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REPORT ABUSIVE REPLY
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Message Subject
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California schools to begin monitoring for Fukushima radiation 'arriving this year'
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psyoptics |
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Post Content
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There is no more radiation because the material fizzed out.
You do realize the million year half life only exists if the energy isn't being used, right?
You do realize the plant didn't have enough radioactive material to cause a global catastrophe right?
Not even a single atomic weapon has that much power.
It took 6 months, but the material is done transmogrifying.
Do you really think there is such thing as an immortal energy source on this planet?
Really?
Quoting: Anonymous Coward 52583283 Nice fairy tale. Denial is for stupid people Intelligent people: A.) Ask for proof B.) Provide contrary evidence I have done both. Google "Half Life Radiation". here are some by products ......
Plutonium is the heaviest primordial element by virtue of its most stable isotope, plutonium-244, whose half-life of about 80 million years is just long enough for the element to be found in trace quantities in nature.[3] Plutonium is mostly a byproduct of nuclear reactions in reactors where some of the neutrons released by the fission process convert uranium-238 nuclei into plutonium.[4]
Both plutonium-239 and plutonium-241 are fissile, meaning that they can sustain a nuclear chain reaction, leading to applications in nuclear weapons and nuclear reactors. Plutonium-240 exhibits a high rate of spontaneous fission, raising the neutron flux of any sample containing it. The presence of plutonium-240 limits a plutonium sample's usability for weapons or its quality as reactor fuel, and the percentage of plutonium-240 determines its grade (weapons grade, fuel grade, or reactor grade).
Plutonium-238 has a half-life of 88 years and emits alpha particles. It is a heat source in radioisotope thermoelectric generators, which are used to power some spacecraft. Plutonium isotopes are expensive and inconvenient to separate, so particular isotopes are usually manufactured in specialized reactors.
Quoting: [link to en.wikipedia.org]
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