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What is Mercury? Naturally occurring element (atomic number 80) - PDF document

The Global Biogeochemical Mercury Cycle What is mercury? Mercury species in nature Their properties and place in the cycle How is mercury converted among its various forms? The mercury cycle: Major steps: in general


  1. The Global Biogeochemical Mercury Cycle • What is mercury? • Mercury species in nature – Their properties and place in the cycle • How is mercury converted among its various forms? • The mercury cycle: – Major steps: in general – Budget (fluxes and pools) – Major steps: details What is Mercury? • Naturally occurring element (atomic number 80) • Heavy metal, can be toxic to organisms • Only metal that is liquid at room temperature • Highest volatility of any metal • Exists in several forms – Form strongly influences • Biochemistry and bioavailability of mercury • Movement of mercury through environment Mercury Species in Nature • 3 possible valence states (electrical charge) – No charge: Hg 0 (elemental mercury, pure form) – Oxidized: Hg 1+ (mercurous, monovalent) Hg 2+ (mercuric, divalent) - more stable cation - associated with compounds: 1) - inorganic, mercury salts - examples: mercuric sulfide (HgS, mineral cinnabar), mercuric chloride (HgCl 2 ), mercuric oxide (HgO) 2) - organic (carbon-based) -example: dimethylmercury (Me 2 Hg) - more toxic than inorganic forms of Hg, bioaccumulates •1

  2. Mercury Species: Chemical properties, role in mercury cycle Form Properties Role in mercury cycle Hg 0 -not very water soluble Atmospheric transport -Inert, not reactive -volatilizes easily Hg 2+ -water soluble Wet deposition -reactive Hg p -attaches to small Deposition particles (Hg 0 attached to/adsorbed onto particles) MeHg -very water soluble Bioaccumulation -volatile -bioaccumulates, toxic Mercury Species in the Biogeochemical Mercury Cycle Note importance of: Hg 0 in atmospheric • transport – Total Hg atm ~ 95% Hg 0 • Hg 2+ , Hg p in deposition • HgS (insoluble) as sink • MeHg in bioaccumulation • Inorganic and organic complexes – Represent most of the Hg in water, soil, sediments, plants and animals http://www.ec.gc.ca/MERCURY/ EH/EN/eh-b.cfm?SELECT= EH How is Mercury Converted Among its Various Forms? • 2 main types of reactions convert mercury through its various forms: – Oxidation-reduction oxidation Hg 0 Hg 2+ reduction inert more reactive – Methylation-demethylation methylation Hg 2+ + CH 3 CH 3 Hg + demethylation •2

  3. Mercury Oxidation • Oxidation of Hg 0 in atmosphere – Important mechanism involved in deposition of mercury on land and water Hg 0 Hg 2+ Reactivity Inert More reactive Volatility High Low Solubility in water Low High Atmospheric residence time ~ 1 -1 1.5 years < 2 weeks Relevance to cycle - Emitted to atmosphere - Rapidly taken up in rain water, snow or adsorbed - Long-distance transport onto small particles (> thousands of miles before oxidized and - Subsequent deposition redeposited in environment in environment via “wet” for further cycling or “dry” deposition” Mercury Oxidation in the Arctic • Arctic phenomenon called “Mercury depletion” or “Mercury sunrise” – Occurs at end of dark polar winters when sun rises in spring – Rapid photochemical conversion of Bromine, chlorine ions (reactive chemicals released from sea salt) Hg 0 Hg 2+ Atmospheric deposited on snow/ice mercury levels (“depleted”) pulse of reactive mercury at start of growing season http://www.ec.gc.ca/science/sandemar99/article3_e.html Mercury Methylation • Methylation of Hg 2+ Hg 2+ CH 3 Hg + + CH 3 mercuric species methyl group methylmercury highly toxic bioaccumulative (builds up in living tissues, food chain) – A natural, biological process • Occurs in a variety of bacteria, especially methanogens – use enzymes containing vitamin B-12 •3

  4. Mercury Methylation – Factors influencing formation of methylmercury: • Methylating microbes – Methanogenic (methane producing) and sulfate- dependent bacteria • Anoxic/Anaerobic (oxygen poor) water and sediments – Wetlands and river sediments • Low pH (acidic) environments with high concentrations of organic matter • Temperature The Mercury Cycle The Mercury Cycle: 6 Major steps 1. Release from sources • Emission from natural and anthropogenic sources 2. Transportation and circulation • Movement in gaseous form through atmosphere 3. Deposition • On land and surface waters 4. Conversion into insoluble mercury sulfide (HgS) • Ocean sediments represent final sink 5. Bioconversion into more volatile or soluble forms such as methylmercury 6. Reentry into the atmosphere or Bioaccumulation in foodchains •4

