12
1 © 2008 Brooks/Cole 1 Chapter 11: Liquids, Solids and Materials Chemistry: The Molecular Science Moore, Stanitski and Jurs © 2008 Brooks/Cole 2 The Liquid State A liquid forms when a gas condenses. This occurs at low T (and/or high P). Average intermolecular attraction > average E k . Molecules are close together and in constant motion They have a distribution of speeds (and E k ) A few have enough E k to slide past each other. © 2008 Brooks/Cole 3 Liquids are very hard to compress Molecules are close together and resist moving closer. Used as hydraulic fluids to transmit pressure. The Liquid State Viscosity = Resistance to flow. High viscosity = slow flow. low viscosity: water, ethanol, gasoline… high viscosity: honey, corn syrup … © 2008 Brooks/Cole 4 High viscosity is caused by: Large intermolecular attractions. Large entanglement of molecules. Higher T = lower viscosity E k > E barrier required to move past another molecule. • Increase T = increase average E k . More molecules have E k > E barrier The Liquid State © 2008 Brooks/Cole 5 Liquid molecules attract each other. Surface molecules experience unbalanced forces. They are not as well stabilized. Smaller surface area higher stability. The Liquid State © 2008 Brooks/Cole 6 Raindrops are spherical (surface/V ratio minimized). Surface tension = E required to form a flat surface. Substance Formula Surface Tension J/m 2 at 20°C Octane C 8 H 18 2.16 x 10 -2 Ethanol C 2 H 5 OH 2.23 x 10 -2 Chloroform CHCl 3 2.68 x 10 -2 Benzene C 6 H 6 2.85 x 10 -2 Water H 2 O 7.29 x 10 -2 Mercury Hg 46. x 10 -2 The Liquid State

The Liquid State © 2008 Brooks/Cole 1 Chapter 11: Liquids, Solids and Materials Chemistry: The Molecular Science Moore, Stanitski and Jurs © 2008 Brooks/Cole 2Published in: American

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1

© 2008 Brooks/Cole 1

Chapter 11: Liquids, Solids and Materials

Chemistry: The Molecular ScienceMoore, Stanitski and Jurs

© 2008 Brooks/Cole 2

The Liquid State

A liquid forms when a gas condenses.

• This occurs at low T (and/or high P).

• Average intermolecular attraction > average Ek.

Molecules are close together and in constant motion

They have a distribution of speeds (and Ek)

A few have enough Ek to slide past each other.

© 2008 Brooks/Cole 3

Liquids are very hard to compress

• Molecules are close together and resist movingcloser.

• Used as hydraulic fluids to transmit pressure.

The Liquid State

Viscosity = Resistance to flow.

• High viscosity = slow flow.

low viscosity: water, ethanol, gasoline…

high viscosity: honey, corn syrup …

© 2008 Brooks/Cole 4

High viscosity is caused by:

• Large intermolecular attractions.

• Large entanglement of molecules.

Higher T = lower viscosity

• Ek > Ebarrier required to move past another molecule.

• Increase T = increase average Ek.

More molecules have Ek > Ebarrier

The Liquid State

© 2008 Brooks/Cole 5

Liquid molecules attract each other.

Surface molecules experience unbalanced forces.

They are not as well stabilized.

Smaller surface area higher stability.

The Liquid State

© 2008 Brooks/Cole 6

Raindrops are spherical (surface/V ratio minimized).

Surface tension = E required to form a flat surface.

Substance Formula Surface Tension

J/m2 at 20°C

Octane C8H18 2.16 x 10-2

Ethanol C2H5OH 2.23 x 10-2

Chloroform CHCl3 2.68 x 10-2

Benzene C6H6 2.85 x 10-2

Water H2O 7.29 x 10-2

Mercury Hg 46. x 10-2

The Liquid State

2

© 2008 Brooks/Cole 7

Why don’t all liquids form spheres in all cases?

It’s a balancing act …

Gravity pulls down (giving a puddle).

Surface tension contracts (into a sphere).

The “winner” depends on the amount of liquid and

any surface/liquid attractions. A drop of water:

puddles on a dirty surface

“beads” on a waxy surface

The Liquid State

© 2008 Brooks/Cole 8

Capillary action

A competition between:

• Adhesion: forces between a surface and a liquid.

