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Good Ozone and Bad Ozone

Good Ozone and Bad Ozone. MEES, March 5, 2008 Mort Sternheim, mort@umassk12.net Rob Snyder, snyder@umassk12.net STEM Education Institute Center for Hierarchical Manufacturing University of Massachusetts Amherst. MEES, March 5, 2008 Mort Sternheim, mort@umassk12.net

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Good Ozone and Bad Ozone

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  1. Good Ozone and Bad Ozone MEES, March 5, 2008 Mort Sternheim, mort@umassk12.net Rob Snyder, snyder@umassk12.net STEM Education Institute Center for Hierarchical Manufacturing University of Massachusetts Amherst MEES, March 5, 2008 Mort Sternheim, mort@umassk12.net Rob Snyder, snyder@umassk12.net STEM Education Institute Center for Hierarchical Manufacturing University of Massachusetts Amherst

  2. National Science Foundation grant to the UMass Center for Hierarchical Manufacturing, award # 0531171 NASA grant to the STEM Education Institute (ended), award # NNG05GN64G Our sponsors Advertisement: We are accepting teacher applications for International Polar Year and Nanotechnology Summer Institutes

  3. Today’s agenda • Ozone and ultraviolet (UV) light • Nanoparticles and sunscreen • Hands on sunscreen activity • Ozone is a health problem • Measuring ozone handouts Today’s materials on line: www.umassk12.net/nano/MEES

  4. The big ideas • Ultraviolet light causes skin damage and cancer • Ozone in the stratosphere blocks UV, partly • Sunscreen blocks UV, partly • Nanoparticles in sunscreen improve blocking • Tropospheric ozone is a major part of smog, damages plants, animals, and people

  5. 1. Ozone and UV • Ordinary oxygen gas: O2 (2 oxygen atoms) • Ozone: O3 (3 oxygen atoms) • Polar molecule, like water • Ozone is much more reactive, unstable • Pale blue, poisonous gas Bad! • Absorbs ultraviolet radiation! Good!

  6. The Sun’s radiation spectrum • ~ 43% is in the visible range • ~ 49% is in the near infrared range • ~ 7% is in the ultraviolet range • < 1% is x-rays, gamma rays, radio waves Most of the sun’s radiation is Ultraviolet (UV), Visible & Infrared (IR) : . Source: Adapted from http://www.ucar.edu/learn/imgcat.htm

  7. Some types of electromagnetic radiation • The sun emits several kinds of electromagnetic radiation: Visible (Vis), Infrared (IR) and Ultra Violet (UV). Note the split into UVA, UVB, UVC • Each kind is distinguished by a characteristic wavelength, frequency and energy • Higher energy radiation can damage our skin High Energy Low Energy Source: http://www.arpansa.gov.au/is_sunys.htm

  8. What is Radiation? • Light radiation is often thought of as a wave with a wavelength (l), speed (c), and frequency (f) related by • Since c (the speed of light) is constant, the wavelength and frequency are inversely related • This means that light with a short wavelength will have a high frequency and visa versa. Source: http://www.pueblo.gsa.gov/cic_text/health/sun_uv/sun-uv-you.htm

  9. E E  f f Radiation energy comes in packets or photons • The size of an energy packet or photon (E) is determined by the frequency of the radiation (f) • Radiation with a higher frequency has more energy in each packet • The amount of energy in a packet determines how it interacts with our skin

  10. Skin Damage • Very high energy radiation (UVC) is currently blocked by the ozone layer • High energy radiation (UVB) does the most immediate damage (sunburns) • But lower energy radiation (UVA) can penetrate deeper into the skin, leading to long term damage Source: N.A. Shaath. The Chemistry of Sunscreens. In: Lowe NJ, Shaath NA, Pathak MA, editors. Sunscreens, development, evaluation, and regulatory aspects. New York: Marcel Dekker; 1997. p. 263-283.