  5. Global Mercury Budget Note: 1) Sources 2) Deposition • Local vs. regional/global 3) Global deposition • Terrestrial vs. marine 4) Atmospheric fluxes 5) Atmospheric reservoir 6) Riverine transport http://www.ec.gc.ca/MERCURY/ EH/EN/eh-mb.cfm?SELECT= EH Global Mercury Budget: some salient points • Anthropogenic emissions ≥ (greater than or exceed; estimates vary) natural releases • ~ ½ of mercury released falls out locally – Other ½ travels, changes in chemical and physical form • Most local deposition � dry particles • Global deposition � rain, snow • Long-range fallout affects terrestrial and marine ecosystems • ~ 1/2 of global deposition lands on terrestrial ecosystems; rest to marine Global Mercury Budget: some salient points • Fluxes between – Atmosphere and land, atmosphere and ocean are much greater than transport from land � ocean via riverine discharge • Mercury storage in atmospheric reservoir has increased by factor of 3 Transport rate of mercury from land � oceans has • increased by factor of 4 • Average residence time of mercury in – Atmosphere 11 days – Soil 1000 years – Oceans 3200 years 2.5 x 10 8 years – Sediments •5

  6. Global Mercury Cycle: “Pre-man” Global Mercury Cycle: Present day The Mercury Cycle: 6 Major steps 1. Release from sources Emission from natural and anthropogenic sources • 2. Transportation and circulation • Movement in gaseous form through atmosphere 3. Deposition • On land and surface waters 4. Conversion into insoluble mercury sulfide (HgS) • Ocean sediments represent final sink 5. Bioconversion into more volatile or soluble forms such as methylmercury 6. Reentry into the atmosphere or Bioaccumulation in foodchains •6

  7. Sources • “Geologic” mercury – Mercury that exists in a stable state in Earth’s crust • Active mercury cycle begins when mercury is released from this stable form through – Natural processes – Human intervention Sources: Emissions estimates • Total global mercury emissions ~ 5000t/yr – Recent scientific studies estimate ~ 50-80% mercury emitted is result of human activities; rest is natural • Estimates very uncertain – Why difficult to distinguish between natural and anthropogenic emissions? • Lack accurate data on emissions past and present • Leap-frogging – Mercury deposition and re-emission Types of Sources • Natural • Anthropogenic – Direct – Re-emitted • We emitted years ago • Land, surface waters re-emitted mercury into atmosphere http://www.epa.gov/mercury/control_emissions/global.htm •7

  8. Natural sources of Mercury • Mercury – Occurs naturally throughout our solar system – On Earth • Geological deposits – cinnabar (HgS mineral) up to 86% Hg – Rocks » Granite 0.2 ppm Hg » Other crustal rocks 0.1 ppm Hg http://www.ec.gc.ca/MERCURY/ SM/EN/sm-ns.cfm?SELECT= SM Natural Sources of Mercury • Natural processes can release mercury from crust to water, soil, atmosphere – Examples: • Volcanic eruptions • Weathering of rocks • Under sea vents • Hot springs • Mercury also concentrates in – Plants – Sediments rich in organic matter – Fossil fuels (examples: coal, oil) http://www.pollutionprobe.org/Reports/mercuryprimer.pdf Natural sources of Mercury • As mercury is incorporated in biosphere, releases attributed to – Vegetation – Forest fires – Water bodies – Sea salt spray – Soils •8

  9. Natural sources of Mercury • Natural emission from continental sources 1000 t/yr • Evasion from oceans – Pre-industrial 600 t/yr – Today 2000 t/yr • Higher due to re- emission of mercury deposited from human activities http://www.ec.gc.ca/MERCURY/ EH/EN/eh-mb.cfm?SELECT= EH Anthropogenic Sources • Types of anthropogenic releases – Incidental release • Result of an activity that does not involve direct/deliberate use of mercury • Examples: burning coal, processing metals (Cu, Zn), generate electricity from energy sources (coal, other fossil fuels), cremation – Direct/deliberate release • Deliberate use of mercury in products and processes • Examples: intentional extraction, electrical switches Presence of Mercury from Deliberate Uses in Canada •9

  10. Canadian Anthropogenic Mercury Emissions by Source (2001) • Coal fired power and heat production – Largest single source of mercury emissions http://pubs.acs.org/hotartcl/est/98/apr/4903hanB.ev.html U.S. Anthropogenic Emission Sources (1994-1995) Coal-fired utility boilers - Largest point source of mercury emissions Electric utilities, Municipal waste combustors, Commercial/industrial boilers, Medical waste incinerators ~ 80 % of total amount http://pubs.acs.org/hotartcl/est/98/apr/mer.html Worldwide distribution of emissions • Asia ~ ½ • US anthropogenic mercury emissions ~ 3% of global total • Emissions from US power sector ~ 1% of total global emissions http://www.epa.gov/mercury/control_emissions/global.htm •10

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