• Cohesion: forces between liquid molecules.

The shape of the meniscus illustrates the relative

strength of the adhesive and cohesive forces

The Liquid State

© 2008 Brooks/Cole 9

The Liquid State

© 2008 Brooks/Cole 10

Volatility = tendency of a liquid to vaporize.

low T

velocity or energy

num

ber

of m

ole

cule

s

Threshold

for

escape

high T

Volatility increases with increased T.

Increase T = increase Ek = more can escape.

Vapor Pressure

© 2008 Brooks/Cole 11

If a liquid container is:

Open – the liquid can evaporate completely.

Closed – the liquid evaporates but cannot disperse.

Vaporized molecules can condense.

• more vapor = faster condensation

At some time:

evaporation rate = condensation rate.

P increases but reaches a maximum.

Vapor Pressure

© 2008 Brooks/Cole 12

Vapor Pressure

Equilibrium vapor pressure is independent of the

volume or surface area of the liquid

A liquid boils when the vapor P = atmospheric P

• Vaporization occurs throughout the liquid.

• Bubbles of pure vapor form and rise to the surface.

3

© 2008 Brooks/Cole 13

The normal bp occurs at 1 atm = 760 mmHg.

Boiling Point

Boiling points (bp) vary with pressure.

Norm

al bp =

78.5

°C

ethanol Water boils

at 100°C

at sea level

1 atm

Norm

al bp

-40 -20 0 20 40 60 80 100 120

Temperature, °C

Va

po

r p

ressu

re,

mm

Hg

1000

500

0

H 2O

diethyl ether

bp =

34.6

°CSalt Lake City (4400 ft) P=650 mmHg

Water boils at 95°C

in Salt Lake City

© 2008 Brooks/Cole 14

Clausius-Clapeyron Equation

The relationship between vapor pressure and T:

ln = – –P2

P1

Hvap

R

1

T2

1

T1

Ethanol

NOTE: Absolute T must be used.

Plot ln P versus 1/T

slope = – Hvap

R

© 2008 Brooks/Cole 15

Clausius-Clapeyron Equation

The normal bp of water = 100°C and Hvap = 40.71

kJ/mol. At what T will water boil if P = 500 Torr?

ln = – P2

P1

1

T2

1

T1

- Hvap

R

ln = – 500

760

1

3731

T2

- 40710 J g-1

8.315 J K-1mol-1

- 0.4187 = - 4896.3 - 2.681 x 10-31

T2

T2 = 361 K = 88 °C

© 2008 Brooks/Cole 16

Phase Changes: Solids, Liquids & Gases

Vaporizationlow T

velocity or energy

num

ber

of m

ole

cule

s

Threshold

for

escape

high T

• High Ek molecules leave.

• The average Ek of the liquid drops.

• The liquid cools.

Vaporization is endothermic

Condensation

The reverse process is exothermic

© 2008 Brooks/Cole 17

Phase Changes

H°vap = – H°cond

Molar heat of vaporization, H°vap

Heat required to vaporize 1 mol (P = 1 bar).

Molar heat of condensation, H°cond

Heat released when 1 mol condenses (P = 1 bar).

For H2O(l) H2O(g) H° = H°vap = +40.7

kJ/molFor H2O(g) H2O(l) H° = H°cond = -40.7 kJ/mol

© 2008 Brooks/Cole 18

Melting and FreezingThe molecules in a solid are closely packed and in

constant motion. They

vibrate about fixed positions

do not have enough E to slide past each other.

A solid melts when

• Ek > forces holding the particles in their fixed

positions.

Melting is endothermic.

Freezing (solidification, crystallization) is exothermic.

4

© 2008 Brooks/Cole 19

Phase Changes

H°fus = – H°cryst

Molar heat of crystallization, H°cryst

Heat released when 1 mol crystallizes (P = 1 bar).

For H2O(s) H2O(l) H° = H°fus = +6.02 kJ/mol

For H2O(l) H2O(s) H° = H°cryst = -6.02 kJ/mol

Normal melting or freezing occurs at P = 1 atm

Molar heat of fusion, H°fus

Heat required to melt 1 mol (P = 1 bar).

