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Impact Hazards

Impact Hazards. Can we predict impacts?. Incomplete inventory of objects May be a million km-sized objects Initial observations don't permit completely accurate predictions Comets vent gases and change orbits The meaning of probability of impact Planets don’t “wander”

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Impact Hazards

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  1. Impact Hazards

  2. Can we predict impacts? • Incomplete inventory of objects • May be a million km-sized objects • Initial observations don't permit completely accurate predictions • Comets vent gases and change orbits • The meaning of probability of impact • Planets don’t “wander” • Observational uncertainty

  3. Example, Measuring A Lot • You measure the lot 5 times, getting 99.7, 99.9, 100.1, 100.0 and 100.3 feet. • Average = 100 • Best estimate but might not be true value • Any random measurement has even odds of being too high or low • P All 5 too high or low = (1/2)5 = 1/32 • P 4 too high or low = 5/32 • P 3 too high or low = (5*4/2)/32 = 10/32

  4. Impact Probability

  5. Impact Probability

  6. The Torino Scale of Impact Hazard • Named for the city in Italy, not a person • Assesses both probability of event and potential effects of impact, so measures two different things • Not completely consistent.

  7. The Torino Scale of Impact Hazard • Low or no hazard • 0 - No danger, or object too small to penetrate atmosphere • 1 - Normal. No likelihood of impact • Merits attention by astronomers • 2 - Close pass but no cause for concern • 3 - 1% chance of impact causing local damage • 4 - 1% chance of impact causing regional damage • Threatening • 5 - Close pass by object capable of causing regional damage • 6 - Close pass by object capable of causing global effects • 7 - Very close pass by object capable of causing global effects • Certain Impact • 8 - Impact capable of causing local damage or tsunami • 9 - Impact capable of causing regional damage or tsunami • 10 - Impact with global effects

  8. Torino Scale

  9. MeteoritePeekskill, NY 1992

  10. Chondrite

  11. Stony-Iron Meteorite

  12. Iron Meteorite

  13. Meteo-Wrongs • Meteorites Never: • Have internal cavities • Have layers • Have veins • Flatten on impact • Mold around objects • Almost never light in color outside • If you “think” it’s magnetic, it’s not magnetic

  14. Nope

  15. Nope

  16. Uh-uh

  17. No Way

  18. Nope

  19. Nope

  20. Nope

  21. Tektites • Very silica-rich, water poor glassy rocks • Terrestrial vs. Extraterrestrial origin? • Volcanic vs. Impact origin? • Problems: • Odd chemistry • If terrestrial, why are they spread so widely? • If extraterrestrial, why are they so localized? • Now considered impact glass • Atmospheric shock wave evacuates atmosphere

  22. Tektites

  23. Spectrum of Impact Scenarios • Atmospheric impact and air burst (Tunguska, 1908) • Surface impact causing local damage • Surface impact with 100 km damage radius • Surface impact with 1000 km damage radius • Surface impact with global effects

  24. Tunguska, 1908

  25. Tunguska, 1908

  26. Sikhote-Alin Fall, February 12, 1947Mass = 100,000 Kg

  27. Sikhote-Alin Crater

  28. Sikhote-Alin Crater

  29. Sikhote-Alin Crater

  30. Near Miss, August 10, 1972

  31. 1972 Near Miss • Object was about the size of a bus • Entered Atmosphere over Utah, travelling north, exited over Canada • Velocity 15 km/sec • Missed by 58 km

  32. Returning to Space

  33. Carangas, Peru, 2007

  34. Carangas, Peru, 2007

  35. What happens during impact • Atmospheric entry • Microscopic objects gradually decelerate • Millimeter-sized objects vaporize, seen as meteors • Meter-sized objects may fragment and survive passage • House-sized objects hit with force • Contact-compression phase • Transient crater phase • Rebound and collapse phase

  36. Impact Processes • Impact releases kinetic energy instantaneously – Explosion • Explosion scaling: Volume proportional to energy • Radius scales as cube root of energy • Energy Measures • Kiloton = 4.2 x 1012 Joules = 1012 calories • Megaton = 4.2 x 1015 Joules = 1015 calories • Note: Small “c” calories

  37. Kinetic Energy • Assume 10 m rocky object • Volume = 1000 m3, Density = 3000 kg/m3 • Mass = 1000 m3 x 3000 kg/m3 = 3 x 106 kg • Velocity = 30 km/sec = 30,000 m/sec • K = ½ mv2 = ½(3 x 106 kg)(30,000)2 • K = 13.5 x 1014 Joules = 270 Kt = 13 Hiroshima nuclear weapons

  38. What is an Explosion? • Instantaneous point release of energy • Can be mechanical, chemical or nuclear • Damage is caused by the surrounding material: air, water or solid • Explosions would cause little damage in space

  39. All Large Explosions Make Mushroom Clouds

  40. Environmental Effects of Impacts • Radiant heat and flash burns • Blast wave • Seismic waves • Tsunami • Ejecta • Stratospheric dust • Liberated volatiles (carbon dioxide, sulfur, methane) • Impact volcanism - a myth

  41. Averting Impact Hazards • Simplest Strategy: Detection + Diversion • Destruction too unpredictable • Can object be destroyed? • “Cookie crumbs have no calories” • In real life, the pieces matter • The longer the lead time, the easier diversion becomes • Only need a close miss • Detection is cheap and off-the shelf

  42. Diversion “The question is: how to do it? These things must be done … delicately.” • Nukes? • Thrusters? • Space tug? • Gravitational? • Solar Sail • Laser?

  43. Asteroid Itokawa

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