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Acid Rain - Atmospheric Chemistry - Lecture Slides, Slides of Chemistry

Major topics of Atmospheric Chemistry course are Acid Rain, Aerosol, Aerosols Optics, Geochemical Cycles, Global Models, Trop Ozone Pollution and many others. These lecture slides contain following keywords: Acid Rain, Natural Ph of Rain, United States, Chemical Composition of Precipitation, Long-Term Trend, Sulfate Wet Deposition, Aerosol Concentrations, Ammonium Wet Deposition, Nitrate Wet Deposition and Aerosol Concentrations, Trend in Frequency of Acid Rain

Typology: Slides

2012/2013

Uploaded on 08/21/2013

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NATURAL pH OF RAIN
Equilibrium with natural CO2 (280 ppmv) results in a rain pH of 5.7:
22-1
222
7
22 3 1
210
33 2
( ) 3 10 M atm
9 10 M
7 10 M
HO
H
CO g CO H O K
CO H O HCO H K
HCO CO H K









2
1/2
1
[]( )
HCO
HKKP

This pH can be modified by natural acids (H2SO4, HNO3, RCOOH…)
and bases (NH3, CaCO3) natural rain has a pH in range 5-7
“Acid rain” refers to rain with pH < 5 damage to ecosystems
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NATURAL pH OF RAIN

Equilibrium with natural CO

2

(280 ppmv) results in a rain pH of 5.7:

2

2

2

2

2

7

2

2

3

1

2

10

3

3

2

M atm

M

M

H O

H

CO

g

CO

H O

K

CO

H O

HCO

H

K

HCO

CO

H

K

2

1/ 2

1

[

]

(

)

H

CO

H

K K

P

This pH can be modified by natural acids (H

2

SO

4

, HNO

3

, RCOOH…)

and bases (NH

3

, CaCO

3

natural rain has a pH in range 5-

“Acid rain” refers to rain with pH < 5

damage to ecosystems

PRECIPITATION PH OVER THE UNITED STATES

LONG-TERM TREND IN US SO

2

EMISSIONS

Sulfate wet deposition and aerosol concentrations, 1980-2010 Leibensperger et al. [2011]

Ammonium wet deposition and aerosol concentrations, 1980- Leibensperger et al. [2011]

TREND IN FREQUENCY OF ACID RAIN (pH < 5)

Lehmann et al. [2007]

BUT ECOSYSTEM ACIDIFICATION IS PARTLY A TITRATION PROBLEM

FROM ACID INPUT OVER MANY YEARS

Acid-neutralizing capacity (ANC)

from CaCO

3

and other bases

Acid fluxF

H+

0

acidification

t

H

F

dt

ANC

Electronic structure of mercury

Mass number = 80: 1s

2 2s

2

2p

6

3s

2

3p

6

3d

10

4s

2

4p

6

4d

10

4f

14

5s

2

5p

6

5d

10

6s

2

Complete filling of subshells gives elemental Hg(0) stability, high volatility

Two stable oxidation states: Hg(0) and Hg(II)

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Orbital energies vs.

atomic number

Energetic arrangement of orbitalsis such that mercury (Z=80) hasall its subshells filled

RISING MERCURY IN THE ENVIRONMENT

Global mercury deposition has roughly tripled since preindustrial times

Dietz et al. [2009[

HUMAN EXPOSURE TO MERCURY IS MAINLY FROM FISH CONSUMPTION

Tuna is the #1 contributor

Mercury biomagnification factor

State fish consumption advisories

EPA reference dose (RfD) is 0.

μ

g kg

d

(about 2 fish meals per week)

ELEMENTAL MERCURY IS GLOBALLY DISTRIBUTED IN ATMOSPHERE

Human emission (2006)

Streets et al. [2009];Soerensen et al. [2010]

Mean Hg(0) concentration in surface air: circles = observed, background = model

Transport around

northern mid-latitudes:

1 month

Transport to southern

hemisphere: 1 year

LOCAL POLLUTION INFLUENCE FROM EMISSION OF Hg(II)

High-temperature combustion emits both Hg(0) and Hg(II)

Hg(0)

Hg(II)

GLOBAL MERCURY POOL

NEAR-FIELDWET DEPOSITION

Photoreduction?

MERCURY DEPOSITION

“HOT SPOT”

Hg(II) concentrations in surface air: circles = observed, background=model

Large variability of Hg(II) implies atmospheric lifetime of only days

against deposition

Selin et al. [2007]

Thus mercury is BOTH a global

and a local pollutant!