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Page 1: Topic 12 Topic 12 Topic 12: Kinetic Theory Table of Contents Topic 12 Topic 12 Basic Concepts Additional Concepts

Topic 12Topic 12

Page 2: Topic 12 Topic 12 Topic 12: Kinetic Theory Table of Contents Topic 12 Topic 12 Basic Concepts Additional Concepts

Topic 12: Kinetic Theory

Table of ContentsTable of ContentsTopic 12Topic 12

Basic Concepts

Additional Concepts

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• In the late 1800s, two scientists, Ludwig Boltzmann and James Maxwell, independently proposed a model to explain the properties of gases in terms of particles in motion. This model is now known as the kinetic-molecular theory.

Gases

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• The model makes the following assumptions about the size, motion, and energy of gas particles.

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• The particles in a gas are separated from one another by empty space.

Particle size

• The volume of the empty space is much greater than the volume of the gas particles themselves.

• Because gas particles are far apart, there are no significant attractive or repulsive forces among them.

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• Gas particles are in constant, random motion. Until they bump into something (another particle or the side of a container), particles move in a straight line.

Particle motion

• When gas particles do collide with something, the collision is said to be elastic.

• An elastic collision is one in which no kinetic energy is lost.

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Particle energy

• Mass and velocity determine the kinetic energy of a particle, as represented in the equation below.

KE = kinetic energym= mass of the particlev = velocity of the particle

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Particle energy

• The velocity of a particle includes both its speed and its direction.

• Each particle in a sample containing only one gas will have the same mass but not the same velocity.

• Thus, all the particles in a sample of gas do not have the same kinetic energy.

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Particle energy

• Temperature is a measure of the average kinetic energy of the particles in a sample of matter.

• At a given temperature, all gases have the same average kinetic energy.

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Explaining the behavior of gases

• The kinetic-molecular theory explains the following behavior of gases.

• Low Density Density is a measure of mass per unit volume. The difference between the high density of a solid and the low density of a gas is due mainly to the large amount of space between the particles in the gas. There are fewer particles in a gas than in a solid of the same volume.

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Explaining the behavior of gases

• Compression and expansion A gas will expand to fill its container. Thus, the density of a sample of gas will change with the volume of the container it is placed in. The gas will become more dense as it is compressed into a smaller container. The gas will become less dense as it expands in a larger container.

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• Diffusion refers to the movement of one material through another, such as when onegas flows into a space already occupied by another gas.

Explaining the behavior of gases

• Diffusion Gas particles flow past each other easily because there are no significant forces of attraction between them.

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• Effusion If you have ever seen a tire deflate from a puncture, you are familiar with effusion. Effusion is the escape of a gas through a small opening in its container.

Explaining the behavior of gases

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Gas pressure

• When gas particles collide with the walls of their container, they exert pressure on the walls.

• Pressure is force per unit area.

• The pressure exerted by the particles in the atmosphere that surrounds Earth is called atmospheric pressure, or air pressure.

• Air pressure varies at different locations on Earth.

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Gas pressure

• Air pressure at higher altitudes, such as on a mountaintop, is slightly lower than air pressure at sea level.

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• At Earth’s surface, air pressure is approximately equal to the pressure exerted bya 1-kilogram mass on a square centimeter.

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Gas pressure

• Air pressure is measured using a barometer.

• A barometer consists of a thin tube closed on one end and filled with mercury.

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Gas pressure

• The tube is placed so that the level of the mercury is determined by air pressure.

• The mercury rises when the air pressure increases and falls when the air pressure decreases.

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Forces of Attraction

• The attractive forces that hold particles together in ionic, covalent, and metallic bonds are called intramolecular forces.

• Intermolecular forces, which are weaker than intramolecular forces, also can hold particles together.

• Three types of intermolecular forces are described below: dispersion forces, dipole–dipole forces, and hydrogen bonds.

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Dispersion forces

• Weak forces that result from temporary shifts in the density of electrons in electron clouds are called dispersion forces, or London forces.

