I am trying to perform the calculation that Luis Alvarez used to establish the size of the K-T impactor. I used the following information:
- Assume that the clay layer with iridium was uniformly distributed around Earth by the impact.
- On average, the layer had a concentration of iridium of 10 parts per billion (ppb) by weight.
- On average, the layer was 4 cm thick.
- The density of the layer was 2.5 g/cm3.
- Assume the meteor was spherical, with a density of 6.0 g/cm3, and an iridium content of 0.5 parts per million (ppm) by weight.
- The radius of Earth is 6378 km.
What is the diameter of the meteorite? The answer isn't exactly 10 km, as stated. By how much would you have to change the assumed thickness of the iridium layer to arrive at an asteroid diameter of exactly 10 km?
My attempt:
$m_{layer} = \pi(2.5 g/cm^3)((6378 \cdot 10^5)^4 - (6378 \cdot 10^5 - 4)^4) = 3.26 \cdot 10^{28} g$
$m_{iridiuminlayer} = (3.26 \cdot 10^{28})(10^{-8}) = 3.26\cdot 10^{20} g$
Here is where I get stuck. It seems there is not sufficient information to calculate the radius of the meteor, as D = m/V, and we are given density and a mass ratio. I tried doing the second portion, in which you assume the diameter of the asteroid is 10 km, calculating the mass of the meteor, the iridium in the meteor, and the average iridium distribution over Earth's surface. I would be able to solve the rest of the question if I knew how to calculate the Volume/mass of the meteor. Please help!