98.7% of the water vapor in the gas at 100°C will condense out in the soil.
How to find fraction?
To determine the fraction of water vapor that condenses out in the soil, compare the partial pressures of water vapor at the initial and final conditions.
Initial conditions:
Temperature: 100°C
Pressure: 98.6 kPa
Dew point: 30°C
Final conditions:
Temperature: 14°C
Pressure: 109.1 kPa
To calculate the partial pressure of water vapor at the initial conditions, use the following equation:

where:
= partial pressure of water vapor
= saturation vapor pressure at the given temperature
RH = relative humidity
The relative humidity can be calculated using the following equation:

where
= actual vapor pressure.
Find the saturation vapor pressure at 30°C from a table of vapor pressures. At 30°C, the saturation vapor pressure is 4.24 kPa.
Plugging in the values for
and RH:
= 4.24 kPa × (30.0% / 100%)
= 1.272 kPa
At 14°C, the saturation vapor pressure of water is 1.22 kPa.
To calculate the partial pressure of water vapor at the final conditions, use the following equation:

where
= initial partial pressure of water vapor.
Plugging in the values for
,
, and
:
= 1.22 kPa × (1.272 kPa / 98.6 kPa)
= 0.016 kPa
To find the fraction of water vapor that condenses:
Fraction of water vapor that condenses =

Plugging in the values for
and
:
Fraction of water vapor that condenses = (1.272 kPa - 0.016 kPa) / 1.272 kPa
= 0.987
Therefore, 98.7% of the water vapor in the gas at 100°C will condense out in the soil.