• When two nonpolar molecules are in close contact, the electron cloud of one molecule repels the electron cloud of the other molecule.

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Dispersion forces

• As a result, the electron density in each electron cloud is greater in one region of the cloud.

• Two temporary dipoles form.

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Dispersion forces

• Weak dispersion forces exist between oppositely charged regions of the dipoles.

• Dispersion forces, which are the weakest intermolecular forces, are important only when no stronger forces are acting on the particles.

• Dispersion forces are noticeable between identical nonpolar molecules as the number of electrons involved increases.

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Dipole–dipole forces

• Attractions between oppositely charged regions of polar molecules are called dipole–dipole forces.

• Polar molecules have a permanent dipole and orient themselves so that oppositely charged regions match up.

• Dipole–dipole forces are stronger than dispersion forces as long as the molecules being compared are similar in mass.

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Hydrogen bonds

• A hydrogen bond is a dipole–dipole attraction that occurs between molecules containing a hydrogen atom bonded to a small, highly electronegative atom with at least one lone electron pair.

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Hydrogen bonds

• The hydrogen must be bonded to a fluorine, an oxygen, or a nitrogen atom.

• Hydrogen bonds explain why water is a liquid at room temperature, while compounds of comparable mass are gases.

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Liquids and Solids

• The kinetic-molecular theory also explains the behavior of liquids and solids.

• However, the forces of attraction between particles in liquids and solids must be considered as well as their energy of motion.

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Liquids

• Liquids conform to the shape of their container but have a fixed volume.

• The particles in a liquid maintain a fixed volume because the forces of attraction between them limit their range of motion.

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Density and compression

• The density of a liquid is much greater than that of its vapor at the same conditions.

• The higher density is due to intermolecular forces, which hold the particles together.

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Fluidity

• Fluidity is the ability to flow.

• Liquids are less fluid than gases.

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Viscosity

• A measure of the resistance of a liquid to flow is called viscosity.

• The stronger the intermolecular forces, the higher is the viscosity.

• Viscosity also increases with the mass of a liquid’s particles and the length of molecule chains.

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Surface tension

• The energy required to increase the surface area of a liquid by a given amount is called surface tension.

• Surface tension is a measure of the inward pull by particles in the interior of the liquid.

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Capillary action • The movement of a liquid up a narrow glass

tube is called capillary action, or capillarity. • Capillary action occurs when adhesive

forces are greater than cohesive forces. • Adhesion is the force of attraction between

molecules that are different, such as water molecules and the molecules of silicon dioxide in glass.

• Cohesion is the force of attraction between identical molecules, such as water molecules.

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Solids

• Strong attractive forces between the particles in a solid limit the movement of the particles to vibrations around fixed locations.

• Thus, solids have a definite shape and volume.

• Because solids are so dense, ordinary amounts of pressure will not compress them into a smaller volume.

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• A solid whose atoms, ions, or molecules are arranged in an orderly, geometric, three-dimensional structure (lattice) is called a crystalline solid.

Crystalline solids

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Crystalline solids • The individual pieces of a crystalline solid

are called crystals. • Crystalline solids are divided into five

categories based on the types of particles they contain: • atomic solids • molecular solids • covalent network solids • ionic solids • metallic solids

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Crystalline solids

• Noble gases are atomic solids whose properties reflect the weak dispersion forces between the atoms.

• Molecular solids are held together by dispersion forces, dipole–dipole forces, or hydrogen bonds.

• Elements that are able to form multiple covalent bonds, such as carbon and silicon, are able to form covalent network solids.

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• Metallic solids consist of positive metal ions surrounded by a sea of mobile electrons.

Crystalline solids

• The type of ions and the ratio of ions determine the structure of the lattice and the shape of the crystal in an ionic solid.

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Crystalline solids • Not all solids are crystalline. • The particles in an amorphous solid are not

arranged in a regular, repeating pattern and do not form crystals.

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Crystalline solids

• Examples of amorphous solids include glass, rubber, and many plastics.

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Phase Changes

• Most substances can exist in three states— solid, liquid, and gas—depending on the temperature and pressure.

