The boiling temperature of nitrogen at atmospheric pressure at sea level ( 1
atm pressure) is \(-196^{\circ} \mathrm{C}\). Therefore, nitrogen is commonly
used in low-temperature scientific studies since the temperature of liquid
nitrogen in a tank open to the atmosphere will remain constant at
\(-196^{\circ} \mathrm{C}\) until it is depleted. Any heat transfer to the tank
will result in the evaporation of some liquid nitrogen, which has a heat of
vaporization of \(198 \mathrm{~kJ} / \mathrm{kg}\) and a density of \(810
\mathrm{~kg} / \mathrm{m}^{3}\) at 1 atm.
Consider a 3-m-diameter spherical tank that is initially filled with liquid
nitrogen at 1 atm and \(-196^{\circ} \mathrm{C}\). The tank is exposed to
ambient air at \(15^{\circ} \mathrm{C}\), with a combined convection and
radiation heat transfer coefficient of \(35 \mathrm{~W} / \mathrm{m}^{2} \cdot
\mathrm{K}\). The temperature of the thin-shelled spherical tank is observed to
be almost the same as the temperature of the nitrogen inside. Determine the
rate of evaporation of the liquid nitrogen in the tank as a result of the heat
transfer from the ambient air if the tank is \((a)\) not insulated, \((b)\)
insulated with 5 -cm-thick fiberglass insulation \((k=0.035 \mathrm{~W} /
\mathrm{m} \cdot \mathrm{K})\), and (c) insulated with 2 -cm-thick
superinsulation which has an effective thermal conductivity of \(0.00005
\mathrm{~W} / \mathrm{m} \cdot \mathrm{K}\).