Uses of Radioisotopes: Medicine, Industry, and Carbon Dating
CSEC Physics: Real-World Applications
Essential Understanding: Radioactive isotopes have practical applications in medicine, industry, and archaeology. The predictable decay of radioisotopes allows us to use them as tracers, for cancer treatment, and for determining the age of ancient artifacts. This article explores how scientists harness the power of radioactivity for beneficial purposes.
What Are Radioisotopes?
Radioisotopes are radioactive forms of elements. They have the same chemical properties as stable isotopes of the same element, but their nuclei are unstable and emit radiation as they decay. This property makes them incredibly useful in various applications.
⚗️ Chemical Identity
Radioisotopes behave identically to their stable counterparts in chemical reactions, allowing them to be absorbed by living organisms or incorporated into materials without detection.
☢️ Radioactive Emission
The decay process emits detectable radiation (alpha, beta, or gamma rays), which allows scientists to track the position and movement of the radioisotope.
⏱️ Predictable Half-Life
Each radioisotope decays at a constant, predictable rate. This allows scientists to calculate time elapsed (in carbon dating) or ensure the radioactivity diminishes to safe levels.
Medical Applications
🩺 Medical Tracers - Technetium-99m
What it is: Technetium-99m (the "m" stands for metastable) is the most widely used radioisotope in medicine. It emits gamma rays that can be detected by special cameras.
How it works:
- Technetium-99m is attached to a compound that targets specific organs or tissues
- The patient receives the tracer through injection, inhalation, or swallowing
- A gamma camera detects the gamma rays and creates images of the organ
- Abnormalities appear as "hot spots" (more tracer) or "cold spots" (less tracer)
Uses:
- Heart scans to detect blocked arteries
- Bone scans to identify tumors or fractures
- Thyroid scans to assess function
- Lung scans to check for blood clots
💉 Radiotherapy - Cobalt-60 and Iodine-131
How it works: High-energy gamma radiation from radioisotopes can destroy cancer cells while minimizing damage to surrounding healthy tissue.
Cobalt-60 Therapy:
- Used in external beam radiation therapy
- Precise gamma rays target tumors deep within the body
- Non-invasive alternative to surgery for some cancers
Iodine-131 Therapy:
- Taken up by the thyroid gland naturally
- Used to treat overactive thyroid (hyperthyroidism) and thyroid cancer
- Beta radiation destroys overactive thyroid cells
Industrial Applications
🔧 Tracers in Industry
Radioisotopes serve as "tracers" to track the movement of materials through complex systems.
Pipeline Leak Detection:
- A small amount of radioactive material is added to the fluid in a pipeline
- Geiger counters are used to scan the area around the pipeline
- Higher than normal radiation readings indicate the location of a leak
- This method is fast, accurate, and doesn't require excavating the entire pipeline
Thickness Gauging:
- Beta emitters (such as Strontium-90) are used to measure paper, plastic, or metal sheet thickness
- Radiation passing through the material is measured by a detector on the other side
- Less radiation reaches the detector if the material is thicker
- Readings are used to automatically adjust rolling mills for consistent thickness
🔬 Sterilization
Gamma radiation from Cobalt-60 is used to sterilize medical equipment, food products, and cosmetics. The high-energy radiation kills bacteria, viruses, and other pathogens without heating the product or leaving residue.
Carbon Dating
The Science of Carbon-14 Dating
Where:
- N = remaining amount of Carbon-14
- N₀ = original amount of Carbon-14
- n = number of half-lives that have passed
🌳 How Carbon-14 Dating Works
Step 1: Carbon-14 Formation
Carbon-14 (¹⁴C) is continuously formed in the upper atmosphere when cosmic rays collide with nitrogen atoms:
\[ ^14_7N + ^1_0n \rightarrow ^14_6C + ^1_1H \]
Step 2: Carbon-14 Enters Living Organisms
Plants absorb CO₂ containing Carbon-14 from the atmosphere. Animals obtain Carbon-14 by eating plants. The ratio of Carbon-14 to Carbon-12 remains constant in living organisms.
Step 3: After Death
When an organism dies, it no longer absorbs Carbon-14. The existing Carbon-14 begins to decay with a half-life of approximately 5,730 years.
Step 4: Measuring and Calculating
Scientists measure the ratio of Carbon-14 to Carbon-12 in the sample and use the half-life formula to calculate when the organism died.
Carbon-14 Half-Life Timeline
100% ¹⁴C
Living
50% ¹⁴C
5,730 years
25% ¹⁴C
11,460 years
12.5% ¹⁴C
17,190 years
6.25% ¹⁴C
22,920 years
3.1% ¹⁴C
28,650 years
🧮 Carbon Dating Calculator
Enter the percentage of Carbon-14 remaining to calculate the age of the sample!
Other Dating Methods
🪨 Potassium-Argon Dating
Half-life: 1.25 billion years
Used for: Dating very old rocks and geological formations (millions to billions of years old)
Used to determine the age of the Earth and prehistoric volcanic eruptions.
🌋 Uranium-Lead Dating
Half-life: 4.5 billion years
Used for: Dating the oldest rocks on Earth and meteorites
Considered the most accurate method for dating ancient geological samples.
☢️ Tritium Dating
Half-life: 12.3 years
Used for: Dating young groundwater and ocean water (recent decades)
Useful for tracking the movement of water in aquifers and oceans.
Safety Considerations
- Using lead shielding to block radiation
- Maintaining safe distances from radioactive sources
- Limiting exposure time
- Wearing dosimeters to monitor exposure levels
Summary: Key Takeaways
- Medical Tracers: Technetium-99m is used for imaging organs and detecting abnormalities
- Radiotherapy: Cobalt-60 and Iodine-131 are used to treat cancer
- Industrial Tracers: Radioisotopes detect leaks and measure material thickness
- Carbon-14 Dating: Uses the 5,730-year half-life to determine the age of organic materials up to 50,000 years old
- Safety: Radioisotopes must be handled with proper shielding, distance, and time management
- Half-Life Formula: Apply \( N = N_0 \times (1/2)^n \) to calculate remaining amounts or time elapsed
