jessica weber spring 2008 updated from dan gloudemans, spring 2005

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Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

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Page 1: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

Jessica WeberSpring 2008

Updated from Dan Gloudemans, Spring 2005

Page 2: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

VOC’s Ozone

Formation, natural/other VOC’s

Destruction, natural/other CFC’s

Measurement / EPA AQI Ozone hole Phenomenon What is being done about Ozone?

OTC CARB

Recent News Fun Facts Questions

Page 3: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

Organic Compound – contains carbon and hydrogen Ie: octane, butane…, sugar

VOC = Volatile Organic Compound, organics that evaporate easily

VOC’s are compounds that lead to the formation of ground level Ozone – “smog”

VOC’s can be found in anything from paints to deodorant

Page 4: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

Ozone is beneficial in Stratosphere blocks many ultra violet rays (λ < 320 nm) 90% of ozone is found here

Ozone is harmful in Troposphere it is a highly reactive gas that can affect the normal

functioning of the lungs Thickness of the ozone varies seasonally and

geographically Greatest concentrations are between 15 and 40 km,

ranging from 2-8 ppm Found during the spring in mid-to-high latitudes

Lowest concentration is found during Sept –Oct over Antarctica (ozone hole phenomenon)

Page 5: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005
Page 6: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

Ozone first formed - ~500 million years ago Ozone formation – atomic Oxygen

O3 is unstable, creates ozone-oxygen cycle

Most natural ozone formation occurs in the Tropics

“Chapman reactions” So called after S. Chapman who is famous for his paper 'A theory of upper-atmosphere ozone, Mem. Roy. Meteorol. Soc.' in 1930 which set out the first theoretical explanation of the ozone layer in the stratosphere.

Page 7: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

Photochemical reaction of NOx (Nitrogen oxides: collectively NO and NO2) with peroxy radicals in the presence of sunlight

HO2 + NO → OH + NO2 NO2 + hν → NO + O O + O2 → O3

Results in commonly known “Summertime Air Pollutant”

Sources of Nox Motor vehicles, Industrial Commercial Residential Fuel

Combustion, Utilities Sources of VOC

Industrial Commercial Processes, Motor Vehicles, Consumer Solvents

Page 8: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

VOC production (2004)

Page 9: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

Ozone destruction by UV radiation Ozone dissociates by absorbing a UV proton with λ<240

nm, photolysis

O + O3 → 2 O2 Large volcanic eruptions can affect ozone levels

Increases stratospheric chlorine concentrations by producing aerosols

Page 10: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

Free radical catalysts (NO, OH, Cl, Br) Causing ozone levels in the northern hemisphere to

drop approximately 4% per decade. CFC (choloroflurocarbon) compoundsPhotodissociation of CFCs

Contain chlorine and bromine radicals CFCl3 + hν → CFCl2 + Cl

Once separate from parent compound can react with ozone

Cl + O3 → ClO + O2

ClO + O → Cl + O2

A single Cl atom can continuously destroy ozone for 2 years

Page 11: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

Destruction allows more UV radiation through at harmful wavelengths causing increased genetic damage to living creatures and organisms.

Fortunately, where DNA is easily damaged, such as by wavelengths shorter than 290 nm, ozone strongly absorbs UV.

At the longer wavelengths where ozone absorbs weakly, DNA damage is less likely. If there were a 10% decrease in ozone, the amount of

DNA damaging UV radiaton increases by about 22%. DNA damage can most commonly lead to skin cancer

Increased UV radiation is expected to affect crop yields UV rays kill cyanobacteria on roots of rice plants

Page 12: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

Reported in Dobson Units (DU) G.M.B. Dobson

developed a spectrophotometer that was used to measure stratospheric ozone

Measure concentration of ozone in a column

1 DU = 0.01 mm of Ozone

300 DU a typical value Thus, 300 DU = 3 mm

O3 spread evenly across earth

Page 13: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

Measures presence of 5 pollutants

ground-level ozone

particle pollution carbon monoxide sulfur dioxide nitrogen dioxide

0-500 Scale 100 is National Air

quality standard ~200 – unhealthy -

whole population could be affected

>300 - Hazardous

Page 14: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

Over Antarctica First discovered/measured in 1985 by

the British Antarctic Survey TOMS (Total Ozone Mapping

Spectrometer) During the winter season, a vortex of

winds develops around the pole and isolates the polar stratosphere

As temperatures drop below -78°C (-109°F), thin clouds form of ice, nitric acid, and sulphuric acid

Chemical reactions on the surfaces of ice crystals in the clouds release active forms of CFCs

Page 16: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

2006 2007

Page 17: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

US adopted Montreal Protocol in 1987 – limit CFCs States most dangerous CFCs phased out by

2000 With compliance of the Montreal Protocol;

the ozone layer is expected to begin to recover in coming decades due to declining ozone-depleting substance concentrations (2005 article) In 2006, the ozone layer saw the worst level of

depletion in recorded ozone history.

