon or carbonyl measurements.