Title: Non Criteria Atmospheric Pollutants International Perspectives
1NATURAL POLLUTERS VOLCANOES FORESTS COASTS DESERTS
Free Flowering MakinMagic
219thC ENVIRONMENTAL SETTING
- Fogs, cholera, sewage
- Krakatoa 1883
- Blood Rain 1903
- Tunguska 1908
- Halleys comet 1910
- End of guano
- Dramatic sunsets world-wide Ascroft sketches for
Symons Report
3TUNGUSKA 1908
High temperatures at the head of the Meteor
cause a Zeldovic type reaction N O2 ? NO O
- Widespread atmospheric observations of night-
glow - O3 loss
The nitric oxide then destroys ozone layer NO
O3 ? NO2 O2 Acid Rain!
4HALLEY'S COMET (1910)
- Spectra of comet tail showed hydrogen, water
- In addition poisonous CO and CN which caused
public concern as the Earth would pass through
Halley's tail!
5DMS
nM
- Seasonal cycles of DMS production from
phyto-planktonic blooms - Southern Ocean an important region
- Acid rain in coastal regions? Data Andrea et
al
12
JAN
6
JUL
0
6CLAW Hypothesis
- CCN from marine DMS increases albedo
and lowers temperature. This in turn might
feedback by lowering planktonic growth and
lessening DMS and CCN production - Gaia hypothesis postulates such
geo-physiological control
7SEASALT
- Large amounts of sea spray but mostly from bubble
bursting not spume - Microlayer enrichment of metals
- Reactions with acids e.g. H2SO4 2NaCl
? Na2SO4 2HCl? - Asthmatic effects?
8AGRICULTURAL EFFECTS
- Aeolian erosion of sulfate containing
dusts - Grazing increased in last few millennia
- Ploughing
- River-diversion
- Forest fires
9AGRICULTURE
-
- Grazing increased in last few millennia
- Ploughing
- River-diversion
- Forest fires
- Dispersive sources
- Ploughing
- Pesticides
- Pollen dispersal
Aeolian erosion of sulfate containing dusts
10LIGHTNING
- Shock
- N2 O2 ? 2NO
- NO3- in rain
- Artificial fertilizers
11Mary Shellys Frankenstein
- Tambora Eruption1815 and the year without a
summer
12RATE OF ACID RAIN FORMATION
- Different rates of conversion of HCl, HF and SO2
to soluble acids affects rainfall acidity - Mercury also important
1000 km
13VOG
- Volcanic fog (or vog) can be hazardous to human
health and crops
Threats in HawaiI, Costa Rica etc
Vog from Pu'u O'o www.geosci.unc.edu/.../VolcanicH
azards.html
14DUST VEIL INDEX
- Climate may be affected by volcanic dust, but
sulfur may be more important - Residence time
15AIRCRAFT IN FLIGHT
- Volcanic ash particles can severely damage
aircraft and lead to engine failure. -
16GALUNGGUNG VOLCANO INDONESIA, 1982.
- BA 747 on a flight from Kuala Lumpur, Malaysia,
to Perth, Australia encountered ash from this
eruption and lost thrust from all four engines
and descended from 36,000 ft to 12,500 ft before
all four engines were restarted. - All four engines replaced
17DUST CHEMISTRY
Typically treated as an inert matrix, but rare to
include inorganic or rarer organic chemistry
NEUTRALIZATION
OZONE INTERACTIONS
SOLUBILZATION
DUST EMISSION
18TAIWAN DUST RECORD SEDIMENTS FROM LAKE
- Notable increase in flux
- dry periods since 1340
- Cold/dry and frequent dust storms 500, 700,
900 1350, 1500... Lou JY et al, Science in
China D (1997)
Flux to anoxic lake mg cm-2 y-1
Chen-Tung Chen et al
19SIZE
BEFORE
Coarse mode increases during dust storms
18 to 20 March 2002
DURING
Lee, C.-T et al. Atmospheric Environment (2006)
20SUDANDUST
Initially bulk composition reflects soil Little
evidence of chemistry
21URBAN INTERACTIONSUPTAKE OF ORGANIC MATERIALS
- oleic acid and linoleic acid in the aerosols
suggested cooking main source of fatty acids in
urban areas - PAHs and fatty acids decreased sharply after the
dust storm
Hou, X. et al. Atmospheric Environment (2006)
22PAH ONSILICA
Perraudin et al (2007)
23INORGANIC REACTIONS
- affect pH
- calcium is a dominant soluble ion
- secondary transformation of sulfate and nitrate
on dust
Rodhe H. EST (2002) Wang, Y. et al.