  11. Good ozone • In the stratosphere, absorbs 97+ % of solar UV, protecting life from harm • Produced by solar UV light from O2 : • O2+ UV (radiation < 240 nm) → 2 O • O + O2 → O3 • Ozone – oxygen cycle: • O3+ UV (< 320 nm) → O2 + O • This cycle heats the atmosphere slightly, so ozone is a greenhouse gas

  12. Ozone In the Atmosphere 100 60 Thermosphere 80 50 40 Mesosphere 60 Altitude (miles) 30 Altitude (km) 40 90% of ozone is in the stratosphere 20 20 10 10% of ozone is in the troposphere Troposphere 0 0 0 2 4 6 8 Ozone (parts per million) 12

  13. Ozone is the Earth’s natural sunscreen 100 60 Thermosphere 80 50 UVc - 100% Absorption Mesosphere UVb - 90% Absorption 40 UVa - 50% Absorption & Scattering 60 Altitude (miles) 30 Altitude (km) 40 20 20 10 Troposphere 0 0 0 2 4 6 8 Ozone (parts per million) 13

  14. Ozone layer • Ozone in stratosphere, 10 to 50 km above surface • Ozone Can be depleted by free radical catalysts – NO, OH, Cl, Br – from natural sources • Also from chlorofluorocarbons (CFCs) (freons) and bromofluorocarbons (halons) • UV light produces free Cl, Br radicals • Cl, Br catalyze chain reactions destroying ~100,000 ozone molecules • Used in aerosols, refrigerators, air conditioners, fire extinguishers

  15. Chemicals that Destroy Stratospheric Ozone • Cl is much more abundant than Br • Br is about 50 times more effective at O3 destruction From Ozone FAQ - see http://www.unep.org/ozone/faq.shtml From Ozone FAQ - see http://www.unep.org/ozone/faq.shtml

  16. Ozone depletion • Ozone levels decreasing ~4% per year since ’70’s • More skin cancer? • Larger seasonal decrease in lower altitudes (troposphere) in polar regions: the ozone hole • CFC’s phased out globally by 1996 (Montreal Protocol, 1987) – will take decades to leave atmosphere • Ozone levels have stabilized • Recovery will take decades

  17. Low level (tropospheric) ozone • Formed by interaction of UV with hydrocarbons, nitrogen oxides from natural sources plus car exhausts, etc. • Major air pollution (smog) component • Can cause serious damage to lungs • Fatal in very high concentrations for people, animals • Damage to plants • UNH Forest Watch looks at white pine needles which store data for 3 years • www.forestwatch.sr.unh.edu • Excellent school project • Measure with ozone sensitive paper, new meters

  18. Ozone levels • 3 – 10 ppb: Threshold of perception. Typical indoor level when outdoor levels are low • 50 ppb: Maximum allowed indoor levels • 100 ppb: Maximum allowed in industrial work area • 150 - 500 ppb: Typical outdoor peak urban levels • 300 ppb: Threshold for nasal, throat irritation • 500 ppb: Smog alert #1 in Los Angeles. Can cause nausea, headaches; lead to lung edema.

  19. Higher ozone levels • 1000 – 1500 ppb: Smog alerts #2, 3 in LA. Headaches, chest pains after 2 hours • 12,000 ppb: Lethal for guinea pigs after 3 hrs • 50,000 ppb: Lethal for humans after 60 minutes

  20. 2. Nanoparticles and sunscreen • 1 nanometer = 10-9 meter ~ 10 atomic diameters • Nanoparticles: 1 to 100 nm in diameter, or about 10 to 1000 atomic diameters • Sunscreen PowerPoint and activities based on NanoSense web site • http://nanosense.org/activities/clearsunscreen

  21. Nano Products • Number of products using nanomaterials is growing very rapidly • Doubling every year? • Clothing, food and beverages, sporting goods, coatings, cosmetics, personal care • Sunscreens: many use nanomaterials • Some labeled as containing nanoparticles • Some not labeled

  22. http://www.masspolicy.org/pdf/workshop/rejeski.pdf

  23. Why Use Sunscreen? Too much unprotected sun exposure leads to: • Premature skin aging (e.g. wrinkles) • Sunburns • Skin cancer Sources: http://www.oasishospital.org/previousnews.html; http://wohba.com/archive/2005_03_01_archive.html

