Mercury in the Atmosphere Thomas M. Holsen Clarkson University - - PowerPoint PPT Presentation
Mercury in the Atmosphere Thomas M. Holsen Clarkson University - - PowerPoint PPT Presentation
Mercury in the Atmosphere Thomas M. Holsen Clarkson University Outline Outline Sources of Atmospheric Hg Sources of Atmospheric Hg Anthropogenic Anthropogenic vs vs natural natural Anthropogenic sources
Outline Outline
- Sources of Atmospheric Hg
Sources of Atmospheric Hg
- Anthropogenic
Anthropogenic vs vs natural natural
- Anthropogenic sources
Anthropogenic sources
- Forms of Hg in the atmosphere
Forms of Hg in the atmosphere
- Hg concentrations in NYS
Hg concentrations in NYS
- Hg deposition processes
Hg deposition processes Acknowledgements Acknowledgements – – C Driscoll, M Cohen, NY DEC, YJ C Driscoll, M Cohen, NY DEC, YJ Han, S Lai, J Han, S Lai, J Pagano Pagano, M Milligan , M Milligan
Global Sources of Mercury Global Sources of Mercury to the Atmosphere (in metric tons per year) to the Atmosphere (in metric tons per year)
Source Source Seigneur et Seigneur et
- al. 2004
- al. 2004
Bergan Bergan et al. et al. 1999 1999 Mason & Mason & Sheu Sheu 2002 2002 Direct Anthropogenic Direct Anthropogenic 2143 2143 2160 2160 2400 2400 Recycled Anthropogenic Recycled Anthropogenic 2134 2134 2000 2000 2090 2090 Total Anthropogenic 4277 4160 4490 Natural Natural 2134 2134 1900 1900 2110 2110 Total (% of Anthropogenic Origin) 6411 (67%) 6060 (69%) 6600 (68%) from C. Driscoll
U.S. Emissions of Mercury
50 100 150 200 250 TPY 1990 Emissions 1996 Emissions 1999 Emissions
Other Non-MACT Other MACT Hazardous Waste Incineration Chlorine Production Industrial Boilers Municipal Waste Combustors Medical Waste Incinerators Utility Coal Boilers
210 185 118
U.S. Anthropogenic Emissions of Mercury
Source: EPA 1990, 1996 NTI and EPA 1999 NEI. Short tons per year.
From M. Cohen
Based on 1999 NEI
From YJ Han
Atmospheric Mercury Species Atmospheric Mercury Species
Elemental Mercury (Hg0)
Predominant species, Long range transport Globally distributed, 0.5 to 2 years residence time
Gaseous divalent mercury (RGM, Hg2+, )
Oxidized mercury: Hg(II) : HgCl2, other species? Highly water soluble -> short atmospheric life time (0.5-2 days) Local and Regional effects
Particulate Mercury (Hgp)
Species largely unknown – probably Hg(II) Local and Regional Effects (0.5-2 days)
Estimated Speciation Profile for U.S. Estimated Speciation Profile for U.S. Atmospheric Mercury Emissions (1999) Atmospheric Mercury Emissions (1999)
RGM
Simplified Mercury Cycle from C. Driscoll
Hg sampling sites in NYS Hg sampling sites in NYS
+ Potsdam
+ Sterling
+ Stockton
Potsdam and Stockton funded by NYSERDA, Potsdam and Stockton funded by NYSERDA, Sterling by US EPA Sterling by US EPA
Sterling, NY Sterling, NY
Between Oswego and Rochester on a bluff overlooking the lake
Manual Air Sampling Manual Air Sampling
TGM: Adsorption into Gold traps RGM: Annular Denuder coated by KCl
Monthly Average TGM Concentrations, ng/m Monthly Average TGM Concentrations, ng/m3
Date
May 00 July 00 May 01 July 01 Sep 01 Nov 01 Jan 02 Mar 02 May 02 July 02 Sep 02 Nov 02 Jan 03 Mar 03
TVM Concentrations (ng m-3)
- 6
- 4
- 2
2 4 6 8 10 12 Stockton site Potsdam site Sterling site
Daily TGM Concentrations, ng/m Daily TGM Concentrations, ng/m3
3
TGM Concentration
0.00 10.00 20.00 30.00 40.00 50.00 60.00 70.00 80.00 90.00 12/6/1999 4/19/2001 9/1/2002 1/14/2004 5/28/2005 10/10/2006 Date Concentration, ng m-3 Potsdam Stockton Sterling
Daily RGM Concentrations, pg/m Daily RGM Concentrations, pg/m3
3
RGM Concentration
0.00 10.00 20.00 30.00 40.00 50.00 60.00 70.00 80.00 90.00 Date 5/14/2002 7/7/2002 8/30/2002 10/11/2002 12/4/2002 1/27/2003 3/22/2003 5/15/03 7/8/03 8/31/03 10/24/03 12/17/03 2/9/04 Date Concentration, pg m-3 Potsdam Stockton Sterling
Computation of Trajectories Computation of Trajectories -
- HYSPLIT4
HYSPLIT4
- NOAA Model
NOAA Model
- Predicts history of
Predicts history of air movement air movement
Potential Source Contribution Function Potential Source Contribution Function (PSCF) (PSCF)
Sampling site Cell 1 Cell 1 Cell 2 Cell 2 Back-trajectory representing high concentration PSCF value Cell 1 = 2/3 Cell 2 = 0/2 Back-trajectory representing low concentration
JP JP-
- PSCF result for TGM measurements taken in Potsdam,
