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Nuclear Spectroscopy

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E X P E R I M E N T 11<br />

Potassium 40<br />

INTRODUCTION<br />

Potassium is an element essential for all life, including<br />

human. It is found especially in the muscle tissue. It is<br />

used in fertilizers, and its percent content by weight is<br />

given in the third number of the description of fertilizer.<br />

Fertilizer labeled 30-15-24 has 24% of its total<br />

weight as potassium.<br />

Potassium as an element is 93.3% mass 39, 6.7% mass<br />

41 (giving the atomic weight of 0.933 x 39 + 0.067 x 41<br />

= 39.1), and 0.0117% mass 40. Although 39 K and 41 K<br />

are stable to radioactive decay, 40 K is radioactive with a<br />

half-life of 1.28 x 10 9 years. Radioactivity from the 40 K<br />

in our own bodies accounts for about half of our yearly<br />

exposure to all sources of radiation! It is an important<br />

isotope to study, and it can be purchased at any health<br />

food store by anyone old enough to hold money.<br />

As illustrated in Figure 11.1, 40 K will decay by β −<br />

emission 89.3% of the time to the ground state of 40 Ca<br />

with no gamma emission. 40 K will decay 10.5% of the<br />

time by electron capture to an excited state of 40 Ar,<br />

resulting in a gamma of 1,460.8 keV being emitted. It<br />

is this gamma that you can detect as evidence for 40 K.<br />

A measure of the absolute activity of 40 K will provide a<br />

measure of the total potassium present. It can also<br />

provide a measure of the half-life of 40 K. The activity of<br />

a radioactive sample is the number of decays per<br />

second of that isotope. If it is not being replenished by<br />

some other radioactive process and N(t) represents<br />

the number of parent ( 40 K) atoms at time, t, then the<br />

activity, A(t), for an isotope with decay constant, λ total<br />

(λ= ln2/T 1/2<br />

= 0.693/T 1/2<br />

), and half-life, T 1/2<br />

, is<br />

11.2<br />

0+<br />

40<br />

18 Ar<br />

1461<br />

0<br />

EC,<br />

β<br />

11%<br />

+<br />

4<br />

~0.1%<br />

λtotal = λ + λ<br />

β<br />

+ −<br />

9<br />

1.28x10 y<br />

40<br />

19 K<br />

β<br />

Since N(t) is just 0.0117% of the number of potassium<br />

atoms present at the time of counting, the decay<br />

constant and half-life of potassium can be determined<br />

from a measurement of the present activity. The<br />

relative abundance of 40 K, 0.0117%, is known from<br />

mass-spectrometer measurements.<br />

40<br />

K is found in most soils, building materials, plants<br />

and animals. This will provide a photopeak background<br />

that must be corrected with a background<br />

subtraction. This can be as large as your source strength.<br />

It is important for this chapter’s experiments and<br />

those that follow to increase the shielding around and<br />

under your detector. Any pure metal, such as iron or<br />

lead of a few centimeters’ thickness will significantly<br />

reduce your detected background. Commercial environmental<br />

shields are also available.<br />

89%<br />

β<br />

–<br />

0+ 0<br />

40<br />

20 Ca<br />

Figure 11.1 Schematic energy level diagram of the<br />

radioactive decay of 40 K.<br />

where<br />

11.1<br />

At ()<br />

dN()<br />

t<br />

dt<br />

d<br />

dt N e −λ<br />

( 0)<br />

totalt<br />

= = ( ) =<br />

λ<br />

total<br />

λ t<br />

N( 0) e − total = λ N( t)<br />

total<br />

32

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