  24. Skin Cancer Rates are Rising Fast Probability of getting skin cancer: 1930 : 1 in 5,000 2004 : 1 in 65 2050 : 1 in 10… Skin cancer: • Is ~50% of all cancer cases • Has > 1 million cases diagnosed each year • Causes 1 person to die every hour Causes of the increase: • Decrease ozone protection • Increased time in the sun • Increased use of tanning beds Sources: http://www.msnbc.msn.com/id/8379291/site/newsweek/ ; http://www.skincarephysicians.com/skincancernet/whatis.html; http://www.msu.edu/~aslocum/sun/skincancer.htm

  25. Sun Radiation Summary Increasing Energy Increasing Wavelength

  26. Which Sunscreen Should You Use??? New and Improved Now with Nano-Z Broadband Protection Safe for Children SPF 50 Goes on Clear

  27. A Brief History of Sunscreens: The Beginning • First developed for soldiers in WWII (1940s) to block “sunburn causing rays” These were called UVB rays WWII soldier in the sun Shorter wavelengths (more energy) called UVC Longer wavelengths (less energy) called UVA Sources: http://www.bbc.co.uk/wiltshire/content/articles/2005/05/05/peoples_war_feature.shtml http://www.arpansa.gov.au/is_sunys.htm

  28. A Brief History of Sunscreens: The SPF Rating • Sunscreens first developed to prevent sunburn • Ingredients were good UVB blockers • SPF (Sunscreen Protection Factor) Number • Measures the strength of UVB protection only • Higher SPF # = more protection from UVB • Doesn’t tell you anything about protection from UVA Sources: http://www.shop.beautysurg.com/ProductImages/skincare/14521.jpg and http://www.shop.beautysurg.com/ProductImages/skincare/14520.jpg

  29. A Brief History of Sunscreens: The UVA Problem • UVA rays have no immediate visible effects but cause serious long term damage • Cancer • Skin aging • Sunscreen makers working to find UVA blockers • No official rating of UVA protection yet Twenty different skin cancer lesions Source: http://www.cs.wright.edu/~agoshtas/fig8.jpg

  30. How do you know if your sunscreen is a good UVA blocker?

  31. Know Your Sunscreen:Look at the Ingredients • Lotion has “inactive ingredients” • Don’t block UV light • UV blocking agents are “active ingredients” • Usually have more than one kind present • UV blocking agents suspended in a lotion • “Colloidal suspension” • Two kinds of active ingredients • Organic ingredients and inorganic ingredients Source: Original Image

  32. Organic Ingredients: The Basics • Organic = Carbon Atoms • Hydrogen, oxygen & nitrogen atoms are also often involved • Structure • Covalent bonds • Exist as individual molecules • Size • Molecular formula determines size • Typical a few to several dozen Å (<10 nm) Octyl methoxycinnamate (C18H26O3) an organic sunscreen ingredient Sources: http://www.3dchem.com/molecules.asp?ID=135# and original image

  33. Organic Ingredients: UV Absorption • Electrons capture the energy from UV rays • They jump to higher energy levels • The energy is released as infrared rays which are harmless (each ray is low in energy) hf=2.48 eV 3hf=2.48 eV Source: Adapted from http://www.3dchem.com/molecules.asp?ID=135#and http://members.aol.com/WSRNet/tut/absorbu.htm

  34. Organic Ingredients: Absorption Range • Organic molecules only absorb UV rays whose energy matches difference between electron energy levels • Different kinds of molecules have different peaks and ranges of absorption • Using more than one kind of ingredient (molecule) gives broader protection One Ingredient Two Ingredients Three Ingredients Source: Graphs adapted from http://www.aims.gov.au/pages/research/projects/sunscreens/pages/sunscreens02.html

  35. Organic Ingredients: Absorption Range cont. • Most organic ingredients that are currently used were selected because they are good UVB absorbers • The FDA has approved 15 organic ingredients • Sunscreen makers are trying to develop organic ingredients that are good UVA blockers • Avobenzone (also known as Parasol 1789) is a new FDA approved UVA blocker Source: http://jchemed.chem.wisc.edu/JCEWWW/Features/MonthlyMolecules/2004/Oct/JCE2004p1491fig4.gif

  36. How are inorganic sunscreen ingredients different from organic ones? How might this affect the way they absorb UV light?

