Final answer:
The age of the mineral sample can be determined using the half-life of U-238 and the current amounts of U-238 and Pb-206. By comparing the remaining U-238 to the amount of Pb-206, and applying the formula for radioactive decay, we can estimate the time elapsed since the rock formed.
Step-by-step explanation:
To determine the age of the material using radioactive dating and U-238's half-life, we compare the amount of uranium-238 (238U) left in the sample to the amount of lead-206 (206Pb), which is the end product of its decay.
Knowing that the half-life of U-238 is 4.5 × 109 years, we use the following formula that relates the original amount of U-238 (No), the current amount of U-238 (N1), and time (t):
N1 = No(1/2)(t/half-life)
We are given that the sample currently contains 72.0 mg of U-238 and 18.0 mg of Pb-206. Since one mole of U-238 decays into one mole of Pb-206, this means that originally there were (72.0 mg + 18.0 mg) of U-238 in the sample. Using (72 mg + 18 mg) as No and the current 72 mg of U-238 as N1, we substitute these values into the formula:
72 = (72 + 18)(1/2)(t/4.5 × 109)
Solving for t, the age of the rock, we get:
t = (4.5 × 109) × log2((72+18)/72)
Calculating this gives us an age estimate for the rock sample.