Upload
frederico-genezini
View
69
Download
5
Embed Size (px)
Citation preview
Radioactive decay and counting statistics
Jørgen Gomme
The decay equation Predictability and chance
Radioactivity measurements and statistics in practice
F07
2011 Isotope techniques, F07 (JG) 2
Outline
The decay equation Stochastic nature of radioactive decay Poisson-distribution Controlling the stability of counting instrumentation Accuracy and precision
2011 Isotope techniques, F07 (JG) 3
An amount of material containing N radioactive atoms has the acitivity A:
Number of decays (nuclear disintegrations) per unit time.
dNAdt
≡
The fundamental SI-unit for activity is the becquerel (Bq):1 Bq ≡ 1 disintegration per second
The old unit (still occasionally used) is the curie (Ci):1 Ci =3.7000×1010 Bq1 Bq =2.7027×10-11 Ci
N
Activity
2011 Isotope techniques, F07 (JG) 4
Counting efficiency and counting rate
∆N decays occur in the radioactive sample in a period of length ∆t
The detector (and the associated instrumentation) only records a fraction of these decays (ε = counting efficiency)
∆M impulses are recorded during the period ∆t The counting rate (pulse rate) is r = ∆M/∆t
M Nrt t
ε∆ ∆= =
∆ ∆
# decays# counts
counting efficiency
counting time
2011 Isotope techniques, F07 (JG) 5
Predictability and chance...
2011 Isotope techniques, F07 (JG) 6
Radioactive decay is a stochastic phenomenon
Impossible to predict when a radioactive atom decays, but the probability of decay in a given period of time is known
Radioactive decay follows a Poisson-distribution
Consequences for:
Uncertainty in radioactivity measurements
Check of instrument performance
λ
2011 Isotope techniques, F07 (JG) 7
0tA A e λ−=
The decay equation may be derived from the assump-tion, that each individual nucleus of a given radio-nuclide has a well-defined probability (λdt) for decay in the time interval dt
The decay equation provides an exact relation between the activity and the number of atoms (amount of the radio-active substance)…
… or between the activity at two different points in time:
The decay law
dNAdt
≡
2011 Isotope techniques, F07 (JG) 8
Number of decays / counts per unit time– according to the decay law
( )( )
0
0
1
1
t
t
N N e
M N e
λ
λε
− ∆
− ∆
∆ = −
∆ = −
From the decay equation we might expect the same number of decays in succesive periods of constant length, ∆t
Assuming constant counting efficiency ε, also the number of counts per period would be constant
None of these predictions are fulfilled in practice: The radioactive decay is a stochastic phenomenon
Number of decays:
Number of counts:
2011 Isotope techniques, F07 (JG) 9
Varying number of decays in succesive periods ∆t
The decay equation predicts a constant number of decays per unit time
However, the actual number of decays in succesive periods of the same length vary, i.e. radioactive decay is a stochastic phenomenon
MeanEmpiricalStandarddeviation
0
1
2
3
4
5
6
12-1
3
14-1
5
16-1
7
18-1
9
20-2
1
22-2
3
24-2
5
26-2
7
28-2
9
30-3
1
32-3
3
34-3
5
36-3
7
38-2
9
Mean
2011 Isotope techniques, F07 (JG) 10
Repeated measurements of sample counting rate: Variation around a mean value
In practice, two different sources of variation:– Stochastic nature of radioactive decay– Instrumental variability – instability in detector and
electronics The stochastic nature of radioactive decay may be related to
the decay constant λ (probability of decay in unit time) Instrumental variability may be seen as a phenomenon, that
is reflected in fluctuating counting efficiency, ε
Repeated measurements on the same sample
2011 Isotope techniques, F07 (JG) 11
Sources of variation
How to perform radioactivity measurements, so that the results are representative of the ”true activity” of the sample?
Differentiating between the variability due to:
Stochastic nature of radioactive decay
Instrumental instability
In practical work: Uncertainty and errors in sample preparation represents an additional source of variation – to be discussed later.
2011 Isotope techniques, F07 (JG) 12
Stochastic nature of radioactive decay
Probability theory: Repeated meaurements on the same sample will follow a distribution, that may be described analogously to the binomial distri-bution – a situation corresponding to ”throwing dice”
The binomial distribution gives an expression for the probability P(∆N) of observing ∆N decays during the period ∆t when the total number of radioactive atoms is N0
2011 Isotope techniques, F07 (JG) 13
Radioactive decay, compared to throwing dice
The probability of getting exactly 10 sixes when doing 50 throws with a single die is: 0.116 (11.6 %)
2011 Isotope techniques, F07 (JG) 14
It may be shown mathematically, that in the limiting case the binomial distribution approaches the Poisson-distribution (when the probability for any nucleus decaying in the observation period is small):
ν is the true value (expectation value for the number of decays in the period ∆t)
P(∆N) is the probability for ∆N decays in the period ∆t
Poisson-distribution– the ”law of rare events”
( )0 1 tN e λν − ∆= −
2011 Isotope techniques, F07 (JG) 15
Poisson error
For the Poisson distribution, the theoretical standard devia-tion (standard error, ”Poisson error”) is always equal to the square root of the true value (the expectation value).
