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Regional Basic Professional Training Course in Korea

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❙ 13 ❙<br />

1. Nuclear Reactor Pr<strong>in</strong>ciples<br />

The half-life (T½) of a radioactive element is the time required for one-half of the nuclei<br />

<strong>in</strong> a sample to decay. It can be obta<strong>in</strong>ed by plac<strong>in</strong>g N = No/2 <strong>in</strong> the above equation:<br />

No/2 = No e -λT½<br />

[7]<br />

Divid<strong>in</strong>g by No and tak<strong>in</strong>g the logs, we get:<br />

log e(½) = -λ T½ [8]<br />

and<br />

log e(½) = -log e (2) [9]<br />

thus<br />

T½ = loge(2)/ λ = 0.693 /λ [10]<br />

S<strong>in</strong>ce the dis<strong>in</strong>tegration rate or activityof the sample is proportional to the number of<br />

unstable nuclei, this also varies exponentially with time:<br />

A = Ao e -λt<br />

[11]<br />

This relationship is illustrated <strong>in</strong> Figure 1.3, which shows the variation <strong>in</strong> sample activity<br />

with time. In one half-life, the activity decays to one-half its <strong>in</strong>itial value, or ½Ao. In two<br />

half-lives it decays to ¼Ao, and so forth. This method can be applied to isotopes whose<br />

dis<strong>in</strong>tegration rates changes appreciably over a reasonable count<strong>in</strong>g period.

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