Background Radiation: Sources and Measurement

CSEC Physics: The Invisible Radiation Around Us

Essential Understanding: Background radiation is the ever-present ionising radiation that surrounds us every day, coming from natural sources in our environment, from space, and even from within our own bodies. Understanding background radiation is essential for accurate radioactive measurements and appreciating our natural radiation exposure.

🔑 Key Concept: Background is always present
📈 Exam Focus: Three major sources
🎯 Practical Skill: Correcting measurements for background

What is Background Radiation?

📡

Background Radiation Defined

Definition: Background radiation is the ever-present ionising radiation that exists in our environment at all times, originating from natural sources that have been present since before human existence.

Key Characteristics:

  • Cannot be eliminated or reduced to zero
  • Comes from multiple natural sources
  • Present everywhere on Earth and in space
  • Affects all radioactive measurements
  • Exposure is constant throughout our lives

Typical Value: Approximately 2.4 millisieverts (mSv) per year globally

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Why Background Matters in Experiments

The Problem: When measuring radioactivity from a source, the Geiger counter or detector picks up BOTH the radiation from your source AND the background radiation.

The Solution: Subtract the background count rate to get the true activity of your sample.

Formula:

\[ \text{Corrected Count Rate} = \text{Measured Count Rate} – \text{Background Count Rate} \]

Example: If your source measures 85 Bq and background is 5 Bq, the true activity is 80 Bq.

🌟 Did You Know?

Even in “clean” areas with no nuclear facilities or mining, background radiation never drops to zero. This is because cosmic rays from space constantly bombard the Earth, and radioactive elements like uranium, thorium, and potassium-40 are naturally present everywhere in the Earth’s crust, air, water, and even in the foods we eat!

The Three Major Sources of Background Radiation

🌌

1. Cosmic Rays

Source: High-energy particles from outer space, primarily from the Sun and distant stars and galaxies.

Composition:

  • Protons (about 90%)
  • Alpha particles (about 9%)
  • Electrons and other particles (about 1%)

Factors Affecting Exposure:

  • Altitude: Higher at mountains, lower at sea level
  • Latitude: Higher near the poles (Earth’s magnetic field is weaker)
  • Time: Increases during solar flares

Contribution: About 10% of total background exposure

🏔️

2. Terrestrial Radiation

Source: Radioactive materials naturally present in the Earth’s crust, including uranium, thorium, and their decay products.

Key Radionuclides:

  • Uranium-238: Found in rocks and soil
  • Thorium-232: Common in granite and basalt
  • Radon-222: Noble gas produced from uranium decay
  • Potassium-40: Present in rocks and minerals

Factors Affecting Exposure:

  • Local geology (granite areas have higher levels)
  • Building materials (brick and stone homes)
  • Indoor accumulation (poor ventilation)

Contribution: About 50% of total background exposure

🫀

3. Internal Radiation

Source: Radioactive isotopes that are naturally present within our bodies, incorporated through food, water, and air.

Key Radionuclides:

  • Potassium-40 (K-40): Most significant internal source
  • Carbon-14 (C-14): Incorporated into all organic tissue
  • Rubidium-87 (Rb-87): Present in body tissues
  • Polonium-210 (Po-210): Found in respiratory tract

How We Get These:

  • Bananas contain potassium including K-40
  • All organic food contains carbon including C-14
  • Water and air contain trace radioactive elements

Contribution: About 40% of total background exposure

Background Radiation Breakdown by Source

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Visualizing Background Radiation Sources

Objective: Understand the relative contributions of different sources to our total background radiation exposure.

Cosmic Rays

From outer space

10%
Terrestrial

Rocks, soil, radon

50%
Internal

In our bodies (K-40, C-14)

40%

Man-Made Sources of Radiation

While background radiation comes from natural sources, humans also create additional radiation exposure through various activities and medical procedures. These are not part of background radiation but are worth understanding for context.

🏥

Medical Sources

Common Procedures:

  • X-rays (dental, chest, CT scans)
  • CT scans (highest medical dose)
  • Nuclear medicine (radioactive tracers)
  • Radiation therapy for cancer

Average Dose: About 0.6 mSv per year from medical procedures (varies widely)

Note: These are NOT background radiation but ADD to our total exposure.

