Open AccessVertical profiling and determination of landscape fluxes of biogenic nonmethane hydrocarbons within the planetary boundary layer in the Peruvian Amazon
Author(s) -
Helmig Detlev,
Balsley Ben,
Davis Kenneth,
Kuck Laura R.,
Jensen Mike,
Bognar John,
Smith Tyrrel,
Arrieta Rosaura Vasquez,
Rodríguez Rodolfo,
Birks John W.
Publication year - 1998
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 - 10.1029/98jd01023
Subject(s) - isoprene , environmental chemistry , aerosol , flame ionization detector , environmental science , chemistry , methacrolein , volatile organic compound , atmospheric sciences , gas chromatography , chromatography , geology , organic chemistry , monomer , copolymer , methacrylic acid , polymer
Vertical profiles of volatile organic compounds (VOCs) within the convective 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 were observed for isoprene, followed by α‐pinene, p ‐cymene, and β‐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‐methylfuran were observed throughout the CBL. Besides the ubiquitous chlorofluorocarbons, anthropogenic VOC concentrations were at the lower end of concentration ranges observed in rural air. From the vertical profiles, BVOC surface flux estimates were derived. Emission rates were estimated from five vertical profiles using the mixed‐layer gradient and CBL budget methods. Emission estimates varied depending on method and choice of statistics, but were within 3000–8200 μg compound m −2 h −1 for isoprene, 120–370 μg m −2 h −1 for α‐pinene, 40–75 μg m −2 h −1 for β‐pinene, about 16 μg m −2 h −1 for p ‐cymene, and 40–50 μg m −2 h −1 for camphene. The changes in the ratios of MAC and MVK to isoprene with altitude were utilized to estimate the mixing times between the surface layer, mixed layer and lower troposphere.