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Nuclear Bombs

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Nuclear Bombs The First Nuclear Bombs There are two main types of bombs which release energy from the nuclei of atoms. The simplest kind is an atomic bomb. – PowerPoint PPT presentation

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Title: Nuclear Bombs


1
Nuclear Bombs
2
The First Nuclear Bombs
3
  • There are two main types of bombs which release
    energy from the nuclei of atoms. The simplest
    kind is an atomic bomb. Like a nuclear power
    plant, it releases great quantities of energy
    through a process called nuclear fission, or
    'splitting', of a large unstable (radioactive)
    element like uranium or plutonium.

4
  • The energy source is a mass of radioactive
    material such as uranium or plutonium. This
    material is very unstable every atom's nucleus
    is ready to fall apart ('decay') at the slightest
    nudge, releasing unneeded energy and extra
    neutrons. In the diagram, the plutonium (B) is
    given that nudge by the outer casing of TNT (A),
    which explodes all around it.

5
  • The plutonium is unstable, or radioactive. Its
    atoms are constantly 'falling apart', breaking up
    into smaller elements that are more stable. Every
    time one nucleus does this, it releases the extra
    energy it no longer needs to hold it together, as
    well as a few left-over neutrons. This energy,
    and the escaping neutrons, is what we describe as
    the radiation being emitted from the radioactive
    plutonium. This energy and flow of escaping
    neutrons can damage human cells, so radioactivity
    is dangerous.Enough atoms in the chunk of
    plutonium are breaking down at any one time to
    make the chunk of plutonium warm up, but not
    enough to be considered an explosion.

6
  • What happens in the bomb, however, changes that!
    The force of the TNT explosion causes the
    plutonium to be squashed, or compressed in size,
    and become very dense. This is called its
    'critical mass' the plutonium is now so densely
    packed together that the neutrons escaping from
    the decaying nuclei of plutonium cannot escape
    from the plutonium without bumping into another
    plutonium atom!

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8
  • When they hit another atom, they cause that
    nucleus to break down too, whether it was ready
    to or not. That second nucleus releases more
    energy, and more neutrons, which in turn go on to
    hit and break up further nuclei. The decaying
    nuclei cause more decaying nuclei, and so on, in
    a rapidly escalating chain reaction ... and all
    because the plutonium has been squeezed into such
    a dense state (by the TNT) that the escaping
    neutrons that normally would fly out of the
    material now can't, without hitting other nuclei!

9
  • Within a very tiny fraction of a second, all the
    nuclei in the chunk of plutonium have been hit by
    escaping neutrons, and have broken down. The
    extra energy in trillions of atomic nuclei is all
    released at once! This energy is considerable
    the atomic bomb dropped on Hiroshima in WWII was
    an example of this process.

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13
Initial Explosive Conditions
  • Maximum temperature at burst point several
    million degrees centigrade. A fireball of
    15-meters radius formed in 0.1 millisecond, with
    a temperature of 300,000 degrees centigrade, and
    expanded to its huge maximum size in one second.
    The top of the atomic cloud reached an altitude
    of 17,000 meters.

14
Black Rain
  • Radioactive debris was deposited by "black rain"
    that fell heavily for over an hour over a wide
    area.

15
Damaging Effects of the Atomic Bomb
  • Intense thermal heat emitted by the fireball
    caused severe burns and loss of eyesight. Thermal
    burns of bare skin occurred as far as 3.5
    kilometers from ground zero (directly below the
    burst point). Most people exposed to thermal rays
    within 1-kilometer radius of ground zero died.
    Tile and glass melted all combustible materials
    were consumed.

16
Blast
  • An atomic explosion causes an enormous shock wave
    followed instantaneously by a rapid expansion of
    air called the blast these represent roughly
    half the explosion's released energy. Maximum
    wind velocity 440 meters per second. Wooden
    houses within 2.3 kilometers of ground zero
    collapsed. Concrete buildings near ground zero
    (thus hit by the blast from above) had ceilings
    crushed and windows and doors blown off.

17


Bodily Injuries
  • Acute symptoms. Symptoms appearing in the first
    four months were called acute. Besides burns and
    wounds, they included general malaise, fatigue,
    headaches, loss of appetite, nausea, vomiting,
    diarrhea, fever, abnormally low white blood cell
    count, bloody discharge, anemia, loss of hair.
  • Aftereffects. Prolonged injuries were associated
    with aftereffects. The most serious in this
    category were keloids (massive scar tissue on
    burned areas), cataracts, leukemia and other
    cancers.

18
Radiation
  • People exposure within 500 meters of ground zero
    was fatal. People exposed at distances of 3 to 5
    kilometers later showed symptoms of aftereffects,
    including radiation-induced cancers.
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