PSCF result for TGM measurements taken in Potsdam, Stockton, and Sterling in NY Stockton, and Sterling in NY
Tekran Automated Speciation System –
highly time resolved concentrations
Hg concentrations obtained with a Hg concentrations obtained with a Tekran Speciation System Tekran Speciation System
05/14/05 05/18/05 05/22/05 05/26/05 05/30/05 06/03/05 06/07/05 06/11/05 06/15/05 06/19/05 06/23/05 06/27/05 07/01/05 07/05/05 07/09/05
Elemental Hg [ng m-3]
0.0 0.5 1.0 1.5 2.0 2.5 3.0
RGM & Particulate Hg [pg m-3]
- 2
2 4 6 8 10 12 14 Elemental Hg Reactive gaseous Hg Particulate Hg
Relationship between Relationship between Hg and SO Hg and SO2
2
concentrations in concentrations in Rochester, NY Rochester, NY Data from NY DEC Data from NY DEC
Hg Deposition Processes Hg Deposition Processes
- Wet deposition
Wet deposition – – Hg associated with rain, dew, Hg associated with rain, dew, snow, fog (mostly RGM) snow, fog (mostly RGM)
- Particle dry deposition
Particle dry deposition – – Hg associated with Hg associated with atmospheric particles (mostly RGM) atmospheric particles (mostly RGM)
- Air
Air-
- surface exchange (water and vegetation)
surface exchange (water and vegetation)
- RGM deposition only
RGM deposition only
- Hg(0) deposition and emission
Hg(0) deposition and emission
Deposition Processes
Air-water exchange Wet deposition (RGM, Hg(p)) Dry particle deposition (Hg(p)) Wet and dry deposition, stomata uptake RGM, Hg(0) RGM → Hg(0) Hg(0) litterfall throughfall
Mercury Deposition Mercury Deposition
- Predominant source of mercury in most
Predominant source of mercury in most watersheds is atmospheric deposition ( watersheds is atmospheric deposition (Lindqvisit Lindqvisit et al. 1991; Mason 1994). et al. 1991; Mason 1994).
- Deposition of mercury has increased two to three
Deposition of mercury has increased two to three-
- fold over the past two centuries, with some
fold over the past two centuries, with some locations exhibiting greater than a twenty fold locations exhibiting greater than a twenty fold increase ( increase (Meili Meili 2003; 2003; Nriaguand Nriaguand Becker 2003). Becker 2003).
From C. Driscoll
Historical deposition of mercury to sediments in West Pond and Historical deposition of mercury to sediments in West Pond and Little Echo Pond in the Adirondack region ( Little Echo Pond in the Adirondack region (Lorey Lorey and Driscoll, and Driscoll, 1999) 1999)
Regional and Global Contributions to Total Hg Regional and Global Contributions to Total Hg Deposition to the Catskill, NY Receptor Site Deposition to the Catskill, NY Receptor Site
USA Canada
- S. America
Europe Africa Asia Natural
60% 16% 13% 5% 2% 2% 2% Seigneur et al. 2002 for NYSERDA
(A) Precipitation Depth (mm) (B) Hg concentration in precipitation (ng L-1) (C) Hg wet deposition flux (µg m-2)
Event Event-
- based wet
based wet deposition Potsdam, deposition Potsdam, NY, Sept. 2003 NY, Sept. 2003 – – Apr. Apr. 2004) 2004)
Sponsored by NYSERDA and US Sponsored by NYSERDA and US EPA EPA
PSCF result for wet deposition PSCF result for wet deposition
PSCF value (max intensity, mean) 0.1 - 0.2 0.2 - 0.3 0.3 - 0.5 0.5 - 0.7 0.7 - 1
Based on 1999 NEI
From YJ Han
Dry Deposition Dry Deposition
Difficult to measure Function of surface type, Hg species, particle size,
meteorological conditions
Modeled as product of particle concentration and
deposition velocity, Flux = Vd × Hg(p)
Generally thought to be equal to or greater than wet
deposition
Area that needs additional research
Air Air-
- Water Exchange
Water Exchange
- f Hg
- f Hg0
= K = KOL
OL (
(C Cd
d-
- C
Ca
a/H)
/H)
KOL: mass transfer coeff. C Cd
d –
– dissolved dissolved concentration concentration Ca Ca – – air concentration air concentration H – Henry’s Law constant → RGM - deposition only → Hg(0) - deposition and evasion
Hg Mass Balance for Lake Ontario Hg Mass Balance for Lake Ontario
Conclusions Conclusions
- There are significant anthropogenic emissions of
There are significant anthropogenic emissions of Hg Hg – – biggest source in US is utility coal biggest source in US is utility coal combustion combustion
- The form of Hg in the atmosphere controls its
The form of Hg in the atmosphere controls its fate and transport fate and transport
- There is evidence that North America sources