chapters 13 & 17 phases and heat. phases of matter chapter 13

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Chapters 13 & 17 Phases and Heat

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Page 1: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Chapters 13 & 17

Phases and Heat

Page 2: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Phases of Matter

Chapter 13

Page 3: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Phases

There are three phases, or states, that we will discuss

Solid Liquid Gas

Page 4: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Solids

form of matter that has a definite shape and definite volume.

Use (s) to denote solids in chemical reactions

Page 5: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Solids

In most solids the atoms, ions, or molecules are packed tightly together

The particles in solids tend to vibrate around fixed points

When you heat a solid, its particles vibrate more rapidly, eventually the solid breaks down and melts.

Page 6: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Types of Solids

Crystalline Solids In a crystal the particles are arranged in

an orderly, repeating, three-dimensional pattern called a crystal lattice. There are many different shapes of crystalline solids, pg 397

Page 7: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Types of Solids

Non-Crystalline Solids Amorphous solids lack an orderly internal

structure. Ex – Rubber, plastic, and asphalt.

Glass – transparent fusion product of inorganic substances that have cooled to a rigid state without crystallizing. Sometimes called super-cooled liquids.

Page 8: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13
Page 9: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Allotropes

Two or more different molecular forms of the same element in the same physical state Different properties because they have

different structures

Page 10: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Allotropes of Carbon

Page 11: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Liquids

form of matter that has a definite volume, indefinite shape, and flows.

Use (l) to denote liquids in chemical reactions

Page 12: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Liquids

In liquids the atoms or molecules are able to slide past each other.

In liquids there are intermolecular attractions between the atoms or molecules, which determine the liquid’s physical properties.

When you heat a liquid the particles vibrate more rapidly and start moving past each other faster.

Page 13: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Gases

form of matter that takes both the shape and volume of its container

Use (g) to denote gases in chemical reactions

Page 14: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Phase Changes

Six Changes Solid Liquid Melting Liquid Solid Freezing Liquid Gas Vaporization Gas Liquid Condensation Solid Gas Sublimation Gas Solid Deposition

Page 15: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Phase Changes

During any given phase change, both phases can exist together in equilibrium

Example At 0°C, water can exist in both the liquid

and solid phases in equilibrium

Page 16: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Energy

When energy is added to a reaction, or phase change, it is called Endothermic

When energy is released during a reaction, or phase change, it is called Exothermic

Page 17: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Phase Changes

Which phase changes are endothermic, requiring the addition of energy?

Melting Vaporization Sublimation

Page 18: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Phase Changes

Which phase changes are exothermic, releasing energy?

Freezing Condensation Deposition

Page 19: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13
Page 20: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Phase Diagram of CO2

Page 21: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13
Page 22: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Energy

What is energy? Capacity to do work Ability to do work

Two main types Kinetic Potential

Page 23: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Types of Energy

Kinetic Energy Energy of motion Related to the speed and mass of

molecules

Potential Energy Stored energy

Page 24: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Temperature

How is energy related to Temperature?

What happens to the temperature of a substance when you add energy? Particles move faster Temperature increases

Page 25: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Temperature

Relationship between energy, particle speed, and temperature

Temperature Definition Average Kinetic Energy

Page 26: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Temperature Scales

Kelvin (K) and Celsius (°C) scales Kelvin scale is called the absolute

scale Related to the kinetic energy of a

substance Celsius scale is a relative scale

based on the boiling and freezing points of water

Page 27: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Temperature Conversion

K = °C + 273

Page 28: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Pressure

What is pressure?

Physics – Force per unit area

Chemistry – related to the number of collisions between particles and container walls

Page 29: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Pressure Conversion

1 atm = 101.3 kPa

Page 30: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Vapor Pressure

Pressure exerted by vapor that has evaporated and remains above a liquid

Related to temperature As temperature increases, vapor

pressure increases

Page 31: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Boiling vs. Evaporation

Boiling Vapor pressure equals external, or

atmospheric pressure

Evaporation Some molecules gain enough energy to

escape the liquid phase At temp. less than boiling point

Page 32: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Normal Boiling Point

Boiling Point at Standard Pressure

1 atm or 101.3 kPa

Page 33: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Evaporation

Why is evaporation considered a cooling process?

