10.1 - Radioactivity Flashcards
How has radiation been important to our evolution
Human beings can survive small doses of nuclear radiation relatively unscathed. This has been important in our evolution, as the natural environment incorporates low levels of radiation from natural sources. This is called background radiation.
In the uk what is background radiation like
In the uk it averages to less than one radioactive particle every two seconds in any given place.
How could we measure background radiation, what result would you expect
If we measure background radiation using a Geiger-Müller (G-M) tube, the number of counts per second usually ranges from 0.2 - 0.5 depending on the exact location.
How are radiation levels often reported
Radiation levels are often reported in counts per second, and the unit is called the becquerel (Bq) after Henri Becquerel, the frêńçh physicist credited with the discovery of spontaneous radiation in 1896.
Levels of background radiation dose in Great Britain is measured in Bq….
A unit for measuring radiation energy delivered to the body.
What are the sources of background radiation
Radon gas (50%) Ground and buildings (14%) Medical (14%) Food and drink (11.5%) Cosmic rays (10%) Nuclear power and weapons (0.3%) Other (0.2%)
Tell me about the background radiation sources in WORDS
The actual exposure to nuclear radiation that any individual will receive from their environment will depend on where they are and for how long, as different environmental factors contribute to the local level of background radiation. On earth, approximately half of the background radiation is from naturally radioactive gases in the atmosphere, particularly radon.
Where is radon produced
Radon is produced in the decay of uranium ore present in certain rocks (especially granite) and thus is more prevalent in certain parts of the world than others. In Cornwall in the uk, some houses are fitted with radon detectors and special ventilation systems to flush out excess radon gas from the household atmosphere.
Where is the most naturally radioactive place on earth? Fun fact
Ramsar, in Iran, where the dosage can be more than 200 times the natural dose rate in the uk.
How can we investigate background radiation
It is easy to determine the average background radiation in your area using a Geiger muller tube and counter. As radioactive decay is a random and spontaneous process, the activity in your lab must be measured over a long period of time (30 minutes or more) and then an average calculated. Otherwise, you may find that the measurement is, by chance, particularly high or particularly low and thus does not truly indicate the average over time. For example, if the G-M tube and counter are set to counting for two hours, and the final count is then divided by 7200(seconds), this will give a good approximation to the average over time as the count time is long compared with the average count of about 0.5 Bq. Measurements of radioactivity that have had the background radiation deducted, so that they only represent activity by a radioactive source under test, are known as corrected counts.
What are corrected counts
Measurements of radioactivity that have had the background radiation deducted, so that they only represent activity by a radioactive source under test, are known as corrected counts.
The background count will skew the results of investigations into nuclear radiations what must we do
Whenever such an investigation is undertaken, the background radiation must also be measured separately and then deducted from each count measured in the main part of the investigation.
Many nuclei are slightly unstable and there is a slight probability that, each second they may …..
Decay
What does decay mean
With a nuclei, this means that a nucleon may change from one type to another, or the composition or energy state of the nucleus as a whole may change.
When a nuclear decay occurs, what happens
The radiation particle emitted will leave the nucleus carrying a certain amount of kinetic energy.
As the particle travels, it will ionise particles in its path, losing a small amount of that kinetic energy at each ionisation. When all the kinetic energy is transferred, the radiation particle stops and is absorbed by the substance it is in at that moment.
What are the three main types of nuclear radiation
Alpha (a symbol ish)
Beta (B)
Gamma (y) radiation.
Each one comes about through a different process within the nucleus, each one is composed of different particles, and each one has different properties.
How can we investigate radiation penetration
You can investigate the penetrating power of alpha, beta and gamma radiation using a Geiger-Müller tube to detect them. Between the source and the GM tube, place absorber sheets that progressively increase in density, and measure the average count rate. This investigation is often simulated using computer software. This removes all risk of exposure to radiological hazards.
The absorber sheets will be made from paper, lead and aluminium. Use a data logging computer to record counts.
What are alpha particles
Alpha particles are composed of two protons and two neutrons, the same as a helium nucleus.
How ionising are alpha particles
This is a relatively large particle with a significant positive charge (+2e), so it is highly ionising.
An alpha particle moving through air typically causes 10,000 ionisations per millimetre. As it ionises so much, it quickly loses its kinetic energy and is easily absorbed. A few centimetres travel in air is enough to absorb an alpha particle, and they are also blocked by paper or skin.
Tell me an example of an alpha decay equation
241,95 Am —> 237,93 Np + 4,2 a
What is the decay constant symbol
Lamder symbol
What is the decay constant
Since radioactive decay is a spontaneous and random process, any radioactive nucleus may decay at any moment. For each second that it exists, there is a certain probability that the nucleus will decay. This probability is called the decay constant.
Can we predict when a nucleus will decay
Just like guessing which number will come up next in a lottery, it is not possible to predict when any given nucleus will decay. The likelihood that a particular nucleus will decay is not affected by factors outside the nucleus, such as temperature or pressure, or by the behaviour of neighbouring nuclei - each nucleus decays entirely independently.
If we have a large sample of the nuclei, what will the probability of decay determine
The fraction of these nuclei that will decay each second. Naturally, if the sample is larger, then the number that decay in a second will be greater.
The number decaying per second is called
The activity
What is the symbol for activity
A (or dN/dt)
What is activity proportional to
The number of nuclei in the sample,N.
Mathematically how is activity expressed
A = -lamder x N
dN/dt = -lamder x N
The minus sign in this formula occurs because the number of nuclei in the sample, N, decreases with time. In practice we ignore the negative sign when using the formula.
What’s the unit for the decay constant
s^-1
What activity, A measured in
Bq
How is the formula for the rate of decay of nuclei in a sample formed
It’s a differential equation. We have previously met this type of equation when studying the discharge of a capacitor. The equation
dN/dt = -lamder x N can be solved to give a formula for the number of nuclei remaining in a sample, N, after a certain time, t:
N = N(subscript 0) x e(^-lamder x t)
Where N(subscript 0) is the initial number of nuclei within a sample.
The exponential mathematics that govern radioactive decay is identical in structure to those for the discharge of capacitors.
N is the number of nuclei…
REMAINING in a sample.
Tell me about half life as a measure of activity
As we have seen, the activity of a radioactive sample decreases over time as the radioactive nuclei decay, leaving fewer radioactive nuclei available to decay. While the activity of a sample depends on the number of nuclei present, the rate at which the activity decreases depends only on the particular isotope. A measure of this rate of decrease of activity is the half life, t(subscript 1/2)
The rate at which the activity decreases depends only on the…
Particular isotope
Half life is a measure of
Rate of decrease of activity
What is half life ?
This is the TIME taken for half of the atoms of that nuclide (type of atom/isotope) within a sample to decay.
Mathematically, how can the half life equation be found
By putting N = 1/2N(subscript 0) into the decay equation
N = N(subscript 0) x e(^-lamder x t)
N(subscript 0)/2 = N(subscript 0) x e(^-lamder x t(subscript 1/2)
N(subscript 0) cancels out on both sides
1/2 = e(^-lamder x t(subscript1/2)
Take natural logs
ln(1/2) = -lamder x t(subscript 1/2)
-ln(2) = -lamder x t(subscript 1/2)
t(subscript 1/2) = ln(2)/lamder
Rearranging this also gives us an equation for the decay constant
Lamder = ln(2)/t(subscript 1/2)