© 2008 Brooks/Cole 20

Phase Changes

Sublimation – the direct conversion of a solid to a gas

Examples

Solid CO2 (dry ice) sublimes.

Ice (v.p. = 4.6 mmHg @ 0°C) in a frost-free ‘fridge is removed

by blowing dry air over it…

Deposition is the reverse process: (g) (s)

Example: plating Al onto the surface of a CD

H°sub = – H°dep

© 2008 Brooks/Cole 21

Phase Changes

endothermic

process

(heat added)

exothermic

process

(heat released)

© 2008 Brooks/Cole 22

Phase Changes

Substance mp(°C) Hfus(kJ/mol) bp(°C) Hvap(kJ/mol)

O2 (16 e-) –248 0.445 –183.0 6.8

F2 (18 e-) –220 1.020 –188.1 6.54

Cl2 (34 e-) –103 6.406 –34.6 20.39

Br2 (70 e-) –7.2 10.794 59.6 29.54

Nonpolar molecules

London forces increase as the number of e- increase.

The data support this trend…

© 2008 Brooks/Cole 23

Phase Changes

Substance mp(°C) Hfus(kJ/mol)* bp(°C) Hvap(kJ/mol)*

SO2 (32 e-) –76 7.4 –10.0 24.9

HCl (18 e-) –115 2.0 –85.1 16.2

HBr (36 e-) –87 2.4 –66.8 17.6

H2O (10 e-) 0 6.0 +100.0 40.7

HF (10 e-) –83 4.6 +19.5 7.5

NH3 (10 e-) –78 5.6 –33.5 23.4

Polar molecules

More difficult to explore trends.

Values depend on London, dipole forces and H-bonding.

*At the normal phase-transition temperature (Air Liquide Gas Encyclopedia)

© 2008 Brooks/Cole 24

Phase Changes

Substance mp(°C) Hfus(kJ/mol)

NaCl 800 30.21

NaBr 747 25.69

NaI 662 21.95

Ionic solids

All Na+ ions / halide ion (-1 charge) compounds.

They only differ in halide size: I- > Br- > Cl-

Larger ion further apart weaker attraction

5

© 2008 Brooks/Cole 25

Heating Curve

Convert 100 g of ice at -20°C into vapor at 120°C.

© 2008 Brooks/Cole 26

TOTAL heat required = 308.9 kJ

Heat the ice to 0°C.

H = mc T = (100g)(2.06 Jg-1°C-1)(0-[-20]°C) = 4.1 kJ

Convert the ice to water

H = n Hfus = (100g/18.02g mol-1)(6.020 kJ/mol) = 33.4 kJ

Heat the water from 0°C to 100°C.

H = mc T = (100g)(4.184 Jg-1°C-1)(100 - 0°C) = 41.8 kJ

Convert water to steam (at its normal bp).

H = n Hvap = (100g/18.02 g mol-1)(40.7 kJ/mol) = 225.9 kJ

Heat steam from 100 to 120°C.

H = mc T = (100g)(1.84 Jg-1°C-1)(120 - 100°C) = 3.7 kJ

Heating Curve

© 2008 Brooks/Cole 27

Pre

ssu

re (

atm

)

Temperature (°C)

Phase Diagrams

Solid Liquid

Gas

critical point

triple pointsublimation

deposition

freezing

melting

condensation

vaporization

Melting point

curve

Vapor-pressure

curve

Supercritical

fluid

© 2008 Brooks/Cole 28

Phase Diagrams

Triple point

Three phases in equilibrium. T and P are fixed.

Water T = 0.01°C, P = 4.58 mmHg

CO2 T = -57°C, P = 5.2 atm

Critical point

The end of the liquid/gas equilibrium line. It occurs at

the critical temperature, Tc and critical pressure, Pc

Water Tc = 374°C, Pc = 218 atm

CO2 Tc = 31°C, Pc = 73 atm

Above Tc a gas cannot be liquefied (at any P)

© 2008 Brooks/Cole 29

Supercritical CO2 is an important solvent. It is used:

Above Tc and Pc the substance is neither a liquid nor

a gas. It is a supercritical fluid.

It has:

• to extract caffeine from coffee beans

• as a dry-cleaning fluid

• a density characteristic of a liquid.

• flow properties of a gas.