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Phase Changes• States of substances are called phases when

they coexist as physically distinct parts of a mixture, such as ice water.

• When energy is added to or taken away from a system, one phase can change into another.

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temperature at which the forces holding the crystal lattice together are broken and the solid becomes a liquid.

• The melting point of a crystalline solid is the

Phase changes that require energy

• The amount of energy required to melt one mole of a solid depends on the strength of the forces keeping the particles together.

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Phase changes that require energy

• If a substance is usually a liquid at room temperature (as water is), the gas phase is called a vapor.

• Vaporization is the process by which a liquid changes into a gas or vapor.

• When vaporization occurs only at the surface of a liquid, the process is called evaporation.

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Phase changes that require energy

• Vapor pressure is the pressure exerted by a vapor over a liquid.

• As temperature increases, water molecules gain kinetic energy and vapor pressure increases.

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Phase changes that require energy

• When the vapor pressure of a liquid equals atmospheric pressure, the liquid has reached its boiling point, which is 100°C for water at sea level.

• At this point, molecules throughout the liquid have the energy to enter the gas or vapor phase.

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Phase changes that require energy

• The process by which a solid changes directly into a gas without first becoming a liquid is called sublimation.

• Solid air fresheners and dry ice are examples of solids that sublime.

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Phase changes that require energy

• At very low temperatures, ice will sublime in a short amount of time.

• This property of ice is used to preserve freeze-dried foods.

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Phase changes that release energy • Some phase changes release energy into their

surroundings. • For example, when a vapor

loses energy, it may change into a liquid.

• Condensation is the process by which a gas or vapor becomes a liquid. It is the reverse of vaporization.

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Phase changes that release energy

• Water vapor undergoes condensation when its molecules lose energy, their velocity decreases, and hydrogen bonds begin to form between them.

• When hydrogen bonds form, energy is released.

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Phase changes that release energy

• When water is placed in a freezer, heat is removed from the water.

• When enough energy has been removed, the hydrogen bonds keep the molecules frozen in set positions.

• The freezing point is the temperature at which a liquid becomes a crystalline solid.

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Phase changes that release energy

• When a substance changes from a gas or vapor directly into a solid without first becoming a liquid, the process is called deposition.

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Phase diagrams

• Temperature and pressure control the phase of a substance.

• A phase diagram is a graph of pressure versus temperature that shows in which phase a substance exists under different conditions of temperature and pressure.

• A phase diagram typically has three regions, each representing a different phase and three curves that separate each phase.

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Phase diagrams

• The points on the curves indicate conditions under which two phases coexist.

• The phase diagram for each substance is different because the normal boiling and freezing points of substances are different.

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Phase diagrams • The triple point is the point on a phase

diagram that represents the temperature and pressure at which three phases of a substance can coexist.

• All six phase changes can occur at the triple point: freezing and melting, evaporation and condensation, sublimation and deposition.

• The critical point indicates the critical pressure and the critical temperature above which a substance cannot exist as a liquid.

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Basic Assessment QuestionsBasic Assessment Questions

Question 1

Classify each crystalline solid as molecular, ionic, covalent network, or metallic.

A. NaCl

B. SiO2

C. Fe

D. H2O

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Basic Assessment QuestionsBasic Assessment Questions

Answers

A. NaCl

B. SiO2

C. Fe

ionic

covalent network

metallic

D. H2O molecular

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Classify each of the following phase changes.

Question 2

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dry ice (solid carbon dioxide) to carbon dioxide gas

sublimation

Answer 2a

Question 2a

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ice to liquid water

melting

Answer 2b

Question 2b

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liquid bromine to bromine vapor

vaporization

Answer 2c

Question 2c

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moth balls giving off a pungent odor

sublimation

Answer 2d

Question 2d

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liquid water to ice

freezing

Answer 2e

Question 2e

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water vapor to liquid water

condensation

Answer 2f

Question 2f

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Additional Concepts

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Diffusion

• The motions of particles of a gas cause them to spread out to fill the container uniformly.

