This document discusses various topics in physics including nuclear reactions, radioactive decay, stellar nucleosynthesis, nuclear fission and fusion, atomic structure, nuclear power and energy, plate tectonics, earthquakes, tsunamis, and wave mechanics. It provides explanations of physical phenomena like alpha, beta, and gamma radiation, conservation of nucleons, and conservation of energy. It also discusses choices and tradeoffs around different energy sources.
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Physics in the news: Earthquakes, Tsunamis and Nuclear Power
1. Physics in The News: Earthquakes, Tsunamis and Nuclear Power.
2. Work Conservation of Energy Stellar Nucleosynthesis Nuclear Reactions What Radiation is Nuclear Reactors How the Earth Works Wave Mechanics Choices for the Future
3. I like work. It fascinates me. I can sit and look at it for hours. Jerome K. Jerome, English Playwright
19. 2 4 H He 1 2 E + + + 1 3 n H 0 1 In nuclear fusion, two nuclei with low mass numbers combine to produce a single nucleus with a higher mass number. This happens in stars.
20. Protons are positively charged little particles...they repel each other The neutron helps balance out the positive repulsion via the strong nuclear force. Too many or too few neutrons creates instability. Wait. What’s an isotope? What the hell is a Proton? And what is a Neutron For? How do we know all this?
21. Band of Stability and Radioactive Decay: some atoms are more stable than others….just like people.
22. All science is either physics or stamp collecting. Ernest Rutherford, English Physicist. Nobel Prize in not-Stamp Collecting, 1908.
23. Antoine Henri Becquerel (1852-1908) On the rays emitted by phosphorescence [read before the French Academy of Science 24 Feb. 1896 (ComptesRendus 122, 420 (1896)) translated by Carmen Giunta] In an earlier session, M. Chairman Henry announced that phosphorescent zinc sulfide placed in the path of rays emanating from a Crookes tube augmented the intensity of rays passing through the aluminum. Elsewhere, M. Niewenglowski recognized that commercial phosphorescent calcium sulfide emits rays which pass through opaque bodies. This fact extends to various phosphorescent bodies, and in particular to uranium salts whose phosphorescence has a very brief duration. With the double sulfate of uranium and potassium, of which I have a few crystals forming a thin transparent crust, I was able to perform the following experiment: One wraps a Lumière photographic plate with a bromide emulsion in two sheets of very thick black paper, such that the plate does not become clouded upon being exposed to the sun for a day. One places on the sheet of paper, on the outside, a slab of the phosphorescent substance, and one exposes the whole to the sun for several hours. When one then develops the photographic plate, one recognizes that the silhouette of the phosphorescent substance appears in black on the negative. If one places between the phosphorescent substance and the paper a piece of money or a metal screen pierced with a cut-out design, one sees the image of these objects appear on the negative. One can repeat the same experiments placing a thin pane of glass between the phosphorescent substance and the paper, which excludes the possibility of chemical action due to vapors which might emanate from the substance when heated by the sun's rays. One must conclude from these experiments that the phosphorescent substance in question emits rays which pass through the opaque paper and reduces silver salts.
29. 4Be 1H 2He 6C 2He 1H 1H 6C 2He 4Be 8O 2He 2He Stellar NucleoSynthesis: Making everything up to iron!
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31. During a supernova, neutrons bombard heavy ions, building heavy atoms though beta decay. Forged in intense conditions, these atoms are unstable.
32. 14 N 7 Energy + + + 1 4 p He 1 2 Balancing Nuclear Reactions Atomic numbers must balance Mass numbers must balance Use a particle or isotope to fill in the missing protons and neutron Rutherford in 1919 transmutes nitrogen into...
33. 14 17 N O 7 8 Energy + + + 1 4 p He 1 2 Rutherford in 1919 transmutes nitrogen into oxygen.
34. 226 88 4 He 2 Nuclear Reactions: Radium Alpha emission Ra
35. 226 222 Ra Rn 88 86 + 4 He 2 (aka α) Nuclear Reactions: Alpha emission Mass number (A) goes down by 4. atomic number (Z) goes down by 2. Nucleons (nuclear particles… protons and neutrons) are rearranged but conserved
36. 239 239 U Np 92 93 + 0 β -1 Nuclear Reactions: Beta emission Mass number (A) is unchanged. atomic number (Z) goes down up. Here, a neutron breaks down into a proton and an electron.
