Radioactive Decay: 66.6 Mg Initial Mass, 22-Hour Half-Life

by Alex Johnson 59 views

In the fascinating world of nuclear physics, radioactive decay plays a pivotal role. It's a natural process where unstable atomic nuclei lose energy by emitting radiation, transforming into a different atomic nucleus. This process is governed by the principles of exponential decay, making it predictable and quantifiable. Let's delve into a specific scenario: A sample of a radioactive substance starts with an initial mass of 66.6 mg, and this substance decays following a continuous exponential decay model, having a half-life of 22 hours. This article will explore the ins and outs of this scenario, helping you understand the underlying mathematical concepts and practical implications.

Defining Radioactive Decay

At its core, radioactive decay is a spontaneous process. Imagine a room full of popcorn kernels – some will pop sooner, others later, and you can't predict exactly when each kernel will pop. Radioactive decay is similar; you can't pinpoint when a specific atom will decay, but you can statistically predict the decay rate of a large group of atoms. This statistical behavior is beautifully described by the exponential decay model. The exponential decay model hinges on the concept of half-life, which is the time it takes for half of the radioactive material to decay. In our example, the half-life is 22 hours, meaning that every 22 hours, the amount of the radioactive substance is reduced by half. This constant halving is the hallmark of exponential decay.

Exponential Decay Formula

The magic behind quantifying radioactive decay lies in the exponential decay formula. This formula allows us to calculate the amount of radioactive substance remaining after a certain time. The formula is generally expressed as:

N(t) = N₀ * e^(-kt)

Where:

  • N(t) is the amount of the substance remaining after time t.
  • N₀ is the initial amount of the substance.
  • e is the base of the natural logarithm (approximately 2.71828).
  • k is the decay constant, which is specific to the radioactive substance.
  • t is the time elapsed.

In our case, N₀ is 66.6 mg, and we know the half-life is 22 hours. To use the formula effectively, we need to determine the decay constant k. The decay constant is related to the half-life (T₁/₂) by the following equation:

k = ln(2) / T₁/₂

Where ln(2) is the natural logarithm of 2 (approximately 0.693). Plugging in our half-life of 22 hours, we get:

k = 0.693 / 22 ≈ 0.0315 per hour

Now we have all the pieces of the puzzle! We know the initial amount (N₀), the decay constant (k), and we can plug in any time t to find the amount of substance remaining (N(t)).

Applying the Model: Calculations and Predictions

Now, let's put our knowledge into action. Suppose we want to know how much of the radioactive substance remains after 44 hours. This is equivalent to two half-lives, so we would intuitively expect the amount to be reduced to one-quarter of the original. Let's verify this using the formula.

Calculating Remaining Mass

Using the exponential decay formula:

N(44) = 66.6 mg * e^(-0.0315 * 44)
N(44) = 66.6 mg * e^(-1.386)
N(44) ≈ 66.6 mg * 0.25
N(44) ≈ 16.65 mg

As expected, after 44 hours (two half-lives), approximately 16.65 mg of the substance remains, which is indeed one-quarter of the initial amount. This demonstrates the power of the exponential decay model in predicting the behavior of radioactive substances over time.

Determining Time for Specific Mass

What if we want to know how long it will take for the substance to decay to a specific mass, say 10 mg? In this case, we need to rearrange the exponential decay formula to solve for t:

t = (ln(N(t) / N₀)) / -k

Plugging in our values:

t = (ln(10 mg / 66.6 mg)) / -0.0315
t = (ln(0.1502)) / -0.0315
t ≈ (-1.896) / -0.0315
t ≈ 60.2 hours

So, it will take approximately 60.2 hours for the radioactive substance to decay to 10 mg. This type of calculation is crucial in various applications, such as determining the age of artifacts using carbon dating or calculating the safe storage time for radioactive waste.

Real-World Applications of Radioactive Decay

Radioactive decay isn't just a theoretical concept; it has profound implications and numerous applications across various fields.

Medical Applications

In medicine, radioactive isotopes are used for both diagnostic and therapeutic purposes. For example, radioactive iodine is used to treat thyroid cancer, and radioactive tracers are used in medical imaging to visualize organs and tissues. The precise knowledge of decay rates is essential for ensuring the correct dosage and minimizing patient exposure to radiation.

Carbon Dating

One of the most well-known applications of radioactive decay is carbon dating. Carbon-14, a radioactive isotope of carbon, is used to determine the age of organic materials up to about 50,000 years old. By measuring the amount of Carbon-14 remaining in a sample, scientists can estimate when the organism died. This technique has revolutionized archaeology and paleontology.

Industrial Applications

Radioactive materials are also used in various industrial applications, such as gauging the thickness of materials, sterilizing medical equipment, and tracing the flow of liquids and gases in pipelines. Understanding the decay rates is crucial for ensuring the safety and effectiveness of these applications.

Nuclear Power

The heart of nuclear power plants lies in controlled nuclear fission, a process involving the radioactive decay of heavy elements like uranium. The energy released during fission is used to generate electricity. Managing the radioactive waste produced by nuclear power plants is a significant challenge, requiring a deep understanding of decay processes and long-term storage solutions.

Factors Influencing Radioactive Decay

While the exponential decay model is remarkably accurate, it's important to understand its limitations. The decay rate of a radioactive substance is primarily governed by its nuclear properties and is generally unaffected by external factors like temperature, pressure, or chemical environment. This makes radioactive decay a reliable