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Precursors to Particles (P2P) at Cape Grim 2006: campaign overview

journal contribution
posted on 2023-05-16, 20:59 authored by Cainey, JM, Keywood, M, Grose, MR, Krummel, PJA, Galbally, IE, Johnston, P, Gillett, RW, Meyer, M, Fraser, P, Steele, P, Harvey, M, Kreher, K, Stein, T, Ibrahim, O, Ristovski, ZD, Johnson, G, Fletcher, CA, Bigg, EK, Gras, JL
Iodine emissions from coastal macroalgae have been found to be important initiators for nucleation events at Mace Head, Ireland. The source of this iodine is the large beds of the brown kelp Laminaria digitata, which are significantly exposed at low tide. On the coast around Cape Grim, Tasmania, there are beds of the brown kelp Durvillaea potatrum. The Precursors to Particles 2006 (P2P 2006) campaign at the Cape Grim Baseline Air Pollution Station in late summer (February) 2006 focused on the role of this local kelp in providing precursor gases to particle formation. Durvillaea potatorum does not produce iodated precursor gases at the levels observed at Mace Head. IO was measured at 0.5 ± 0.3 ppt, while OIO was below detection limits (9 ppt). The dominant atmospheric iodated species was methyl iodide and the average concentration measured at the Cape Grim Station was 1.5 ± 0.3 pptv in baseline conditions, but showed significant variation in discrete samples collected immediately above the ocean surface. Nucleation events were not detected at the Cape Grim Station, except for one period where the plume of a local bushfire interacted with air of marine origin. The passage of four fronts did not result in nucleation bursts and measurements on the beach 94 m below the Cape Grim Station suggested that Durvillaea potatorum was only a weak source of new particles. © CSIRO 2007.

History

Publication title

Environmental Chemistry

Volume

4

Pagination

143-150

ISSN

1448-2517

Department/School

Institute for Marine and Antarctic Studies

Publisher

CSIRO Publishing

Place of publication

Australia

Repository Status

  • Restricted

Socio-economic Objectives

Air quality

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