37. 10 1 n 5 0 + + 4 He 2 (aka α) What happens when we: B Remember: Nucleons (nuclear particles…protons and neutrons) are rearranged but conserved
38. 10 1 B n 5 0 + + 4 13 He N 2 7 (aka α) What happens when we: Nitrogen usually has 7 protons and 7 neutrons…so this has one too few. Nitrogen-13 is a radioisotope of nitrogen used in positron emission tomography (PET). It has a half life of a little under ten minutes, so it must be made at the PET site. A cyclotron may be used for this purpose.
40. 60 60 Co Ni 27 28 + 0 β -1 What happens when: Cobalt 60 has such a short half life you can’t find it in nature. Usually it is created by bombarding a Co-59 atom with a neutron. When it decays, the Nickel atoms are energized and release gamma rays. They used to be employed in radiation therapy for cancer.
41. 60 59 60 60 Co Co Co Ni 27 27 27 28 + 0 β -1 1 + n 0 Cobalt 60 has such a short half life you can’t find it in nature. Usually it is created by bombarding a Co-59 atom with a neutron. When it decays, the Nickel atoms are energized and release gamma rays. They used to be employed in radiation therapy for cancer.
42. 4Be 1H 2He 6C 2He 1H 1H 6C 2He 4Be 8O 2He 2He Stellar NucleoSynthesis: Making everything up to iron!
43. Fission Chain reaction, given enough neutrons. While induced here, it happens naturally, just more slowly.
44. The radioactive decay process can be thought of as a reversal of their formation in the heat of a supernova. As they decay, they release that energy back, due to conservation of Energy
45. The problem with Half life in radioactive elements: it’s a long time. Where to put it when you don’t want it anymore?
46. What’s Uranium Good for? Until 1960, ceramic glazes. Now, since it is so dense (68.4% denser than lead), it ironically make a great radiation shield. And a dense, piercing projectile.
49. So how do we harness this power to make energy?
50. So how do we harness this power to make energy?
51. Three layers of protection: Uranium in a ceramic matrix, in a Zirconum tube, in a Vessel and a Containment building. All the bad stuff stays locked up
53. When containment fails, what happens? Radiation doesn’t get far. But Radioactive particles do.
54. Cesium-137 looks like Potassium to our bodies, and so is harmful when ingested. When a neutron transforms to a proton and a beta particle, the additional proton changes the atom to barium-137. The nucleus ejects the beta particle. However, the nucleus still has too much energy and ejects a gamma photon (gamma radiation) to become more stable.
55. Radioactive Iodine in absorbed by the thyroid, causing cancers. Iodine is an essential element that enables the thyroid gland to produce thyroid hormones: triiodothyronineand thyroxine-- the two key hormones produced by the thyroid gland the “master gland of metabolism”.
56. Usually these reactions only take place quickly when concentrated and purified. This is done via gas centrifuge.
57. Natural nuclear fission reactor, discovered in 1972 at Oklo in Gabon, by French physicist Francis Perrin. http://en.wikipedia.org/wiki/Natural_nuclear_fission_reactor
58. I feel the Earth move under my feet. Carole King
60. An old idea: Antonio Snider-Pellegrini's Illustration of the closed and opened Atlantic Ocean (1858)
61. Mid-Ocean Ridges: this was quack science in 1912 when Alfred Wegner re- proposed the idea. Only in the 1960s was it explained via sea-floor spreading.
64. http://www.washington.edu/burkemuseum/geo_history_wa/The%20Restless%20Earth%20v.2.0.htm The aesthenosphere is kept loose and flowing largely through heat generated by radioactive decay. The material that is decaying is primarily radioactive isotopes of light elements like aluminum and magnesium. This heat source is small on an absolute scale (the corresponding heat flow at the surface out of the Earth is only about 1/6000 of the Solar energy falling on the surface). “Nevertheless, because of the insulating properties of the Earth's rocks this is sufficient to keep the aesthenosphere plastic in consistency.” http://csep10.phys.utk.edu/astr161/lect/earth/tectonics.html
65. Another View: Hot Spots form from convection currents, lasering their way through the Earth’s crust.
66. So the planet is like this: http://www.youtube.com/watch?v=rNcXataE0YM
77. The physics of wave height and speed: In the deep ocean, the typical water depth is around 4000 m, so a tsunami will therefore travel at around 200 m/s, or more than 700 km/h. Oddly, Tsunamis slow down as they get to land. http://www.bom.gov.au/tsunami/info/index.shtml
78. Conservation of Energy! If we loose Kinetic Energy, we must gain Potential. The Wave increases in Height, an effect called shoaling. A tsunami with a height of 1 m in the open ocean where the water depth is 4000m would have a wave height of 4 to 5 m in water of depth 10 m.