Answer:The height of the mercury column is a measure of the atmospheric pressure pushing down on the pool of mercury. The pressure of the atmosphere can be calculated using the equation:
P = ρgh
where P is the pressure in Pascals (Pa), ρ is the density of mercury (13,595 kg/m³), g is the acceleration due to gravity (9.81 m/s²), and h is the height of the mercury column (687 mm = 0.687 m).
First, we need to convert the density of mercury from kg/m³ to g/cm³ to match the units of the height:
ρ = 13,595 kg/m³ = 13.595 g/cm³
Now we can plug in the values and solve for P:
P = ρgh
P = (13.595 g/cm³) x (9.81 m/s²) x (0.687 m)
P = 101,325 Pa
Finally, we can convert the pressure from Pascals to atmospheres:
1 atm = 101,325 Pa
P(atm) = P(Pa) / 101,325 Pa/atm
P(atm) = 101,325 Pa / 101,325 Pa/atm
P(atm) = 1 atm
Therefore, the pressure of the atmosphere around the pool of mercury is 1 atmosphere (atm).
Step-by-step explanation: