VERTICAL PROFILING AND DETERMINATION OF LANDSCAPE FLUXES OF BIOGENIC NONMETHANE HYDROCARBONS WITHIN THE PLANETARY BOUNDARY-LAYER IN THE PERUVIAN AMAZON
D. Helmig et al., VERTICAL PROFILING AND DETERMINATION OF LANDSCAPE FLUXES OF BIOGENIC NONMETHANE HYDROCARBONS WITHIN THE PLANETARY BOUNDARY-LAYER IN THE PERUVIAN AMAZON, J GEO RES-A, 103(D19), 1998, pp. 25519-25532
Vertical profiles of volatile organic compounds (VOCs) within the conv
ective boundary layer (CBL) were measured at a tropical forest site in
the Peruvian Amazon during July 1996 from a tethered balloon sampling
platform. A profiling technique based on the collection of VOCs onto
solid adsorbent cartridges was used to take samples at altitudes up to
1600 m above ground. VOC analysis was performed by thermal desorption
with gas chromatographic separation and mass spectrometric and flame
ionization detection. A total of 26 VOCs were structurally identified.
VOCs were dominated by biogenic compounds. Highest concentrations wer
e observed for isoprene, followed by alpha-pinene, p-cymene, and beta-
pinene. Combined, all monoterpenes accounted for approximately 15-20%
of the total carbon from biogenic VOCs (BVOCs). The isoprene oxidation
products methacrolein (MAC), methylvinylketone (MVK), and 3-methylfur
an were observed throughout the CBL. Besides the ubiquitous chlorofluo
rocarbons, anthropogenic VOC concentrations were at the lower end of c
oncentration ranges observed in rural air. From the vertical profiles,
BVOC surface flux estimates were derived. Emission rates were estimat
ed from five vertical profiles using the mixed-layer gradient and CBL
budget methods. Emission estimates varied depending on method and choi
ce of statistics, but were within 3000-8200 mu g compound m(-2) h(-1)
for isoprene, 120-370 mu g m(-2) h(-1) for alpha-pinene, 40-75 mu g m(
-2) h(-1) for beta-pinene, about 16 mu g m(-2) h(-1) for p-cymene, and
40-50 mu g m(-2) h(-1) for camphene. The changes in the ratios of MAC
and MVK to isoprene with altitude were utilized to estimate the mixin
g times between the surface layer, mixed layer and lower troposphere.