Critical Temperature and Pressure

© 2008 Brooks/Cole 30

Water Phase Diagram

For most materials, the solid/liquid line has a positive slope.

Water is unusual. Ice can be melted by increased P !

4.58

Solid Liquid Gas

Pre

ssu

re (

mm

Hg

)

Temperature (°C)0 0.01 100

760

triple point

normal fp normal bp

6

© 2008 Brooks/Cole 31

Physical Comparison with Importance in

Property Other Substances and Biological Environment

Specific heat capacity Highest of all liquids and Moderates T in the environment and in

(4.18 J g-1 °C-1) solids except NH3 organisms; climate affected by

movement of water (e.g., Gulf Stream)

Heat of fusion Highest of all molecular Freezing water releases large quantity

(333 J/g) solids except NH3 of thermal E; used to save crops from

freezing by spraying them with liq. water

Heat of vaporization Highest of all molecular Condensation of water vapor in clouds

(2250 J/g) substances releases large quantities of thermal E

fueling storms

Surface tension Highest of all molecular Contributes to capillary action in plants

(7.3 x 10-2 J/m2) liquids causes formation of spherical droplets;

supports insects on water surfaces

Thermal conductivity Highest of all molecular Aids heat transfer in organisms;

(0.6 J s-1 m-1 °C-1) liquids rapidly cools organisms immersed in

cold water, causing hypothermia

Table 11.4 Unusual Properties of Water

Water: A Liquid with Unusual Properties

© 2008 Brooks/Cole 32

Most liquids: Lower T = higher density.

Most materials: dsolid > dliquid

Not water! In winter:

• Surface water cools & sinks until T=4°C.

• Water (T < 4°C) floats on the 4°C layer.

• The top layer cools to 0°C.

• Water freezes “top-down”.

• Ice floats on water, insulating the water below it.

These facts allow aquatic life to survive at low T.

Water: A Liquid with Unusual Properties

© 2008 Brooks/Cole 33

Water: A Liquid with Unusual Properties

© 2008 Brooks/Cole 34

Types of Solids

Ionic (ionic bonding)

• Hard, brittle, high mp. Some are water soluble.

Metallic (metallic bonding)

• Malleable, ductile, good heat/electrical conduction, wide

range of hardness and mp (Pt, Fe, Pb, Hg …)

Molecular (London forces, dipole/dipole forces, and H-bonds)

• Low to moderate mp/bp, soft, poor conductors.

Network (covalent bonds; atoms in infinite arrays)

• Wide range of properties (diamond, graphite, mica …)

© 2008 Brooks/Cole 35

Types of Solids

Solids can be divided into:

Amorphous solids

• no regular repeating units.

• melt over a range of T.

Examples: glass, plastics, ceramics…

Crystalline solids

• long-range order.

• sharp melting points.

Examples: ice, table salt, gems…

© 2008 Brooks/Cole 36

Crystalline Solids

Crystals have planar faces and sharp angles.

The angles are characteristic of the substance.

– they don’t depend on crystal size

– they reflect the shape of the crystal lattice

The smallest part of a lattice that can be used

to construct the full lattice is the unit cell.

7

© 2008 Brooks/Cole 37

Crystalline Solids

2d unit cell example:

• The unit cell is a square.

• Each corner contributes of a

circle to the unit cell.

• Net of 1 circle/unit cell.

• The entire lattice can be formed

by adding unit cells to each

face

© 2008 Brooks/Cole 38

Cubic Unit Cells

Crystals have 3d unit cells. There are 7 types.

The simplest are the cubic cells with 3 subtypes:

– simple (or primitive) cubic (sc).

– body-centered cubic (bcc).

– face-centered cubic (fcc).

Faces meet at 90° with equal-length sides.

© 2008 Brooks/Cole 39

Cubic Unit Cells

Primitive (simple) cubic

• Atoms sit at the corners of squares.

• Layers stack atom-on-atom.

• One atom/cell (8 x 1/8).

• Atoms occupy 52% of the total V.

1

3

24 56

at rear

Each atom has6 equivalent

neighbors:

© 2008 Brooks/Cole 40

Cubic Unit Cells

Body-centered cubic

• An extra (unshared) atom sits inthe center

• (8 x 1/8 ) + 1 = 2 atoms/cell

68 % of the space is occupied.

