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Introduction to Health Physics: Fourth Edition - Ruang Baca FMIPA UB

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490 CHAPTER 9<br />

plus and minus one standard deviation of the mean, 96% between plus and minus<br />

two standard deviations, and so on. The normal distribution, given by Eq. (9.33),<br />

contains the standard deviation, σ , as one of the parameters. The Poisson distribution<br />

(Eq. [9.36]), contains only one parameter, the mean. The standard deviation of the<br />

Poisson distribution is equal <strong>to</strong> the square root of the mean number of observations<br />

made during a given measurement interval:<br />

σ (Poisson) = √ n. (9.38)<br />

The “size” of the sample when we are counting events such as radioactive decay or<br />

other nuclear events is the arbitrary length of time over which we are making the<br />

measurement. In Eq. (9.38), n is equal <strong>to</strong> the <strong>to</strong>tal number of events that occurred<br />

during that time of observation and is thus the average rate for that time interval.<br />

Thus, if we observe 10,000 counts during a 10-minute counting interval, the standard<br />

deviation of the observation is √ 10, 000 = 100 counts per 10 minutes. The<br />

measurement represents a mean value of 10,000 counts for the 10-minute measurement<br />

interval. One of the main virtues of the Poisson distribution is that, for practical<br />

purposes, when n ≥ 20, it is indistinguishable from a normal distribution of the same<br />

mean and of standard deviation equal <strong>to</strong> the square root of the mean. Under these<br />

conditions, all statistical tests that are based on a normal distribution, such as the<br />

t-test, the chi-square criterion, and the variance ratio test (which is called the F-test)<br />

may also be used for Poisson distributions. Although all these tests are applicable<br />

<strong>to</strong> radioactivity measurements, a full discussion of them is beyond the scope of this<br />

book. Details and applications of these tests may be found in the Suggested Readings<br />

at the end of this chapter.<br />

In the example cited above, where 10,000 counts were recorded during 10 minutes<br />

of counting, the mean counting rate, in counts per minute, and the standard<br />

deviation of the mean rate is given by<br />

r ± σr = n<br />

t ±<br />

√<br />

n<br />

. (9.39)<br />

t<br />

Since<br />

σr =<br />

we have<br />

√<br />

n<br />

t =<br />

<br />

n 1<br />

×<br />

t t =<br />

<br />

r × 1<br />

t ,<br />

r ± σr = r ±<br />

<br />

r<br />

, (9.40)<br />

t<br />

which gives 1000 ± 10 cpm. If the activity had been measured over a 1-minute interval<br />

and had given 1000 counts, we would have 1000 ± √ 1000 or 1000 ± 32 cpm.<br />

Precision is a gauge of the reproducibility of a measurement. Thus, we are more<br />

likely <strong>to</strong> observe 1000 cpm during a 10-minute counting time than during a 1-minute<br />

counting period. Numerically, precision is given by the coefficient of variation, CV,<br />

which is defined as the ratio of the standard deviation <strong>to</strong> the mean:<br />

CV = σ<br />

, (9.41a)<br />

mean

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