• Diffusion is the process by which particles of matter fill a space because of random motion.

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Diffusion

• If you have seen dye such as food coloring spreading through a liquid, you have watched diffusion.

• Your sense of smell depends on diffusion and air currents for you to detect molecules of a gas that waft by your nose.

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Diffusion• Diffusion is slow, but in your lungs,

oxygen reaches your blood rapidly enough by diffusion.

• Oxygen diffuses across the walls of tiny blood vessels called capillaries from the air sacs of your lungs that fill with air each time you inhale.

• The rate of diffusion of a gas depends upon its kinetic energy, that is, on the mass and speed of its molecules.

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Diffusion

• The rate of diffusion depends mostly on the mass of the particles.

• Lighter particles diffuse more quickly than heavier particles.

• Because lighter particles have the same average kinetic energy as do heavier particles at the same temperature, lighter particles must have, on average, a greater velocity.

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Effusion

• Graham’s law of effusion states that the rate of effusion for a gas is inversely proportional to the square root of its molar mass.

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Effusion

• Using Graham’s law, you can also compare the rates of diffusion for two gases.

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Finding the Ratio of Diffusion Rates

• The molar mass of helium is 4.00 g/mol; the molar mass of air is 29.0 g/mol.

• What is the ratio of their diffusion rates? Which gas diffuses faster?

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Finding the Ratio of Diffusion Rates

• The ratio of the diffusion rates is 2.69. Helium diffuses about 2.7 times faster than air does.

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Gas pressure

• The pascal (Pa) is the SI unit of pressure. One pascal is equal to a force of one newton per square meter.

• Some scientists use other units of pressure. • For example, engineers use pounds per

square inch. • Barometers and manometers measure

pressure in millimeters of mercury (mm Hg).

• A unit called the torr is equal to 1 mm Hg.

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Gas pressure

• Air pressure is often reported in a unit called an atmosphere (atm).

• One atmosphere is equal to 760 mm Hg, 760 torr, or 101.3 kilopascals (kPa).

• These are all defined units; therefore, they have as many significant figures as needed when used in calculations.

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Dalton’s law of partial pressures

• Dalton found that each gas in a mixture exerts pressure independently of the other gases.

• Dalton’s law of partial pressures states that the total pressure of a mixture of gases is equal to the sum of the pressures of all the gases in the mixture, as shown below.

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Dalton’s law of partial pressures

• The portion of the total pressure (Ptotal) exerted by one of the gases is called its partial pressure (Pn).

• The partial pressure of a gas depends on the number of moles of the gas, the size of the container, and the temperature of the mixture.

• The partial pressure of one mole of any gas is the same at a given temperature and pressure.

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Finding the Partial Pressure of a Gas

• Air is made up of four main gases: N2, O2, Ar, and CO2.

• Air pressure at sea level is approximately 760 mm Hg.

• Calculate the partial pressure of oxygen, given the following partial pressures: N2, 594 mm Hg; Ar, 7.10 mm Hg; and CO2, 0.27 mm Hg.

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Finding the Partial Pressure of a Gas

• Use Dalton’s law of partial pressures to solve the problem.

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Finding the Partial Pressure of a Gas

• The partial pressure of oxygen is about 159 mm Hg.

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Additional Assessment QuestionsAdditional Assessment Questions

Calculate the ratio of diffusion rates for neon and helium. Which gas diffuses faster? About how much faster?

Question 1 Topic 12Topic 12

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He; about 2.25 times faster

Answer

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Calculate the ratio of diffusion rates for ammonia (NH3) and carbon dioxide (CO2). Which gas diffuses more rapidly?

Question 2

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1.61; NH3

Answer

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What is the partial pressure of oxygen gas in a mixture of nitrogen gas and oxygen gas with a total pressure of 0.48 atm if the partial pressure of nitrogen gas is 0.24 atm?

Question 3

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0.24 atm

Answer

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Find the total pressure of a mixture that contains three gases with the following partial pressures: 6.6 kPa, 3.2 kPa, and 1.2 kPa.

Question 4

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11.0 kPa

Answer

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