Gases.

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Presentation transcript:

Gases

The Nature of Gases Gases expand to fill their containers Gases are fluid – they flow Gases have low density 1/1000 the density of the equivalent liquid or solid Gases are compressible Gases effuse and diffuse

Ideal Gases Ideal gases are imaginary gases that perfectly fit all of the assumptions of the kinetic molecular theory. Gases consist of tiny particles that are far apart relative to their size. Collisions between gas particles and between particles and the walls of the container are elastic collisions Pressure is the force created by the collisions of molecules with the walls of a container

Ideal Gases (continued) Gas particles are in constant, rapid motion. They therefore possess kinetic energy, the energy of motion There are no forces of attraction between gas particles The average kinetic energy of gas particles depends on temperature, not on the identity of the particle.

Measuring Pressure The first device for measuring atmospheric pressure was developed by Evangelista Torricelli during the 17th century. The device was called a “barometer” Baro = weight Meter = measure

An Early Barometer The normal pressure due to the atmosphere at sea level can support a column of mercury that is 760 mm high.

Pressure Unit Symbol Definition/Relationship Pascal Pa SI pressure unit 1 Pa = 1 newton/meter2 Millimeter of mercury mm Hg Pressure that supports a 1 mm column of mercury in a barometer Atmosphere atm Average atmospheric pressure at sea level and 0 °C Torr torr 1 torr = 1 mm Hg

Standard Pressure 1 standard atmosphere (atm) 101.3 kPa (kilopascals) 14.7 lbs/in2 760 mm Hg (millimeters of mercury) 760 torr

The Kelvin Scale

Standard Temperature and Pressure “STP” Either of these: 273 Kelvin (273 K) 0 °C Standard Temperature and Pressure “STP” And any one of these: 1 atm 101.3 kPa 14.7 lbs/in2 (psi) 760 mm Hg 760 torr