Hg
Hg
Chapter 11: Atmospheric mercury
A brief human history of mercury poisoning
Qin Shi Huang,
1st emperor of China
Mad hatters
Minimata disaster
Karen Wetterhahn,
Dartmouth professor
Iraq grain disaster
200 BC
19th-20th century
1950s
1971
1997
The perils�of eating too much fish
Jeremy Piven, actor
Richard Gelfond IMAX CEO
Both hospitalized for extended time due to mercury poisoning
from daily fish consumption over many years
Mercury from fish consumption: a global environmental issue
Children IQ deficits (fetal exposure)
Well-established
$8 billion per year cost in US
Adult cardiovascular, fertility effects
Suspected
EPA reference dose (RfD): 0.1 μg kg-1 d-1 (about 2 fish meals per week)
Hg (mg/kg)
Tilefish
Shark
Swordfish
Orange Roughy
Marlin
Canned Tuna (alb)
Bluefish
Grouper, Rockfish
Scorpionfish
Halibut
Sea trout
Sablefish
Lobster
Snapper
Lobster
Mackerel
Skate
Canned Tuna (lt)
Cod
Croaker
Squid
Whitefish
Pollock
Crab
Mercury biomagnification factor
Salmon
Mercury (Hg) is present in atmosphere as an elemental gas – �an amazing property shared only with noble gases
Mass number = 80: 1s2 2s2 2p6 3s2 3p6 3d10 4s2 4p6 4d10 4f14 5s2 5p6 5d10 6s2
to produce Hg(II) (mercuric) compounds
6s2
oxidation
Hg(0)
Hg(II)
reduction
elemental
mercury
mercuric
compounds
Biogeochemical cycle of mercury: critical role of atmosphere
Hg(0)
Hg(II)
particulate
Hg
burial
SEDIMENTS
uplift
volcanoes
erosion
oxidation
Hg(0)
Hg(II)
reduction
biological
uptake
ANTHROPOGENIC
PERTURBATION:
fuel combustion
mining
~20x natural
ATMOSPHERE
OCEAN/SOIL
VOLATILE
WATER-SOLUBLE
Atmosphere enables global transport of mercury
Observed variability of atmospheric Hg implies an atmospheric lifetime against deposition of 0.5 years
Implies gPresent-day cale transport of anthropogenic emissions
Present-day emission of mercury to atmosphere from coal and mining
UNEP [2013]; Shah et al. [2021]
Mercury wet deposition is controlled by global transport
EPA deposition data (circles), model (background)
Global Hg(II) pool
scavenging
Florida T-storm
Highest mercury deposition in US is along the Gulf Coast,
where thunderstorms scavenge globally transported mercury from high altitudes
Selin and Jacob [2008]
How to oxidize Hg(0) to Hg(II) in the atmosphere?
Radical oxidant X ≡ OH, Br
Shah et al. [2021]
Sources of bromine atoms
ocean plankton
CHBr3
bromoform
OH
weeks
deposition
Br
HBr
BrO
O3
CH4
hv
plankton
sea-salt aerosol
Br--
Br2
hv
HOBr
hv
HO2
Shah et al. [2021]
as simulated by GEOS-Chem model
UNEP Minimata Convention on Mercury (2017)�
for coal-fired power plants
Global biogeochemical cycling of mercury: major processes
Global biogeochemical model for mercury
thermocline
Grasshopper effect:�cycling between atmosphere/land/ocean keeps mercury in environment
Amos et al. [2014]
Reservoir fraction
Fate of an atmospheric pulse emitted at time zero:
Atmosphere
Surface soils
Deep soils
Surface/subsurface ocean
Coastal sediments
Deep sediments
Deep ocean
mercury
deep ocean
rivers
SEDIMENTS
Land
Ocean
0
What can we hope from the Minimata Convention?
Effect of zeroing
all human emissions
by 2015
Zeroing human emissions right now would decrease ocean mercury by 50% by 2100, while keeping emissions constant would increase it by 40%
Amos et al. [2013, 2014]
The wild card of climate change:�potential mobilization of the large soil mercury pool
Global soils: 240,000 tons mercury
Oceans: 350,000 tons
Atmosphere: 5,000 tons
Increasing soil respiration
due to warmer temperature
Climate change may be as important as emission controls
for the future of environmental mercury in the century ahead.