2. Atmospheric Pressure with Twice the Number of Molecules
If the Earth's atmosphere contained twice the number of molecules, the atmospheric pressure would be greater than it is now. Atmospheric pressure is directly proportional to the number of gas molecules present in a given volume, as described by the ideal gas law (PV = nRT). If the number of molecules (n) doubles while temperature (T) remains constant, then pressure (P) also doubles, leading to higher atmospheric pressure.
3. Difference in Barometer Readings
If two barometers are placed side by side and exposed to the same atmospheric pressure, but one shows a significantly lower column of liquid (let's assume water) than the other, the likely explanation is the type of liquid used in each barometer.
Barometers typically use mercury or water. Mercury is much denser than water. A standard mercury barometer measures atmospheric pressure in inches of mercury, while a water barometer would need a much higher column to exert the same pressure because water's density is lower.
For example, standard atmospheric pressure of 14.7 psi corresponds to about 29.92 inches of mercury but would require a much taller column of water (approximately 34 feet). If the first student's barometer is using water and shows a much lower column, it could be due to using a much smaller diameter tube or it could be indicating a much lower height due to measurement error.
4. Atmospheric Pressure in Inches of Mercury
If the atmospheric pressure is 0.85 atm, we can calculate the corresponding pressure in inches of mercury using the conversion factor that 1 atm = 29.92 inches of mercury.
To calculate:
\[ \text{Pressure in inches of mercury} = 0.85 , \text{atm} \times 29.92 , \text{inches of mercury/atm} \]
Calculating that gives:
\[ \text{Pressure in inches of mercury} ≈ 0.85 \times 29.92 ≈ 25.4 , \text{inches of mercury} \]
Thus, the atmospheric pressure of 0.85 atm corresponds to 25.4 inches of mercury, which is one of the options provided and falls in line with standard values.