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216 bytes added ,  12:23, May 21, 2008
→‎Rate of decay: Instroduce this assumption; put decay function in here.
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=== Rate of decay ===
 
=== Rate of decay ===
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Another assumption is that the rate of decay is constant.
 
There is no reason to expect that the rate of decay of a radioactive material is largely constant, and it was almost certainly not constant near the creation or beginning of the universe.<ref>At least one example of a change in the rate has been observed in laboratory experiments.  See ''[http://www.creationontheweb.com/content/view/1608/ Radioactive decay rate depends on chemical environment]''.</ref>   
 
There is no reason to expect that the rate of decay of a radioactive material is largely constant, and it was almost certainly not constant near the creation or beginning of the universe.<ref>At least one example of a change in the rate has been observed in laboratory experiments.  See ''[http://www.creationontheweb.com/content/view/1608/ Radioactive decay rate depends on chemical environment]''.</ref>   
    
The process of decay is as follows.  Atoms consist of a heavy central core called the [[nucleus]] surrounded by clouds of lightweight particles (electrons), called [[electron shell]]s. The energy locked in the nucleus is enormous, but cannot be released easily. The phenomenon we know as heat is simply the jiggling around of atoms and their components, so in principle a high enough temperature could cause the components of the core to break out. However, the temperature required to do this is in in the millions of degrees, so this cannot be achieved by any natural process that we know about. The second way that a nucleus could be disrupted is by particles striking it. However, the nucleus has a strong positive charge and the electron shells have a strong negative charge. Any incoming negative charge would be deflected by the electron shell and any positive charge that penetrated the electron shells would be deflected by the positive charge of the nucleus itself.
 
The process of decay is as follows.  Atoms consist of a heavy central core called the [[nucleus]] surrounded by clouds of lightweight particles (electrons), called [[electron shell]]s. The energy locked in the nucleus is enormous, but cannot be released easily. The phenomenon we know as heat is simply the jiggling around of atoms and their components, so in principle a high enough temperature could cause the components of the core to break out. However, the temperature required to do this is in in the millions of degrees, so this cannot be achieved by any natural process that we know about. The second way that a nucleus could be disrupted is by particles striking it. However, the nucleus has a strong positive charge and the electron shells have a strong negative charge. Any incoming negative charge would be deflected by the electron shell and any positive charge that penetrated the electron shells would be deflected by the positive charge of the nucleus itself.
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Calculations involve the well-established function for exponential decay: <math>F</math><sub><math>t</math></sub><math>=e</math><sup><math>-kt</math></sup>.
    
=== Outside influences ===
 
=== Outside influences ===
nsTeam2RO, nsTeam2RW, nsTeam2_talkRO, nsTeam2_talkRW
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