A dry air mass ascends in the atmosphere from the 100 kPa level to the 50 kPa level. Assuming that it does not mix or exchange heat with its surroundings, and that the initial temperature is 283 K, calculate:
a) the initial specific volume at 100 kPa
b) the final temperature at 50 kPa
c) the final specific volume at 50 kPa
d) the change in specific enthalpy (dh) and specific internal energy (du) during the ascent from 100 to 50 kPa
e) the work of expansion done by 1 m³ of air as it rises from 100 to 50 kPa (note that this is not 'dw', rather it is 'w')
f) what would the specific enthalpy change have been for an isobaric cooling to the same final temperature?
g) what would the specific enthalpy change have been for an isothermal expansion to the same final pressure?