© 2008 Brooks/Cole 41

Cubic Unit Cells

Face-centered cubic

1 atom at the center of each face.

Face atoms are shared by 2 cells.

(6 x + 8 x 1/8 ) = 4 atoms/cell.

74% of the space is filled by atoms

© 2008 Brooks/Cole 42

Closest Packing of Spheres

Metal crystals have equal-sized atoms (spheres).

Single

layer

In closest packing, each atom has 6 neighbors/layer

A large percentage of the space is occupied.

8

© 2008 Brooks/Cole 43

Closest Packing of Spheres

Layers stack with the atoms in one

layer resting in “holes” of another.

hexagonal close packing

An abab structure

© 2008 Brooks/Cole 44

Closest Packing of Spheres

Start with “ab”

(“b” layer in “a” holes)

Add another “a” layer

(Green directly over green).

© 2008 Brooks/Cole 45

Cubic Close Packing

has an abcabc structure

(the unit cell is face centered cubic)

Closest Packing of Spheres

© 2008 Brooks/Cole 46

Cubic Close Packed

Start with “ab”.

(“b” layer in “a” holes)

Add “c” (gold) above holes in

the original green “a” layer.

© 2008 Brooks/Cole 47

Ionic Crystal Structures

Ionic crystal structures are more complex.

The ions making up the crystal:

• are not identical to each other.

• may be of very different sizes

• may not have the same charge magnitude.

• may not be “spheres” (polyatomic ions...)

© 2008 Brooks/Cole 48

Ionic Crystal Structures

Many ionic compounds have:

• sc or fcc negative-ion lattices.

• positive ions occupy “holes”.

CsCl unit cell

Cs+

Cl-

CsCl

Simple cubic Cl- (Cs+ in the central hole).

• This is not bcc

• Only use “bcc” if all atoms are identical

• In a unit cell: 8 x 1/8 = 1 Cl- and 1 Cs+

9

© 2008 Brooks/Cole 49

Ionic Crystal Structures

NaCl has an fcc Cl- lattice; Na+ in octahedral holes.

• Each Na+ is surrounded by 6 Cl-.

• Each Cl- is surrounded by 6 Na+.

© 2008 Brooks/Cole 50

It also contains 4 Na+:

12 edges x Na+/edge = 3 Na+

1 center x 1 Na+/center = 1 Na+

The NaCl unit cell contains 4 Cl- ions:

Ionic Crystal Structures

8 corners x 1/8 Cl- / corner = 1 Cl-

6 faces x Cl- / face = 3 Cl-

© 2008 Brooks/Cole 51

Network Solids

Some non-metals link together in extended networks.

DiamondGraphite

335 pm

141 pm

© 2008 Brooks/Cole 52

Materials Science

Study of the relationships between the structure and

the chemical and physical properties of materials.

Four major classes of materials:

Metals

Polymers

• Natural (cotton, rubber…) and synthetic (teflon,

polyethylene…). Thermal and electrical insulators.Nonmagnetic.

© 2008 Brooks/Cole 53

Materials Science

Ceramics

• Nonmetallic. Often clay based. Porcelain,

cement… Poor thermal conductors. Some are

magnetic. Usually crystalline. Include

semiconductors and glasses.

Composites

• Combinations of the 3 other materials. Properties

that exceed those of the individual components.

© 2008 Brooks/Cole 54

Metals

Opaque, shiny, usually crystalline. Form alloys.

• High electrical conductivity

• High thermal conductivity

• Ductile and malleable

• Mostly nonmagnetic (Fe, Ni, Co are exceptions)

• Have luster

Polished metals reflect light. Most metals reflect all

wavelengths equally (appear silvery-white).

• Insoluble in water and other common solvents

10

© 2008 Brooks/Cole 55

Metals

Metal Hfus mp

(kJ/mol) (°C)

Hg 2.3 -38.8

Ga 7.5 29.8

Na 2.6 97.9

Li 3.0 180.5

Al 10.7 660.4

U 12.6 1132.1

Fe 13.8 1535.0

Ti 20.9 1660.1

Cr 16.9 1857.0

W 35.2 3410.1

Hfus (and mp) vary widely:

Hfus

© 2008 Brooks/Cole 56

Metallic bonding = Nondirectional attraction between

M+ and a sea of mobile valence e-.

