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Total- and monomethyl-mercury and major ions in coastal California fog water

Results from two years of sampling on land and at sea

Bibliographic Data

ID19569047
AuthorsP S Weiss‐Penzias (0000-0001-9407-5860, University of California, Santa Cruz), Peter Weiss-Penzias, Kenneth H Coale (Moss Landing Marine Laboratories), Kenneth Coale (Moss Landing Marine Laboratories, Moss Landing, California, United States), Wesley Heim (Moss Landing Marine Laboratories, Moss Landing, California, United States), W A Heim (Moss Landing Marine Laboratories), Daniel Fernández (0000-0003-0012-2094), D M Fernandez (0000-0001-5854-0104, California State University, Monterey Bay), Andrew Oliphant, A J Oliphant (0000-0001-5824-0240, San Francisco State University), Celeste Dodge (0000-0003-0932-1911, Pepperwood Preserve, Santa Rosa, California, United States), Dave Hoskins, James Farlin (University of California, Davis), Robert Moranville (University of California, Santa Cruz), Alex Olson (0000-0002-3371-3213, Moss Landing Marine Laboratories, Moss Landing, California, United States)
EditorsJoel D Blum (0000-0001-5389-8633), Anne Soerensen
Year2016
Volume4
Publication date2016-01-01
Open AccessYes
TypeARTICLE
VenueElementa Science of the Anthropocene (JOURNAL)
Journal identifiersISSN: 2325-1026 • E-ISSN: 2325-1026
PublisherUniversity of California Press (PUBLISHER • US)
DOI10.12952/journal.elementa.000101
OpenAlexW2339402285
LanguageEN
References cited62

Marine fog water samples were collected over two summers (2014–2015) with active strand collectors (CASCC) at eight coastal sites from Humboldt to Monterey counties in California, USA, and on four ocean cruises along the California coastline in order to investigate mercury (Hg) cycling at the ocean-atmosphere-land interface. The mean concentration of monomethylmercury (MMHg) in fog water across terrestrial sites for both years was 1.6 ± 1.9 ng L-1 (<0.01–10.4 ng L-1, N = 149), which corresponds to 5.7% (2.0–10.8%) of total Hg (HgT) in fog. Rain water samples from three sites had mean MMHg concentrations of 0.20 ± 0.12 ng L-1 (N = 5) corresponding to 1.4% of HgT. Fog water samples collected at sea had MMHg concentrations of 0.08 ± 0.15 ng L-1 (N = 14) corresponding to 0.4% of HgT. Significantly higher MMHg concentrations in fog were observed at terrestrial sites next to the ocean relative to a site 40 kilometers inland, and the mean difference was 1.6 ng L-1. Using a rate constant for photo-demethylation of MMHg of -0.022 h-1 based on previous demethylation experiments and a coastal-inland fog transport time of 12 hours, a mean difference of only 0.5 ng L-1 of MMHg was predicted between coastal and inland sites, indicating other unknown source and/or sink pathways are important for MMHg in fog. Fog water deposition to a standard passive 1.00 m2 fog collector at six terrestrial sites averaged 0.10 ± 0.07 L m-2 d-1, which was ∼2% of typical rainwater deposition in this area. Mean air-surface fog water fluxes of MMHg and HgT were then calculated to be 34 ± 40 ng m-2 y-1 and 546 ± 581 ng m-2 y-1, respectively. These correspond to 33% and 13% of the rain fluxes, respectively

Cycling · Geography · Meteorology · Seawater · Air Quality and Health Impacts · Chemistry · Environmental Science · Mercury impact and mitigation studies · Toxic Organic Pollutants Impact · Environmental Chemistry · Geology · Oceanography

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