2011 Isotope techniques, F07 (JG) 16
Predictability and chance
Two sides of the same coin:
The decay law – with its exact relation between the number of radioactive atoms, and the number of disintegrations per unit time
Stochastic nature of radioactive decay
λ
2011 Isotope techniques, F07 (JG) 17
Poisson-distribution for different ν
P(∆N)
∆N
ν = 25
ν = 5
ν = 1For ν > 20 the Poisson-distribution approaches a normal distribution
2011 Isotope techniques, F07 (JG) 18
Counting a radioactive sample
∆M counts are recorced in the time ∆t, giving the count rate r = ∆M/∆t
With the counting efficiency ε, this will correspond to the disintegration rate ∆N/∆t – to be taken as the best estimate of the true value ν
Estimate of standard error on r: sr
The standard error sr (”Poisson error”)is a measure of the variation in the results, that may be explained by the stochastic nature of radioactive decay.
2011 Isotope techniques, F07 (JG) 19
One or several counts on the same sample...?
2011 Isotope techniques, F07 (JG) 20
Repeated determinations – what to expect?
n separate measurements, each of duration ∆t, total counting time n∆t
A single measurement of duration n∆t
2011 Isotope techniques, F07 (JG) 21
One or several counting periods?
From a statistical point of view, we obtain the same information when counting a sample in the following two situations:
– Counting in a single period of length ∆t
– Counting in n periods, each of length ∆t/n
It is the the total counting time (or rather: the total number of counts collected, ∆M), that determines the ”information” obtained, or the ”uncertainty” associated with the measurement.
2011 Isotope techniques, F07 (JG) 22
Absolute and relative standard error
Mrt
∆=
∆
rMst
∆=
∆
( ) 1r rel
Mts M Mt
∆∆= =∆ ∆∆
Count rate:
Absolut standard error(Poisson error):
Relative standard error:
The relative error depends only on the number of counts accumulated
cps
cps
2011 Isotope techniques, F07 (JG) 23
Relative standard error as a function of the number of counts
Number of counts Relative error
100 10.00
200 7.07
500 4.47
1000 3.16
2000 2.24
5000 1.41
10000 1.00
20000 0.71
50000 0.45
100000 0.32
M∆ ( )rel 1/ 100%s M= ∆
2011 Isotope techniques, F07 (JG) 24
Nevertheless: Why sometimes doing repeat counts?
As seen above, this does not provide additional information about the radioactive sample, …
However: Repeated measurements on the same sample gives an
opportunity to evaluate the stability of the counting equipment, or:
It is possible to estimate the following sources of variation:– The stochastic nature of radioactive decay (cf. λ)– Instability of the instrumentation; may be seen as a
variation of ε
Occasionally, a counting period ∆t is divided into n subperiods, each of duration ∆t/n, and for the overall result the mean af nindividual countings is used:
2011 Isotope techniques, F07 (JG) 25
Practical examples, test of stability...
2011 Isotope techniques, F07 (JG) 26
Radioactive sample: 86Rb (T½ = 18.63 d)Counting time (∆t = 5 min), constant for all samples
Observations:
Mean: 31396 counts per 5 min
S.D.: 1591 (5.07 %)
Poisson error:
1: Example from Laboratory 2– counting a series of samples, prepared in the same say
Uncertainty/errors in sample prepa-ration
30040 29105 3084033505 32995 3151529915 31860 3367030515
M∆ =
M∆ =
From sample distribution
From sampling distribution
2
emp
( )
1n
M Ms
n
∆ −∆= =
−
∑
Pois 31396 177 (0.56%)s M= ∆ = =
2011 Isotope techniques, F07 (JG) 27
1: Example from Laboratory 2(cont’d)
The measurement result (count rate per 25 µl sample) is subject to the following sources of variation:– The stochastic nature of radioactive decay– Instrument instability ?– Errors (stochastic / systematic) in sample preparation
(pipetting)
If we want the result expressed as activity (Bq) per 25 µl sample, we must add:– Error (uncertainty) in the determination of the counting
efficiency ε
Errors in sample preparation
Stochastic nature of decay
2011 Isotope techniques, F07 (JG) 28
What is best:1. Counting the sample once in 10 min?2. 10 repeated measurements, each of duration 1 min, i.e.
total counting time = 10 min?