Electrons in Metals, Semiconductors, and Insulators

Valence e- spread throughout the M+ lattice, holding

the M+ ions together.

An electric field can pull valence e- to a “+” electrode

(electrical conduction).

M+ can move without destroying M+ ~ e- attractions

(ductility and malleability).

© 2008 Brooks/Cole 57

Band Theory

Every atom has E-levels (s, p, d…).1

Number of

atoms

e- inatoms

e- in latticeenergy levels

With many atoms, the E-levels get

so close together they form a band

3

2

12

As multiple atoms come togetherorbitals interact.

many

filled

empty

Electrons in Metals, Semiconductors, and Insulators

© 2008 Brooks/Cole 58

The valence band contains the valence e-.

Higher-E orbitals form the conduction band

In a metal, the valence and conduction band overlap.

e- can move freely between bands.

Metals, Semiconductors & Insulators

© 2008 Brooks/Cole 59

band gap

insulator semi-conductorconductor

MetalBands overlap.

Lots of open levels.

e- move freely.

InsulatorLarge band gap

e- cannot jump the gap.

No conduction.

SemiconductorNarrow band gap. Some e- can jump the gap…

Higher T = more energetic e- = better conductor.

Metals, Semiconductors & Insulators

© 2008 Brooks/Cole 60

Metals are better conductors at low T.

typical metal

Re

sis

tan

ce

Temperature (K)

superconductor

Tc

critical T

Superconductors have zero resistance (are perfectconductors) at some (low) T.

0

Superconductors

11

© 2008 Brooks/Cole 61

Metal Tc (K)

Aluminum 1.15

Gallium 1.10

Tin 3.72

Mercury 4.15

Lanthanum 4.9

Lead 7.2

Several metals are superconductors at low T

Nb3Sn alloy 18.1

YBa2Cu3O7 90.

LaBa2Cu3Ox 35.

He(l) boils at 4.2 K

Many He(l)-cooled

magnets use Nb-alloys

1st ceramic

superconductor (1986).

N2(l) boils at 77 K

“Y123” found 4 months later.

Highest Tc so far…Hg0.8Tl0.2Ba2Ca2Cu3O8.23 138.

Some alloys are better…

Superconductors

© 2008 Brooks/Cole 62

Silicon and the Chip

Ultra-pure Si is prepared by zone refining. Impurities are more

soluble in Si(l) than in Si(s). A molten zone is moved through a

sample. Impurities move along in the liquefied portion.

© 2008 Brooks/Cole 63

Silicon and the Chip

Doping is the controlled addition of some other element.

© 2008 Brooks/Cole 64

Silicon and the Chip

A p-n junction. Charge carriers: holes (p-type) and e- (n-type)

© 2008 Brooks/Cole 65

Silicon and the Chip

A photovoltaic cell. Light drives e- around an external circuit

© 2008 Brooks/Cole 66

Cement, Ceramics and Glasses

Amorphous solids:

Concrete = a mix of cement, sand and gravel.

Cement

Tiny metal-oxide particles (CaO, SiO2, Al2O3 & SiO2).

They crystallize irregularly when hydrated.

Made by heating limestone, sand, clay and iron oxide.

High compressive, but low tensile strength.

12

© 2008 Brooks/Cole 67

Cement, Ceramics and Glasses

Ceramics – made from clay or other natural earths.

Permanently hardened by heat.

Silicate ceramics – from clays. China clay (kaolin) is

white and used for table china. Red clay contains Fe.

Oxide ceramics – from metal oxides at high P and T.

Used in high-T applications. Excellent insulators. Canhave good mechanical strength.

Nonoxide ceramics – include Si3N2, SiC, and BN.

High P, T preparation. Hard, strong, but brittle.

© 2008 Brooks/Cole 68

Cement, Ceramics and Glasses

Glasses – optically transparent amorphous solids.

Simplest: vitreous silica = SiO2 in a 3d-lattice.

No long range order. (mp = 1800°C)

Soda lime glass, a SiO2, Na2O, CaO and MgO mix.

More inert and easier to make (mp ~800°C).

It can be colored (blue = add CoO, violet = MnO2…)