chapter 13 lecture

103
Water exists on Earth as a liquid, a solid, and a vapor. As water cycles through the atmosphere, the oceans, and Earth’s crust, it undergoes repeated changes of state. You will learn what conditions can control the state of a substance. BELLWORK-name the following phase changes : a)Solid to liquid b) liquid to solid c)Liquid to gas d) gas to liquid e) Solid to gas Bellwork -State Changes

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Page 1: Chapter 13 Lecture

Water exists on Earth as a liquid, a solid, and a vapor. As water cycles through the atmosphere, the oceans, and Earth’s crust, it undergoes repeated changes of state. You will learn what conditions can control the state of a substance.

BELLWORK-name thefollowing phase changes:a)Solid to liquid b) liquid to solidc)Liquid to gas d) gas to liquide) Solid to gas

Bellwork -State Changes

Page 2: Chapter 13 Lecture

Melting - solid to liquid

Freezing- liquid to solid

Vaporization- liquid to gas

Vapor- a gas that is usually a liquid at room temp

Condensation- changing from a gas to a liquid

Page 3: Chapter 13 Lecture

Chapter 13- States of MatterIntro to Gases

The skunk releases its spray! Within seconds you smell that all-too-familiar foul odor. You will discover some general characteristics of gases that help explain how odors travel through the air, even on a windless day.

Page 4: Chapter 13 Lecture

The Kinetic Molecular Theory explains the behavior of gases.

13.1

Page 5: Chapter 13 Lecture
Page 6: Chapter 13 Lecture

The word kinetic refers to motion.

Page 7: Chapter 13 Lecture

The word kinetic refers to motion.

•The energy an object has because of its motion is called kinetic energy.

Page 8: Chapter 13 Lecture

The word kinetic refers to motion.

•The energy an object has because of its motion is called kinetic energy.

•According to the kinetic theory, all matter consists of tiny particles that are in constant motion.

Page 9: Chapter 13 Lecture

Kinetic Molecular Theory: GASES

Page 10: Chapter 13 Lecture

Kinetic Molecular Theory: GASES

•The particles in a gas are small, hard spheres with an insignificant volume.

Page 11: Chapter 13 Lecture

Kinetic Molecular Theory: GASES

•The particles in a gas are small, hard spheres with an insignificant volume.

•The motion of gas particles is rapid, constant, and random.

Page 12: Chapter 13 Lecture

Kinetic Molecular Theory: GASES

•The particles in a gas are small, hard spheres with an insignificant volume.

•The motion of gas particles is rapid, constant, and random.

•All collisions between gas particles are perfectly elastic (no energy lost).

Page 13: Chapter 13 Lecture

Gas particles are in rapid, constant motion.

13.1

Page 14: Chapter 13 Lecture

Gas particles travel in straight-line paths.

Gas particles move randomly.

13.1

Page 15: Chapter 13 Lecture

A gas fills its container.

13.1

Page 16: Chapter 13 Lecture

Kinetic theory explains gas pressure.13.1

Page 17: Chapter 13 Lecture

Pressure = Force/AreaA force is a push or a pull.

13.1

more area

less area

more pressure!

Same force

Page 18: Chapter 13 Lecture
Page 19: Chapter 13 Lecture

Which would you prefer? Why?

Page 20: Chapter 13 Lecture

Kinetic theory explains gas pressure.13.1

Page 21: Chapter 13 Lecture

Kinetic theory explains gas pressure.13.1

Gas pressure is the force exerted by gas particles hitting the surface of an object.

Page 23: Chapter 13 Lecture
Page 24: Chapter 13 Lecture

An empty space with no particles and no pressure is called a vacuum.

Page 25: Chapter 13 Lecture

Atmospheric pressure is the pressure created by the earth’s gravitational pull on the gases in our atmosphere.

Page 26: Chapter 13 Lecture

Gas pressure is exerted in all directions.

Page 27: Chapter 13 Lecture

A barometer is a device that is used to measure atmospheric pressure.

Page 28: Chapter 13 Lecture

An empty water bottle, closed tightly at high elevation, will be crushed by the atmosphere at sea level.

Pressure Poem

Page 29: Chapter 13 Lecture

Units of Pressure

•The SI unit of pressure is the pascal (Pa).

•One standard atmosphere (atm) is the atmospheric pressure at sea level.