Atmospheric Environment (2005)
24HUMICACIDS
- high molecular weight compounds
- carboxylic and phenolic functional groups
http//www.hagroup.neu.edu/aboutha.htm
25PHOTODEGRADATION OF HUMIC ACID
Yousef Otaibi UEA
26SUNLIGHT PHOTOLYSIS OF HULIS
Yousef Otaibi UEA
27BROWN COLOUR
Abs at ? 400 nm
Surface active material (pmol/m3)
28AEROSOL SURFACTANTS
- Physical effects
- reduce surface tension
- smaller drops
- numerous drops
- longer life-times
- increased albedo
- lower temperatures
- Chemical effects
- solubilzation
- micellization
- lung interactions
Brimblecombe and Latif Env. Chem. 1, 11-12 2004
Facchini et al, Nature 401, 257-259 1999
29FORESTS
- Forests as a source not only in rural areas,
but also on cities such as at Atlanta - Choice or urban trees
30BIOGENIC EMISSIONS AND AIR QUALITY NORTHERN ITALY
- Isoprene and oxidation products
- Source of VOC for photochemical smog Duane et al
Averaged mixing ratios
Averaged OH reactivity indices
31FOREST AEROSOLS
- BIOGENIC EMISSIONS reactive chemistry that
generates ozone but also uses it
Cross in the Mountains Caspar David Friedrich
32da VINCI CODE
Virgin of the Rocks
33FOREST FIRES
- Historical and anthropological
- Ecological
- Health
- Atmospheric
E.A. Johnson and Kiyoko Miyanishi Forest Fires -
Behaviour and Ecological Effects
34FIRES OF 1877-1878
Coast lined with thick fog
Padang thick fog
Palembang enveloped in smoke
Fires also in Ambon and Timor
VERY STRONG ENSO
Potter, 2001
35FIRES OF 1902 and 1910
ONLY MODERATE ENSO
- 1902Severe drought and widespread haze, but
thought as volcanic, duststorms... - 1910 An expansion of rubber plantations in
Malaya
sky with a black pall of smoke.
Potter, 2001
36FIRES OF 1914
Fires destroyed 200 km2
Two months of fog on Lake Toba
Ships complain smoke caused poor visibility
MODERATE-STRONG ENSO
Potter, 2001
37ECOLOGICAL IMPACTS of HAZE
- Acid rain type issues - soil nutrients
- Ozone phytotoxicity
- Lower sunlight so haze decreases leaf carbon gain
Tang YH et al Forest Ecology and
Management 89205-211 (1996)
38AIR TRAFFIC
- Developing the early air routes required an
interest in smoke and visibility. - 1972 event - severe disruption of air traffic
e.g. at Palembang. - 1997 Garuda Airbus crash
39FOREST FIRE CHEMISTRY
- Rain may not be acidic
- Ammonia and organic acids important
HCl, HCOOH K2CO3, NH3
HNO3
H2SO4
Balasubramanian et al JGR 104,26881
40CLIMATE CHANGE and GLOBAL DIMMING
- Particles in the atmosphere can both increase and
decrease global temperature. - Direct effects e.g. carbon
- Indirect effects - e.g. clouds