Determination Of Vapor Pressure | Types |

Determination Of Vapor Pressure.

Determination Of Vapor Pressure.

Various types of methods for the determination of vapor pressure are

  1. The Static Method.

  2. The Dynamic Method.

Static Method.

In the static method, the liquid under test is evaporated in Vaccum above the mercury column of a barometer, and the decrease in the height of the mercury the column is noted.

Dynamic Method.
In the dynamic method, the liquid is boiled under a definite pressure (usually atmospheric pressure) so that the vapors and the liquid are in equilibrium state due to the external pressure.

The Barometric Method.

It is a typical static method. A long barometric tube filled with mercury is inverted in a dish containing mercury. The mercury falls into the tube until the pressure due to the column of mercury is equal to the atmospheric pressure and there is a vacuum produced at the top of the tube. A small quantity of the pure liquid is then introduced into the vacuum with the help of a bent dropper as shown in the figure. The liquid vaporizes and due to its pressure, the mercury column is pressed down. This depression measured in millimeters or centimeters of mercury represents the vapor pressure p of the liquid at the temperature of the experiment.

Determination Of Vapor Pressure

Isoteniscope Method.

This method is due to Smith and Menzies. The isoteniscope consists of a bulb A of about 2 cm diameter which is fused to a bulbed U-tube B with limbs about 3 – 4 cm long. The bulb is a little more than half-filled with the liquid under examination and 3 to 4 cm3. of the liquid are also placed in the U-tube B. The isoteniscope is then attached to the rest of the apparatus as shown in the figure and placed in a constant temperature bath.

Isoteniscope Method for Measuring Vapor Pressure.
Fig. Isoteniscope Method for Measuring Vapor Pressure.
On evacuation, the liquid in the bulb A begins to boil and expels all the air. The pressure is then cautiously restored by admitting air so that the level of the liquid in the two limbs of the U-tube becomes equal.

Under these conditions the pressure read on the barometric leg when subtracted from the atmospheric pressure gives the vapor pressure of the liquid at the temperature of the experiment because the pressure of the vapor in the bulb A is balanced by the pressure of air introduced to bring the liquid in the two limbs of the U-tube at the same level.

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