13.1

Page 30: Chapter 13 Lecture

13.1

Page 31: Chapter 13 Lecture

13.1

450 kPa x

Page 32: Chapter 13 Lecture

13.1

450 kPa x kPa

Page 33: Chapter 13 Lecture

13.1

450 kPa x kPaatm

Page 34: Chapter 13 Lecture

13.1

450 kPa x kPaatm 1

101.3

Page 35: Chapter 13 Lecture

13.1

450 kPa x kPaatm 1

101.3 = 4.4 atm

Page 36: Chapter 13 Lecture

13.1

450 kPa x kPaatm 1

101.3

450 kPa x

= 4.4 atm

Page 37: Chapter 13 Lecture

13.1

450 kPa x kPaatm 1

101.3

450 kPa x kPa

= 4.4 atm

Page 38: Chapter 13 Lecture

13.1

450 kPa x kPaatm 1

101.3

450 kPa x kPamm Hg

= 4.4 atm

Page 39: Chapter 13 Lecture

13.1

450 kPa x kPaatm 1

101.3

450 kPa x kPa760 101.3

mm Hg

= 4.4 atm

Page 40: Chapter 13 Lecture

13.1

450 kPa x kPaatm 1

101.3

450 kPa x kPa760 101.3

mm Hg

= 4.4 atm

= 3400mm Hg

Page 41: Chapter 13 Lecture

for Sample Problem 13.1

Page 42: Chapter 13 Lecture

Particles at a given temperature have a wide range of kinetic energies. Most of the particles have kinetic energies in the middle of this range.

Page 43: Chapter 13 Lecture

Particles at a given temperature have a wide range of kinetic energies. Most of the particles have kinetic energies in the middle of this range.

Page 44: Chapter 13 Lecture

Particles at a given temperature have a wide range of kinetic energies. Most of the particles have kinetic energies in the middle of this range.

Temperature measures Average Kinetic Energy

Page 45: Chapter 13 Lecture

The Kelvin temperature of a substance is directly proportional to average kinetic energy.

13.1

Page 46: Chapter 13 Lecture

The Kelvin temperature of a substance is directly proportional to average kinetic energy.

13.1

The higher the kinetic energy, the higher the temperature.

Page 47: Chapter 13 Lecture

Two substances with the same average kinetic energy are at the same temperature.

Two substances at the same temperature have the same average kinetic energy.

13.1

Page 48: Chapter 13 Lecture

Absolute zero (0 K, or –273.15°C) is the temperature at which the motion of particles theoretically stops.

13.1

Page 49: Chapter 13 Lecture

Absolute zero (0 K, or –273.15°C) is the temperature at which the motion of particles theoretically stops.

•Particles would have no kinetic energy at absolute zero.

13.1

Page 50: Chapter 13 Lecture

Absolute zero (0 K, or –273.15°C) is the temperature at which the motion of particles theoretically stops.

•Particles would have no kinetic energy at absolute zero.

•Absolute zero has never been produced in the laboratory (and not for lack of trying!).

13.1

Page 51: Chapter 13 Lecture

Bellwork- Kinetic Energy

•What is kinetic energy?•How is average kinetic energy related to temperature?•Which has higher kinetic energy, an olympic size pool of water or a cup of hot coffee?

Page 52: Chapter 13 Lecture

Substances that can flow are referred to as fluids. Both liquids and gases are fluids.

13.2

Page 53: Chapter 13 Lecture

The intermolecular attractions (IMFs) are counteracted by motion of molecules. Together they determine the physical properties of liquids.

High IMFs promote a solid state

High temps (motion) promote a gas state.

13.2

Page 54: Chapter 13 Lecture

13.2

If the liquid is not boiling it is called evaporation.

Page 55: Chapter 13 Lecture

When a liquid converts to a gas it is called

vaporization.

13.2

If the liquid is not boiling it is called evaporation.

Page 56: Chapter 13 Lecture

When a liquid converts to a gas it is called

vaporization.

13.2

If the liquid is not boiling it is called evaporation.

Page 57: Chapter 13 Lecture

When a liquid converts to a gas it is called

vaporization.

13.2

If the liquid is not boiling it is called evaporation.

Page 58: Chapter 13 Lecture

In a closed container, evaporated molecules collect as a vapor above any liquid.Vapor pressure is the force exerted by a gas above a liquid.

13.2

Page 59: Chapter 13 Lecture

During evaporation, only molecules with a certain minimum kinetic energy can escape from the surface of the liquid.

Page 60: Chapter 13 Lecture

During evaporation, only molecules with a certain minimum kinetic energy can escape from the surface of the liquid.

Page 61: Chapter 13 Lecture

During evaporation, only molecules with a certain minimum kinetic energy can escape from the surface of the liquid.

Evaporation is a cooling process because the molecules with the highest kinetic energy escape.

Page 62: Chapter 13 Lecture

13.2

In an open container, molecules that evaporate can escape from the container.

Page 63: Chapter 13 Lecture

Some evaporated molecules will condense back into a liquid.

Page 64: Chapter 13 Lecture

Some evaporated molecules will condense back into a liquid.

Page 65: Chapter 13 Lecture

Some evaporated molecules will condense back into a liquid.

A dynamic equilibrium exists between the vapor and the liquid.

The system is in equilibrium when the rate of evaporation equals the rate of condensation.

Page 66: Chapter 13 Lecture
Page 67: Chapter 13 Lecture

DYNAMIC EQUILIBRIUM

Page 68: Chapter 13 Lecture

DYNAMIC EQUILIBRIUM

For each molecule that evaporates a different molecule returns to the liquid.