🏭

Other Man-Made Sources

Additional Exposures:

  • Air travel (increased cosmic ray exposure at altitude)
  • Smoking (polonium-210 in tobacco)
  • Building materials (some contain radioactive elements)
  • Coal power plants (fly ash contains radioactive materials)

Note: Nuclear power plants contribute very little to public exposure (less than 0.1% of total).

Measuring and Accounting for Background Radiation

How to Measure Background Radiation

1
Set up the detector: Place your Geiger-Müller tube in the location where you’ll take measurements, away from any radioactive sources.
2
Take multiple readings: Measure the count rate for at least 2-3 minutes to get a reliable average.
3
Calculate the average: Divide the total counts by the time to get counts per minute (cpm) or convert to Bq if calibrated.
4
Record and subtract: Use this background value to correct all subsequent measurements from your radioactive sources.

Correcting for Background

\[ \text{Source Activity} = \text{Total Reading} – \text{Background Reading} \]

Worked Example:

A Geiger counter reads 85 counts per minute near a radioactive source. When the source is removed, the background reading is 5 counts per minute.

True source activity = 85 – 5 = 80 counts per minute

🔬

Background Correction Simulator

Objective: Practice calculating corrected count rates by subtracting background radiation.

Total Reading

85 Bq

Source + Background

Background

5 Bq

Environmental only

Corrected Reading

80 Bq

Source only

Formula: Corrected Reading = Total Reading – Background Reading

Click “New Problem” to practice more calculations!

🎯

CSEC Examination Mastery Tip

Identifying Background Sources: When asked to identify three sources of background radiation, remember:

  • COSMIC: ☀️ From space (the sky above us)
  • TERRESTRIAL: 🌍 From the Earth (rocks, soil, radon gas)
  • INTERNAL: 🫀 From within us (potassium-40 in our bodies)

Memory Trick: “Cosmic comes from Above, Terrestrial from Below, Internal is Within!”

Remember: Medical X-rays and nuclear power are NOT background radiation – they are additional man-made sources that ADD to our total exposure.

CSEC Practice Arena

Test Your Understanding

1
What is meant by background radiation?
The ever-present ionising radiation from natural sources in our environment
The radiation produced by nuclear power plants
Radiation from medical X-ray machines
The radiation emitted by radioactive waste
Correct Answer: Background radiation is the ever-present ionising radiation from natural sources. It comes from cosmic rays, terrestrial materials, and radioactive isotopes within our own bodies. It cannot be eliminated and is present everywhere.
2
Identify the THREE major sources of background radiation.
Nuclear power plants, medical X-rays, and television sets
Sunlight, ultraviolet radiation, and heat from the Earth
Cosmic rays from space, terrestrial radiation from the Earth, and internal radiation from within our bodies
Mobile phones, WiFi routers, and microwave ovens
Correct Answer: The three major sources of background radiation are:

1. Cosmic rays – high-energy particles from space
2. Terrestrial radiation – radioactive materials in the Earth’s crust
3. Internal radiation – radioactive isotopes like potassium-40 in our bodies
3
A Geiger counter reads 120 counts per minute when placed near a radioactive source. When the source is removed, the reading drops to 8 counts per minute. What is the true activity of the source?
120 counts per minute
8 counts per minute
112 counts per minute
128 counts per minute
Solution: To find the true source activity, subtract the background reading from the total reading:

True Activity = Total Reading – Background
True Activity = 120 – 8 = 112 counts per minute
4
Which radioactive isotope is the most significant source of internal radiation in our bodies?
Carbon-14
Potassium-40
Uranium-238
Radon-222
Correct Answer: Potassium-40 (K-40) is the most significant source of internal radiation in our bodies. We obtain it through food (especially bananas, potatoes, and leafy greens), and it naturally accumulates in our tissues. An average adult contains about 4,000 Bq of potassium-40!

Chapter Summary

Three Major Sources

  • Cosmic Rays: From space (10% of exposure)
  • Terrestrial: From Earth (50% of exposure)
  • Internal: From our bodies (40% of exposure)

Key Formulas

  • Corrected Reading = Total – Background
  • Typical background: ~5-10 Bq depending on location
  • Total annual dose: ~2.4 mSv per year

Remember!

Always subtract background radiation to get accurate measurements!

Background radiation is natural and unavoidable – it surrounds us every moment of every day.

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