If the stochastic nature of radioactive decay is the only source of variation, procedures 1 and 2 will give the same information.
Selecting procedure 2 makes it possible to test the stability of the counting instrumentation.
2: Repeated measurements of the same sample (under identical conditions)
2011 Isotope techniques, F07 (JG) 29
The χ2-test
2011 Isotope techniques, F07 (JG) 30
Error propagation, composite measurements
Rules for estimating the standard error of a composite quantity, based on independent stochastic variables
2 2z x y
z x y
s s s
= ±
= +
Sum or difference:
Product or quotient: /z x y= z xy=eller
22yxz
sssz x y
= +
2011 Isotope techniques, F07 (JG) 31
Example: Correction for background, error estimation
Gross count (radioactive sample + background):
r
MrtMst
∆=
∆∆
=∆
Background:
Net count (radioactive sample – background):
B
BB
Br
MrtM
st
∆=
∆∆
=∆
net B
net B
2 2r r r
r r r
s s s
= −
= +
2011 Isotope techniques, F07 (JG) 32
1536 7.68200
Mrt
∆= = =
∆
BB
B
446 1.12400
Mrt
∆= = =
∆
net B 7.68 1.12 6.56r r r= − = − =
Example: Correction for background, error estimation
r1536 0.196200
Mst
∆= = =
∆
B
Br
B
446 0.053400
Ms
t∆
= = =∆
net B
2 2 2 2 0.196 0.053
0.203r r rs s s= + = +
=
Sample ∆t (s) ∆M (counts)
Unknown 200 1536
Background (B) 400 446
net 6.6 0.2r = ±
cps
cps
cps
cps
cps
cps
cps
2011 Isotope techniques, F07 (JG) 33
Reporting the counting results
Since radioactive decay is a stochastic phenomenon, it is meaningsless to report the results from pulse countings without appending an estimate of the associated error (uncertainty).
E.g., it is senseless to report the result of pulse counting as 6.6 cps.
An estimate of the error of measurement must always be appended :
6.6 ± 0.2 ips
2011 Isotope techniques, F07 (JG) 34
Example from worksheet (Laboratory 1)
net Br r r= −2 2
, ,r net r r Bs s s= +
2011 Isotope techniques, F07 (JG) 35
To every physical measurement is associated a true value.
When describing the validity of measurement data, we must differentiate between:
Precision (reproducibility): How close are the measurements to each other? (repeated measurements of the same quantity)
Accuracy: How close are the measurements to the true value?
Precision and accuracy
2011 Isotope techniques, F07 (JG) 36
Accuracy and precision of measurements
Good accuracy, good precision
Bad accuracy, good precision
Bad accuracy, bad precision
Good accuracy, bad precision
2011 Isotope techniques, F07 (JG) 37
The precision of a method (measurement technique) may be explored by statistical tools
The accuracy of a method can only be ascertained from a detailed knowledge of its systematic sources of error —statistical tools cannot be used for this purpose.
Good accuracy = absence of systematic errors
About precision and accuracy
What is a measurement?(cf. questions to the participants during Laboratory 1)
Measurement: Process of experimentally obtaining one or more quantity values that can reasonable be attributed to a quantity
Quantity: Property of a phenomenon, body or substance, where the property has a magnitude that can be expressed as a number and a reference
Quantity value: Number and reference together expressing the magnitude of a quantity
Measurement principle: Phenomenon serving as a basis of a measurement
2011 Isotope techniques, F07 (JG) 38
Definitions from: International vocabulary of metrology – Basic and general concepts and associated terms (VIM), ISO/IEC Guide 99:2007
... and what that means in practice
Measurement principle: Detecting the number of counts (pulses) in a given period of time in a detector designed to absorb and detect particles or photons of a given kind of ionizing radiation.
Determination of count rate (r = ∆M/∆t)
If the counting efficiency (E) is also known, the count rate may be used to compute the activity of a radioactive sample:
2011 Isotope techniques, F07 (JG) 39
M Nrt t
ε∆ ∆= =
∆ ∆
N rAt ε
∆= =∆
Sources of error in radioactivity measurements– cf. Laboratory 2
2011 Isotope techniques, F07 (JG) 40
Type of measurement
Error source always present
Possible error source
Determining count rate of single sample
•Stochastic nature of radioactive decay (Poisson error)
Instrumental instability (stability test, χ2-test, repeat count of sample)
Determining activity of single sample
•Stochastic nature of radioactive decay (Poisson error)•Error (random/systema-tic) in counting efficiency determination
Instrumental instability
Determining radioactive concentration
•Stochastic nature of radioactive decay (Poisson error)•Error (random/systema-tic) in counting efficiency determination•Error (random/systema-tic) in sample preparation (pipetting error)
Instrumental stability
2011 Isotope techniques, F07 (JG) 41