Page 18: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

Clean Air Act (1963) All class I substances outlawed by Jan 1 2000

chlorofluorocarbon-11 (CFC–11) chlorofluorocarbon-12 (CFC–12) + others

All class II substances outlawed by Jan 1 2030 hydrochlorofluorocarbon-21 + various other

In 2007, President Bush added the 20-in-10 Bill Proposed to reduced gasoline consumption by 20% in

the next 10 years. Ozone “Action Days”

Days > 90°F, little or no wind Encourage to reduce emissions

World Ozone day – September 16th

Started in 1994 by the United Nations General Assembly

Page 19: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

OTC = Ozone Transport Commission Several northeastern states (13 total) Created under Clean Air Act (CAA)

amendments in 1990 Focus on Ground Level Ozone - specifically

NOx emissions - during May – Sept ~“Ozone Season” Northeast and Mid-Atlantic regions of US

NOx Budget Program – sell or store unused allowances Regional emissions trading program

Page 20: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

OTC recommended to EPA to set a standard for the primary ozone level to .060-.070ppm. As well as forming a secondary standard for

protection of crops during the growing season March 13, 2008 – EPA set standard to .075ppm (a

less protective threshold) and did not include a secondary standard Previous standard was .09 ppm exposure measured

over one hour (2005) OTC claims that if the standard had been set

lower benefits to the people in this region would include: Decreased respiratory problems, greater work

productivity, and reduced ER visits due to asthma incidences

Page 21: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

California Air Resource Board (CARB) In addition to NOx, regulate VOC emissions

Overseas all air pollution control efforts in California Money from violations goes to the California Air

Pollution Control Fund Provides support for various pollution-related research

project and programs Recent News

Sited three companies for failure to comply with the Periodic Smoke Inspection program Program that regulates the smoke emissions from

fleet vehicles Fines totaled over $57,000, companies also agreed

to attend classes conducted by the California Council on Diesel Education and Technology

Page 22: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

Fox River Valley Most smog in Wisconsin

Madison rates 47 AQI Milwaukee rates 48 AQI Wisconsin During Action Days

Combining errands Fueling car gas tanks at night

Emissions are less likely to produce ground level ozone

Mowing lawns after 6:00 p.m Properly inflating vehicle tires Carpooling, biking, walking or riding the bus to work

Page 23: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

NASA completed a study (Aug. 2005) that when a hurricane increasing in strength, the ozone level drops These results can be used to forecast hurricanes which

could possibly strike areas of high population If the ozone layer were brought down to the

Earth's surface, air pressure and temperature conditions would compress the ozone into a layer only 2 to 5 mm thick

SmogCity.com Decide weather conditions (temp, wind speed, cloud

cover), population level, and emissions levels Shows ozone levels throughout “created” day, and

gives health warnings if levels are very high

Page 24: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

“Sick Building Syndrome” VOC exposure indoors

Sources: photocopiers, carpets, and furnishings Most common is formaldehyde

Also tobacco smoke can contribute to high levels of VOCs

EPA has found that in some cases the VOC concentration can be 2-5 times higher indoors than outdoors

Page 25: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

The CO2 emissions that produce near-surface global warming in return cool the stratosphere which is expected to produce an increase in O3 depletion

The chemicals which deplete the ozone are also greenhouse gases Contributing to both ozone depletion and

global warming

Page 26: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

How does a city comply with new Ozone Standards? Largest producer targeted How long does it take to implement a new

standard? Can we lab-produce ozone and “insert” into

atmosphere? Can be lab-produced by electrolysis or with a D-cell

battery General reaction: 3 O2 — electricity → 2 O3

Page 27: Jessica Weber Spring 2008 Updated from Dan Gloudemans, Spring 2005

• EPA – “air Now”• How VOCs Contribute To Formation Of Ground-Level Ozone. Chemical &

Engineering News, 1/24/2005, Vol. 83 Issue 4, p26, 1/3p; (AN 16120478)• Chemical & Engineering News; 1/24/2005, Vol. 83 Issue 4, p25, 3p, 1c

“SMOG, POLICY AND CHEMISTRY.”• http://www.dnr.state.wi.us/org/aw/air/ozone/OzActionNotice.htm• http://www.epa.gov/Ozone/science/sc_fact.html “Ozone Science: The

facts Behind the Phaseout”• http://www.nasa.gov/vision/earth/environment/ozone_drop.html “Ozone

levels drop when hurricanes are strengthening”• http://www.ozonelayer.noaa.gov/data/antarctic.htm • “EPA’s New Ozone Standard Falls Short in Protecting the Public

Health, Says Ozone Transport Commission. Ozone Transport Commission.” March 13, 2008

• “California Adopts New Ozone Standard.” California Environmental Protection Agency. April 28, 2005.

• http://dnr.wi.gov/air/ • www.smogcity.com• http://www.ec.gc.ca/ozone/docs/UO/Primer/EN/index.cfm?p=13