Page 69: Chapter 13 Lecture

DYNAMIC EQUILIBRIUM

For each molecule that evaporates a different molecule returns to the liquid.

SAME RATES!!

Page 70: Chapter 13 Lecture
Page 71: Chapter 13 Lecture

DYNAMIC EQUILIBRIUM

Page 72: Chapter 13 Lecture

DYNAMIC EQUILIBRIUMEquilibrium- The amount of liquid and vapor do not change.

Page 73: Chapter 13 Lecture

DYNAMIC EQUILIBRIUMEquilibrium- The amount of liquid and vapor do not change.Dynamic- There is a constant turnover of particles.

Page 74: Chapter 13 Lecture

Vapor pressure increases with Temperature.

13.2

Page 75: Chapter 13 Lecture
Page 76: Chapter 13 Lecture

The particles have increased kinetic energy, so more particles will have the minimum energy needed to escape the liquid.

Page 77: Chapter 13 Lecture

When a liquid is heated to a temperature at which particles throughout the liquid have enough kinetic energy to vaporize, the liquid begins to boil.

Page 78: Chapter 13 Lecture

Liquids boil when their vapor pressure exceeds the pressure pushing down on the liquid (usually atmospheric pressure).

Page 79: Chapter 13 Lecture

13.2

Page 80: Chapter 13 Lecture
Page 81: Chapter 13 Lecture

Boiling Point and Pressure Changes

Page 82: Chapter 13 Lecture

Boiling Point and Pressure ChangesBecause a liquid boils when its vapor pressure is equal to the external pressure, liquids don’t always boil at the same temperature.

Page 83: Chapter 13 Lecture

Boiling Point and Pressure ChangesBecause a liquid boils when its vapor pressure is equal to the external pressure, liquids don’t always boil at the same temperature.

•At high altitudes, atmospheric

pressure is low, so water boils cooler and food needs longer to cook.

Page 84: Chapter 13 Lecture

Boiling Point and Pressure ChangesBecause a liquid boils when its vapor pressure is equal to the external pressure, liquids don’t always boil at the same temperature.

•At high altitudes, atmospheric

pressure is low, so water boils cooler and food needs longer to cook.

• A pressure cooker increases the

boiling point so food cooks fast.

Page 85: Chapter 13 Lecture

Altitude and Boiling Point

Page 86: Chapter 13 Lecture

The normal boiling point is the boiling point of a liquid at atmospheric pressure (1 atm or 101.3 kPa)

Page 87: Chapter 13 Lecture
Page 88: Chapter 13 Lecture

Section 13.3- Solids

Page 89: Chapter 13 Lecture

Solids keep their shape because their particles are in fixed positions.

Page 90: Chapter 13 Lecture

In a crystalline solid, the particles are in an orderly, repeating, three-dimensional pattern called a crystal lattice.

elemental metalionic compound

Page 91: Chapter 13 Lecture

When an element can make more than one structure, the different forms are called allotropes.

13.3

Page 92: Chapter 13 Lecture

When an element can make more than one structure, the different forms are called allotropes.

•Allotropes have different properties because their structures are different.

13.3

Page 93: Chapter 13 Lecture

When an element can make more than one structure, the different forms are called allotropes.

•Allotropes have different properties because their structures are different.

•Only a few elements have allotropes.

13.3

Page 94: Chapter 13 Lecture

Carbon’s allotropes are diamond and graphite

13.3

Page 95: Chapter 13 Lecture

Non-Crystalline SolidsAn amorphous solid lacks an ordered internal structure.•Rubber, plastic, asphalt, and glass are amorphous solids.

Page 96: Chapter 13 Lecture

Non-Crystalline SolidsAn amorphous solid lacks an ordered internal structure.•Rubber, plastic, asphalt, and glass are amorphous solids.

Page 97: Chapter 13 Lecture

Quartz is crystallized SiO2 Glass is amorphous SiO2

Page 98: Chapter 13 Lecture

Non-Crystalline Solids

Quartz is crystallized SiO2 Glass is amorphous SiO2

Page 99: Chapter 13 Lecture

Non-Crystalline SolidsAn amorphous solid lacks an ordered internal structure.

Quartz is crystallized SiO2 Glass is amorphous SiO2

Page 100: Chapter 13 Lecture

Non-Crystalline SolidsAn amorphous solid lacks an ordered internal structure.•A glass has cooled to a rigid state without crystallizing.

Quartz is crystallized SiO2 Glass is amorphous SiO2

Page 101: Chapter 13 Lecture

13.4

Page 102: Chapter 13 Lecture

The change of a substance from a solid to a vapor without passing through the liquid state is called sublimation.

Sublimation occurs in solids with vapor pressures that exceed atmospheric pressure at or near room temperature.

13.4

Page 103: Chapter 13 Lecture

The change of a substance from a solid to a vapor without passing through the liquid state is called sublimation.

Sublimation occurs in solids with vapor pressures that exceed atmospheric pressure at or near room temperature.

13.4