To determine how many years ago the organism was alive based on its radioactive decay, we can use the concept of half-life and the relationship between the initial and final activity of the carbon-14 (C-14) isotope. Let's break this down step by step.
Understanding Radioactive Decay
Carbon-14 is a radioactive isotope that is formed in the atmosphere and taken up by living organisms. When an organism dies, it stops absorbing C-14, and the existing C-14 in its body begins to decay at a known rate, characterized by its half-life. The half-life of C-14 is approximately 5730 years, meaning that after this period, half of the original amount of C-14 will have decayed.
Initial and Final Activity
In your scenario, the initial activity of the living organism is 15 decays per minute, and when it is dead, the activity reduces to 9 decays per minute. This reduction in activity indicates that some of the C-14 has decayed since the organism's death.
Calculating the Fraction of C-14 Remaining
To find out how much C-14 remains, we can express the final activity as a fraction of the initial activity:
- Initial activity (A0) = 15 decays/min
- Final activity (At) = 9 decays/min
The fraction of C-14 remaining is:
Fraction remaining = At / A0 = 9 / 15 = 0.6
Using the Half-Life Formula
The relationship between the remaining quantity of a radioactive substance and time can be expressed using the formula:
N(t) = N0 * (1/2)^(t/T1/2)
Where:
- N(t) = remaining quantity after time t
- N0 = initial quantity
- T1/2 = half-life of the substance
In our case, we can rearrange this formula to find the time (t) since the organism died:
0.6 = (1/2)^(t/5730)
Solving for Time
To solve for t, we can take the logarithm of both sides:
log(0.6) = (t/5730) * log(1/2)
Now, we can isolate t:
t = 5730 * (log(0.6) / log(0.5))
Calculating the Values
Using a calculator, we find:
- log(0.6) ≈ -0.2218
- log(0.5) ≈ -0.3010
Now substituting these values into the equation:
t = 5730 * (-0.2218 / -0.3010) ≈ 5730 * 0.736
t ≈ 4224 years
Final Thoughts
This calculation shows that the organism died approximately 4224 years ago. By understanding the principles of radioactive decay and the half-life of C-14, we can effectively determine the age of ancient organic materials. This method is widely used in archaeology and geology to date artifacts and fossils, providing valuable insights into our past.