To determine the density of air at 40°F and 1.00 atm, the composition of air is essential, typically approximated as 80% nitrogen and 20% oxygen. Using the ideal gas law (PV = nRT), the number of moles of air can be calculated, leading to a volume of approximately 0.79318 L for 1 g of air. This results in a density of about 1.26 g/L, which aligns closely with the standard density of air under similar conditions. The discussion also touches on calculating the mass of octane needed to heat the air in a room, emphasizing the need for heat capacity and proper stoichiometric calculations. Accurate results depend on using the correct air composition and understanding thermodynamic principles.