Lecture Presentation. Chapter 10. Gases. John D. Bookstaver St. Charles Community College Cottleville, MO Pearson Education, Inc.

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Transcription:

Lecture Presentation Chapter 10 John D. Bookstaver St. Charles Community College Cottleville, MO

Characteristics of Unlike liquids and solids, gases Expand to fill their containers. Are highly compressible. Have extremely low densities.

Pressure is the amount of force applied to an area: Pressure P = F A Atmospheric pressure is the weight of air per unit of area.

Units of Pressure Pascals 1 Pa = 1 N/m 2 Bar 1 bar = 10 5 Pa = 100 kpa

Units of Pressure mmhg or torr These units are literally the difference in the heights measured in mm (h) of two connected columns of mercury. Atmosphere 1.00 atm = 760 torr

Manometer The manometer is used to measure the difference in pressure between atmospheric pressure and that of a gas in a vessel.

Standard Pressure Normal atmospheric pressure at sea level is referred to as standard pressure. It is equal to 1.00 atm 760 torr (760 mmhg) 101.325 kpa

Boyle s Law The volume of a fixed quantity of gas at constant temperature is inversely proportional to the pressure.

P and V are Inversely Proportional PV = k Since A plot of V versus P results in a curve. V = k (1/P) This means a plot of V versus 1/P will be a straight line.

Charles s Law The volume of a fixed amount of gas at constant pressure is directly proportional to its absolute temperature.

Charles s Law So, V T = k A plot of V versus T will be a straight line.

Avogadro s Law The volume of a gas at constant temperature and pressure is directly proportional to the number of moles of the gas. Mathematically, this means V = kn

Ideal-Gas Equation So far we ve seen that V 1/P (Boyle s law) V T (Charles s law) V n (Avogadro s law) Combining these, we get V nt P

Ideal-Gas Equation The constant of proportionality is known as R, the gas constant.

Ideal-Gas Equation The relationship V nt P then becomes V = R or nt P PV = nrt

Densities of If we divide both sides of the ideal-gas equation by V and by RT, we get n V = P RT

Densities of We know that Moles molecular mass = mass n = m So multiplying both sides by the molecular mass ( ) gives m V = P RT

Densities of Mass volume = density So, d = m V = P RT Note: One needs to know only the molecular mass, the pressure, and the temperature to calculate the density of a gas.

Molecular Mass We can manipulate the density equation to enable us to find the molecular mass of a gas: d = P RT becomes = drt P

Dalton s Law of Partial Pressures The total pressure of a mixture of gases equals the sum of the pressures that each would exert if it were present alone. In other words, P total = P 1 + P 2 + P 3 +

Partial Pressures When one collects a gas over water, there is water vapor mixed in with the gas. To find only the pressure of the desired gas, one must subtract the vapor pressure of water from the total pressure.

Kinetic-Molecular Theory This is a model that aids in our understanding of what happens to gas particles as environmental conditions change.

Main Tenets of Kinetic-Molecular Theory consist of large numbers of molecules that are in continuous, random motion.

Main Tenets of Kinetic-Molecular Theory The combined volume of all the molecules of the gas is negligible relative to the total volume in which the gas is contained.

Main Tenets of Kinetic-Molecular Theory Attractive and repulsive forces between gas molecules are negligible.

Main Tenets of Kinetic-Molecular Theory Energy can be transferred between molecules during collisions, but the average kinetic energy of the molecules does not change with time, as long as the temperature of the gas remains constant.

Main Tenets of Kinetic-Molecular Theory The average kinetic energy of the molecules is proportional to the absolute temperature.

Effusion Effusion is the escape of gas molecules through a tiny hole into an evacuated space.

Effusion The difference in the rates of effusion for helium and nitrogen, for example, explains why a helium balloon would deflate faster.

Diffusion Diffusion is the spread of one substance throughout a space or throughout a second substance.

Graham's Law KE 1 = KE 2 1/2 m 1 v 1 2 = 1/2 m 2 v 2 2 m 1 v = 2 m 2 2 v 1 2 m 1 v 2 = 2 m 2 v 2 1 = v 2 v 1

Real In the real world, the behavior of gases only conforms to the ideal-gas equation at relatively high temperature and low pressure.

Real Even the same gas will show wildly different behavior under high pressure at different temperatures.

Deviations from Ideal Behavior The assumptions made in the kinetic-molecular model (negligible volume of gas molecules themselves, no attractive forces between gas molecules, etc.) break down at high pressure and/or low temperature.

Corrections for Nonideal Behavior The ideal-gas equation can be adjusted to take these deviations from ideal behavior into account. The corrected ideal-gas equation is known as the van der Waals equation.

The van der Waals Equation (P + n 2 a V 2 ) (V nb) = nrt