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Viefleur
3 months ago
10

A geological sample is found to have a Pb-206/U-238 mass ratio of 0.337/1.00. Assuming there was no Pb-206 present when the samp

le was formed, how old is it? The half-life of U-238 is 4.5 × 109 years.1.4 × 1010 years2.1 × 109 years7.3 × 1011 years7.1 × 109 years2.4 × 1010 years
Chemistry
1 answer:
eduard [2.7K]3 months ago
5 0

Answer:

2.1 times 10 to the power of 9 years

Explanation:

U-238 is a radioactive isotope that emits particles as it decays. This results in a reduction of its mass, converting it into Pb-206.

The duration required for a substance to lose half of its mass is defined as its half-life. By knowing both the initial mass (mi) and the resulting mass (m), the number of half-lives that have occurred (n) can be calculated using the following equation:

m = mi divided by 2 raised to the power of n

The mass of Pb-206 corresponds to the mass that U-238 has lost, thus it can be expressed as mi - m. Consequently, the mass ratio can be represented as:

(mi - m) divided by m = 0.337 divided by 1

mi - m = 0.337m

mi = 1.337m

Inserting mi into the half-life equation gives:

m = 1.337m divided by 2 raised to the power of n

2 raised to the power of n = 1.337m divided by m

2 raised to the power of n = 1.337

ln(2 raised to the power of n) = ln(1.337)

n multiplied by ln(2) = ln(1.337)

n = ln(1.337) divided by ln(2)

n = 0.4190

The elapsed time (t), or the approximate age of the sample, is calculated by multiplying the half-life duration by n:

t = 4.5 times 10 to the power of 9 multiplied by 0.4190

t ≈ 1.88 times 10 to the power of 9 years, which is approximately 2.1 times 10 to the power of 9 years.

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