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Age of Plant or Animal Calculator

Formula Used:

\[ t = \frac{2.303}{k} \times \log_{10}\left(\frac{N_o}{N_t}\right) \]

1/s
Bq
Bq

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1. What is the Age of Plant or Animal Calculation?

The Age of Plant or Animal calculation uses radiocarbon dating to determine the age of organic materials by measuring the remaining amount of carbon-14. This method is based on the radioactive decay of carbon-14 isotopes over time.

2. How Does the Calculator Work?

The calculator uses the radiocarbon dating formula:

\[ t = \frac{2.303}{k} \times \log_{10}\left(\frac{N_o}{N_t}\right) \]

Where:

Explanation: The formula calculates the time elapsed based on the logarithmic decay of carbon-14 isotopes, using the known disintegration constant.

3. Importance of Carbon-14 Dating

Details: Radiocarbon dating is crucial for archaeology, paleontology, and geology to determine the age of organic materials up to approximately 50,000 years old.

4. Using the Calculator

Tips: Enter the disintegration constant in 1/s, original activity in Bq, and current activity in Bq. All values must be positive numbers.

5. Frequently Asked Questions (FAQ)

Q1: What is the typical value for the disintegration constant of carbon-14?
A: The disintegration constant for carbon-14 is approximately 3.8394 × 10-12 per second, which corresponds to a half-life of about 5,730 years.

Q2: How accurate is carbon-14 dating?
A: Carbon-14 dating is generally accurate for materials up to 50,000 years old, with typical accuracy ranges of ±30-100 years depending on sample quality and measurement precision.

Q3: What types of materials can be dated using this method?
A: This method can date any organic material including wood, charcoal, bone, shell, and other plant/animal remains.

Q4: Why is the logarithm base 10 used in the formula?
A: The formula uses base-10 logarithm for convenience in calculation, though natural logarithm could also be used with appropriate conversion factors.

Q5: What are the limitations of carbon-14 dating?
A: Limitations include contamination of samples, variations in atmospheric carbon-14 levels over time, and the method's inability to date materials older than about 50,000-60,000 years.

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