As the molecules with higher kinetic energy evaporate, the average kinetic energy of the substance decreases

Page 34: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Table H

Shows the relationship between temperature and vapor pressure for four specific substances

Page 35: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13
Page 36: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13
Page 37: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Thermochemistry

Chapter 17

Page 38: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Thermochemistry

Heat involved with chemical reactions and phase changes

Page 39: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Heat

Energy transferred from one object to another, usually because of a temperature difference

Measured in Joules (J) or calories (cal)

Heat flows from hot to cold

Page 40: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Heat Transfer

Endothermic Energy being added

Exothermic Energy being released

Page 41: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Specific Heat Capacity

Amount of heat needed to raise the temperature of 1 g of a substance by 1°C Unique for each phase of each substance

4.18 J/(g*°C) for liquid water Listed in Table B of Reference Tables

Page 42: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Heat

What factors affect the amount of heat transferred?

Specific Heat Capacity Mass Temperature difference between objects

Page 43: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Heat Equation

Heat, Q Mass, m Specific Heat Capacity, c Change in Temperature, ΔT

Q=m*c*ΔT

Page 44: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Example

200g of water is heated from 20°C to 40°C, how much heat is needed?

Q = m*c*ΔT Q = (200g) * (4.18J/g°C) * (20°C) Q = 16720 J

Page 45: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Example

How much energy is required to raise the temperature of 50g of water from 5°C to 50°C?

Q = m*c*ΔT Q = (50g) * (4.18J/g°C) * (45°C) Q = 9405 J

Page 46: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Another Example

What is the Specific Heat Capacity of Fe, if it takes 180J of energy to raise 10g of Fe from 10°C to 50°C?

Q = m*c*ΔT 180J = (10g) * c * (40°C) c = 0.45 J/(g*°C)

Page 47: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13
Page 48: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Phase Change

At what temperature does ice melt? 0°C

At what temperature does water freeze? 0°C

Melting point and freezing point are the same

Page 49: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Phase Change

What happens to temperature during phase changes? Temperature remains constant

Temperature remains CONSTANT during a phase change

Page 50: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Phase Change

If energy is being added, what kind of energy is it? Energy being added is potential energy,

not kinetic energy Potential energy is being used to

separate or spread the particles apart

Page 51: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Heat of Vaporization, Hv

Amount of energy needed to vaporize 1g of a substance

Water = 2260 J/g

Q=mHvUse for Liquid Gas orGas Liquid

Page 52: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Heat of Fusion, Hf

Amount of energy needed to melt 1g of a substance

Water = 334 J/g

Q=mHfUse for Solid Liquid orLiquid Solid

Page 53: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Examples

How much energy is needed to melt 10g of ice at 0°C? Q = m*Hf

Q = (10g) * (334J/g) Q = 3340 J

Page 54: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Example

How much energy is needed to vaporize 10g of water at 100°C? Q = m*Hv

Q = (10g) * (2260J/g) Q = 22600 J

Page 55: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Phase Change

Which requires more energy melting or vaporization? Vaporization

Why? Molecules are spread farther apart as a

gas It takes more energy to get gas particles

spread apart

Page 56: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13
Page 57: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Heating (Cooling) Curves

Shows relationship between temperature and time during constant heating or cooling.

Also shows phases, and the phase changes between them.

Page 58: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Heating Curves

Diagonal lines are phases Horizontal lines are phase changes

Time (s)

Tem

p (˚

C)

Gas

Liquid

Solid

Page 59: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Heating Curves

Diagonal lines are phases Horizontal lines are phase changes

Time (s)

Tem

p (˚

C)

VaporizationCondensation

MeltingFreezing

Page 60: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13
Page 61: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Conservation of Energy

Energy can not be created or destroyed, only transferred or converted from one form to another.

Energy lost by one object must be gained by another object or the environment Qlost = Qgained

Page 62: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Example

A chunk of iron at 80°C is dropped into a bucket of water at 20°C.

What direction will heat flow? From the iron to the water Hot to cold

Page 63: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Example

A chunk of iron at 80°C is dropped into a bucket of water at 20°C.

What could be the final temperature, when they both come to equilibrium? Between 20°C and 80°C

Page 64: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Example

A 100g block of aluminum, c=0.90J/g*°C at 100°C is placed into 50g of water at 20°C, what will be the final temperature when the aluminum and water reach equilibrium? Qlost = Qgained

m*c*ΔT = m*c*ΔT 100g*0.90J/g°C*(100°C-Tf) = 50g*4.18J/g°C*(Tf-20°C) 90*(100-Tf) = 209*(Tf-20) 9000-90Tf = 209Tf-4180 13180 = 299Tf

Tf = 44°C

Page 65: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Conservation of Energy

SystemEnergy In Work Done (Energy)

Energy Out

Page 66: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Conservation of Energy

Energy In Work Done (Energy)

Energy Out

Page 67: Chapters 13 & 17 Phases and Heat. Phases of Matter Chapter 13

Conservation of Energy

Food In Metabolism

Waste Out