  37. Inorganic Ingredients: The Basics • Atoms Involved • Zinc or Titanium • Oxygen • Structure • Ionic attraction • Cluster of ions • Formula unit doesn’t dictate size • Size • Varies with # of ions in cluster • ~10 nm – 300 nm Detail of the ions in one cluster Group of TiO2 particles Source: http://www.microspheres-nanospheres.com/Images/Titania/TIO2%20P7.jpg and image adapted from http://www.cse.clrc.ac.uk/msi/projects/ropa.shtml

  38. Inorganic Ingredients: Cluster Size • Inorganic ingredients come in different cluster sizes (sometimes called “particles”) • Different number of ions can cluster together • Must be a multiple of the formula unit • ZnO always has equal numbers of Zn and O atoms • TiO2 always has twice as many O as Ti atoms ~100 nm TiO2 particle ~200 nm TiO2 particle Source: Images adapted from http://www.cse.clrc.ac.uk/msi/projects/ropa.shtml

  39. Inorganic Ingredients: UV Absorption • Inorganics have a different absorption mechanism than organics • Absorb consistently through whole UV range up to ~380nm Source: Graph adapted from http://www.aims.gov.au/pages/research/projects/sunscreens/pages/sunscreens02.html

  40. Why not use inorganics? • Appearance Matters • Traditional inorganic sunscreens have appear white on our skin • Many people don’t like how this looks, so they don’t use sunscreen with inorganic ingredients • Of the people who do use them, most apply too little to get full protection Source: http://www.4girls.gov/body/sunscreen.jpg

  41. Why Do They Appear White? • Traditional ZnO and TiO2 clusters are large • (> 200nm) • Large clusters scatter visible light • (400-700 nm) • Maximum scattering occurs for wavelengths twice as large as the clusters • The scattered light is reflected to our eyes, appearing white Source: Original image

  42. Organic Sunscreen Molecules are Too Small to Scatter Light ~200 nm TiO2 particle Methoxycinnamate (Inorganic) (Organic) (Note that these images are not drawn to scale) Source: Images adapted from http://www.cse.clrc.ac.uk/msi/projects/ropa.shtml and http://www.3dchem.com/molecules.asp?ID=135#

  43. Waves and obstacles • Waves go around small obstacles • Waves scatter all around from obstacles of sizes comparable to a wavelength • Water wave (ripple tank) simulation: http://www.falstad.com/ripple/

  44. What could we do to inorganic clusters to prevent them from scattering visible light? Source: Adapted from http://www.loc.gov/rr/scitech/mysteries/images/sunscreen2.jpg

  45. Nanosized Inorganic Clusters • Maximum scattering occurs for wavelengths twice as large as the clusters • Make the clusters smaller (100 nm or less) and they won’t scatter visible light Source: Graph adapted from http://www.aims.gov.au/pages/research/projects/sunscreens/pages/sunscreens02.html

  46. Nanosized ZnO particles Large ZnO particles Nano-Sunscreen Appears Clear Source: http://www.science.org.au/sats2003/images/barber-slide3.jpg

  47. In Summary… • Nanoparticle sunscreen ingredients are small inorganic clusters that: • Provide good UV protection by absorbing both UVB and UVA light • Appear clear on our skin because they are too small to scatter visible light Source: http://www.smalltimes.com/images/st_advancednanotech_inside_.jpg

  48. Essential Questions: Time for Answers • What are the most important factors to consider in choosing a sunscreen? • How do you know if a sunscreen has “nano” ingredients? • How do “nano” sunscreen ingredients differ from other ingredients currently used in sunscreens?

  49. Testing sunscreen activity • Use UV sensitive beads • Compare opacity/transparency of samples for visible light and UV light

  50. How can we measure ground level ozone? • Ozone paper • Moderate cost • Adequate for relative measurements • Used for NASA Globe project • But: • Inconsistent sensitivity one batch to the next • Insensitive to low ozone levels

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