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Vocabulary practice flashcards covering the kinetic-molecular theory, gas laws (Boyle's, Charles's, Gay-Lussac's, Avogadro's, Ideal, Dalton's), and atmospheric properties.
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Kinetic-molecular theory of gases
A theory describing a gas as particles moving randomly and rapidly, where particle size is small compared to space, no attractive forces exist, and kinetic energy increases with temperature.
Pressure (P)
The force (F) exerted per unit area (A), calculated as Pressure=AF.
Atmosphere (atm) conversion
1 atmosphere (atm) is equal to 760. mm Hg, 760. torr, 14.7 psi, or 101,325 Pa.
Boyle’s law
For a fixed amount of gas at constant temperature, the pressure and volume of the gas are inversely related: P×V=k or P1V1=P2V2.
Charles’s law
For a fixed amount of gas at constant pressure, the volume of the gas is proportional to its Kelvin temperature: TV=k or T1V1=T2V2.
Gay–Lussac’s law
For a fixed amount of gas at constant volume, the pressure of a gas is proportional to its Kelvin temperature: TP=k or T1P1=T2P2.
Combined gas law
An equation that combines Boyle's, Charles's, and Gay-Lussac's laws to show the relationship between P, V, and T: T1P1V1=T2P2V2.
Avogadro’s law
At constant pressure and temperature, the volume of a gas is proportional to the number of moles (n) present: nV=k or n1V1=n2V2.
STP
Standard conditions of temperature and pressure, defined as 1 atm (760 mm Hg) for pressure and 273 K (0 oC) for temperature.
Standard molar volume
The volume of 22.4 L occupied by 1 mole of any gas at STP.
Ideal gas law
A single equation that combines pressure, volume, moles, and temperature: PV=nRT.
Universal gas constant (R)
A constant used in the ideal gas law; its value is 0.0821 L×atm/(mol×K) for atm or 62.4 L×mm Hg/(mol×K) for mm Hg.
Dalton’s law
States that the total pressure (Ptotal) of a gas mixture is the sum of the partial pressures of its component gases: Ptotal=PA+PB+PC.
Ozone (O3)
A gas formed in the upper atmosphere from O2 and O that acts as a shield by absorbing destructive ultraviolet radiation.
Global warming
An increase in the average temperature of the earth's atmosphere, contributed to by greenhouse gases like CO2 which absorb thermal energy.