The traditional calculation to measure a fall through Earth assumes that our planet has a constant density throughout its many layers.
The new approach assumes that when the different densities of Earth's layers are taken into account, the trip is four minutes shorter than predicted.
To get a realistic mass distribution for Earth, Alexander Klotz, a graduate student in physics at McGill University in Canada, relied on the Preliminary Reference Earth Model, which is based on seismic data.
Solving the problem numerically, Klotz found that an object should fall through Earth in 38 minutes and 11 seconds, instead of the 42 minutes and 12 seconds predicted assuming a uniform planet, 'Science magazine' reported.
Klotz found that he got almost exactly the same answer - 38 minutes flat - if he simply assumed that the force of gravity remained constant and equal to the value at the surface as an object plummeted towards the centre.
The research was published in the American Journal of Physics.
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