The atmospheric chemistry of trace gases and particulate matter emitted by different land uses in Borneo

Author:

MacKenzie A. R.1,Langford B.12,Pugh T. A. M.1,Robinson N.3,Misztal P. K.24,Heard D. E.5,Lee J. D.6,Lewis A. C.6,Jones C. E.6,Hopkins J. R.6,Phillips G.27,Monks P. S.8,Karunaharan A.8,Hornsby K. E.8,Nicolas-Perea V.8,Coe H.3,Gabey A. M.3,Gallagher M. W.3,Whalley L. K.5,Edwards P. M.5,Evans M. J.7,Stone D.57,Ingham T.5,Commane R.5,Furneaux K. L.5,McQuaid J. B.7,Nemitz E.2,Seng Yap Kok9,Fowler D.2,Pyle J. A.10,Hewitt C. N.1

Affiliation:

1. Lancaster Environment Centre, Lancaster University, Lancaster LA1 4YQ, UK

2. Centre for Ecology and Hydrology, Penicuik EH26 0QB, UK

3. School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Manchester M13 9PL, UK

4. School of Chemistry, University of Edinburgh, Edinburgh EH9 3JJ, UK

5. School of Chemistry, University of Leeds, Leeds LS2 9JT, UK

6. Department of Chemistry, University of York, York YO10 5DD, UK

7. School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK

8. Department of Chemistry, University of Leicester, Leicester LE1 7RH, UK

9. Malaysian Meteorological Department, Jalan Sultan, Petaling Jaya, Selangor, Darul Ehsan, Malaysia

10. Centre for Atmospheric Science, Department of Chemistry, Cambridge, University, Cambridge CB2 1EW, UK

Abstract

We report measurements of atmospheric composition over a tropical rainforest and over a nearby oil palm plantation in Sabah, Borneo. The primary vegetation in each of the two landscapes emits very different amounts and kinds of volatile organic compounds (VOCs), resulting in distinctive VOC fingerprints in the atmospheric boundary layer for both landscapes. VOCs over the Borneo rainforest are dominated by isoprene and its oxidation products, with a significant additional contribution from monoterpenes. Rather than consuming the main atmospheric oxidant, OH, these high concentrations of VOCs appear to maintain OH, as has been observed previously over Amazonia. The boundary-layer characteristics and mixing ratios of VOCs observed over the Borneo rainforest are different to those measured previously over Amazonia. Compared with the Bornean rainforest, air over the oil palm plantation contains much more isoprene, monoterpenes are relatively less important, and the flower scent, estragole, is prominent. Concentrations of nitrogen oxides are greater above the agro-industrial oil palm landscape than over the rainforest, and this leads to changes in some secondary pollutant mixing ratios (but not, currently, differences in ozone). Secondary organic aerosol over both landscapes shows a significant contribution from isoprene. Primary biological aerosol dominates the super-micrometre aerosol over the rainforest and is likely to be sensitive to land-use change, since the fungal source of the bioaerosol is closely linked to above-ground biodiversity.

Publisher

The Royal Society

Subject

General Agricultural and Biological Sciences,General Biochemistry, Genetics and Molecular Biology

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