When gasses are collected by water displacement, there is always water vapor (gaseous water) present. The amount of water vapor present depends on the temperature. The greater the temperature, the more water vapor present (this quantity is called the vapor pressure). A 1.00 L volume of nitrogen gas measured at 290 K and 0.978 atm was collected at 290 K by water displacement. Use Dalton's Law and the Ideal Gas Law to determine the number of moles of nitrogen gas that were collected. At 290 K, the vapor pressure of water is 14.59 Torr.

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3. When gasses are collected by water displacement, there is always water vapor (gaseous water)
present. The amount of water vapor present depends on the temperature. The greater the
temperature, the more water vapor present (this quantity is called the vapor pressure). A 1.00 L
volume of nitrogen gas measured at 290 K and 0.978 atm was collected at 290 K by water
displacement. Use Dalton's Law and the Ideal Gas Law to determine the number of moles of
nitrogen gas that were collected. At 290 K, the vapor pressure of water is 14.59 Torr.
Transcribed Image Text:3. When gasses are collected by water displacement, there is always water vapor (gaseous water) present. The amount of water vapor present depends on the temperature. The greater the temperature, the more water vapor present (this quantity is called the vapor pressure). A 1.00 L volume of nitrogen gas measured at 290 K and 0.978 atm was collected at 290 K by water displacement. Use Dalton's Law and the Ideal Gas Law to determine the number of moles of nitrogen gas that were collected. At 290 K, the vapor pressure of water is 14.59 Torr.
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