The soil temperature in the upper layers of the earth varies with the
variations in the atmospheric conditions. Before a cold front moves in, the
earth at a location is initially at a uniform temperature of \(10^{\circ}
\mathrm{C}\). Then the area is subjected to a temperature of \(-10^{\circ}
\mathrm{C}\) and high winds that resulted in a convection heat transfer
coefficient of \(40 \mathrm{~W} / \mathrm{m}^{2}\). \(\mathrm{K}\) on the earth's
surface for a period of \(10 \mathrm{~h}\). Taking the properties of the soil at
that location to be \(k=0.9 \mathrm{~W} / \mathrm{m} \cdot \mathrm{K}\) and
\(\alpha=1.6 \times 10^{-5} \mathrm{~m}^{2} / \mathrm{s}\), determine the soil
temperature at distances \(0,10,20\), and \(50 \mathrm{~cm}\) from the earth's
surface at the end of this \(10-\mathrm{h}\) period.