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

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702 CHAPTER 13<br />

and 230 Rn (thoron), which seep out of the ground from the ubiqui<strong>to</strong>us uranium and<br />

thorium series (the average concentration of uranium and thorium in the <strong>to</strong>p 0.3 m<br />

of soil is 1 <strong>to</strong>n and 3 <strong>to</strong>ns, respectively, per square mile) and from their transformation<br />

products. These transformation products attach themselves <strong>to</strong> airborne particles with<br />

which they come in contact, thus contaminating the dust particles with radioactivity.<br />

The limiting activity in the radon daughter chain is 214 Pb (RaB), a beta emitter whose<br />

half-life is 26.8 minutes. In the thoron daughter chain, the limiting activity is 212 Pb<br />

(ThB), a beta-emitting iso<strong>to</strong>pe with a half-life of 10.6 hours.<br />

For routine moni<strong>to</strong>ring of long-lived contaminants, allowance is made for these<br />

activities by (1) counting the air sample several hours after collection, thereby allowing<br />

the 26.8-minute activity <strong>to</strong> decay away, and (2) counting the air sample about<br />

two ThB half-lives later. From these two measurements, the activity of the long-lived<br />

contaminant can be calculated. The counting rate C1 of the first measurement is<br />

due <strong>to</strong> the natural activity and the long-lived contaminant CLL:<br />

C1 = Cn1 + CLL; (13.33)<br />

when the second count is made, the natural activity has decayed <strong>to</strong><br />

Cn2 = Cn1 e −λt , (13.34)<br />

where λ, the decay constant of ThB, is 0.0655 h −1 , and t is the time interval in hours<br />

between the two counts. The second measurement, C2, includes the following:<br />

C2 = Cn2 + CLL, (13.35)<br />

C2 = Cn1 e −λt + CLL. (13.36)<br />

Solving Eqs. (13.35) and (13.36) simultaneously for the long-lived activity gives<br />

CLL = C2 − C1e −λt<br />

1 − e −λt<br />

. (13.37)<br />

W EXAMPLE 13.10<br />

In moni<strong>to</strong>ring for airborne 90 Sr, a 10-m 3 air sample is taken with a membrane filter.<br />

The first measurement, taken 4 hours after sampling, gives a net counting rate of<br />

100 cpm. The second count, 20 hours later, gives a net counting rate of 50 cpm. If<br />

the filter (after treatment <strong>to</strong> prevent electrostatic charge accumulation) was counted<br />

in a windowless 2π gas-flow counter, what was the mean concentration of 90 Sr in<br />

the air?<br />

Solution<br />

Substituting the respective values for C1 and C2 in<strong>to</strong> Eq. (13.37) gives<br />

CLL = 50 − 100e −0.065 h−1 ×20 h<br />

1 − e −0.065 h−1 ×20 h<br />

= 31.5 cpm

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