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Crystal Systems Crystal System Terms Crystal Systems Crystal System Terms

Crystal Systems Crystal System Terms - PowerPoint Presentation

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Crystal Systems Crystal System Terms - PPT Presentation

Unit Cell smallest repeating unit of a crystal structure Slip Planes surface along which layers of atoms can slide past one another plane of closely packed atoms Crystal System Terms Void or Interstice ID: 653279

sulfur crystal planes slip crystal sulfur slip planes atoms crystals packed morton schaffer cubic fcc grain defects grains hcp bcc amorphous boundaries

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Slide1

Crystal SystemsSlide2

Crystal System Terms

Unit Cell

smallest repeating unit of a crystal structure

Slip Planes - surface along which layers of atoms can slide past one another

plane of closely packed atomsSlide3
Slide4
Slide5

Crystal System Terms

Void or Interstice-

empty space in a crystal Slide6

Crystal Packing – loosely packedSlide7

Crystal Packing – More Densely Packed

Most metals are

close packed

- that is, they fit as many atoms as possible into the available volumeSlide8

simple cubic

FCC

– Face Centered Cubic

BCC

- Body Centered Cubic

HCP

– Hexagonal

Close PackedSlide9

Slip Planes of FCC

Morton SchafferSlide10

Slip Planes

Morton Schaffer

1Slide11

Slip Planes

Morton Schaffer

2Slide12

Slip Planes

Morton Schaffer

3Slide13

Slip Planes

Morton Schaffer

4Slide14

Slip Planes

Morton Schaffer

5Slide15

Slip Planes

Morton Schaffer

6Slide16

Slip Planes

Morton Schaffer

7Slide17

Body-centered cubic (BCC)

Face-centered cubic (FCC)

Hexagonal close-packed (HCP)

center atom

Slip Planes

Morton Schaffer

12 Slip Planes

Up to 48 Slip Planes

3 Slip PlanesSlide18
Slide19

STOP – Crystal Models LabSlide20

SIMPLE CUBIC

FACE CENTERED CUBIC

(FCC)

BODY CENTERED CUBIC

(BCC)

HEXAGONAL CLOSE PACKED

(HCP)Slide21
Slide22

Why do Crystal Systems Matter?

Workability

changing the shape of a solid without breaking or cracking

Malleability

ability of being hammered into thin sheets

Ductility

ability of being drawn into wiresSlide23

Workability

Which crystal structure is more workable?

Many slip planes or few slip planes?

Tightly packed or loosely packed? Slide24

Models of Crystals Lab

*more tightly packed = more workable

*more slip planes = more workable

Type of crystal structure

Closely packed?

Many slip planes?

Workability

FCC

BCC

HCPSlide25

Models of Crystals Lab

*more tightly packed = more workable

*more slip planes = more workable

Type of crystal structure

Closely packed?

Many slip planes?

Workability

FCC

Yes

Yes

Highest

BCC

No

Yes

Medium

HCP

Yes

No

LowestSlide26

Crystal Structures & Metals

BCC

FCC

HCP

OtherSlide27

Crystal Structures & Metals

BCC

FCC

HCP

Other

Chromium

Aluminum

Cobalt

Manganese

Iron (<910°C)

Calcium

Magnesium

tin

Molybdenum

Copper

Titanium

Sodium

Gold

zinc

tungsten

Iron (>910°C)

Lead

Nickel

Platinum

silverSlide28

28

Sargent Welch Periodic Table

Crystal structures on the back.Slide29

Crystalline vs. Amorphous?

Orderly arrangement

Repeating pattern

Predictable

Opaque (not see through)

Random arrangement

No repeating pattern

Not predictable

ClearSlide30

Allotropes (review)

Different forms of the same element in the same physical state

Difference is in how the atoms are arranged

Also called polymorphism

Examples:

Carbon – diamond, graphite,

buckyballs

Oxygen – O

2

(atmospheric) and O

3

(ozone)

Sulfur – rhombic, monoclinic, amorphousSlide31

Allotropes of Carbon

buckyballSlide32

Allotropes of Sulfur

rhombic

amorphous

monoclinicSlide33

Solid State Phase Change

Change in crystal structure while remaining a solid.

Example:

Amorphous sulfur changing to crystalline sulfurSlide34

Milk Jug DemoWhat is happening when you heat the plastic to the crystal structure

?

Before heat

 Crystalline b/c it was opaque

During heating  Changing to amorphous, became clear

After heat  atoms were able to go back to close to original states & went back to crystallineSlide35

Sulfur LabGrowing CrystalsSlide36

Sulfur MSDSSlide37

Sulfur MSDSSlide38

Sulfur MSDSSlide39

Sulfur MSDSSlide40

Monday, 9/19/16Review lab on Friday!Slide41

Part A – Rhombic Sulfur

Forming crystals from a solution

What did we do?

Heated

in mineral oil to dissolve

What did we see?

Crystals

formed in

solutionSlide42
Slide43

Part B: Monoclinic Sulfur

Forming crystals from a melted substance

What did we do?

1

. Fill a test tube approximately

1/2

full with sulfur. Keep the sulfur powder off the sides of the test tube.

2

. Make a cone out of

filter paper

and place it in a funnel.

3. Heat the test tube of sulfur

very

slowly - passing it back and forth above the flame. Totally melt to a liquid. Use

Bunsen burner

and test tube clamp. Keep the sulfur

yellow

.

4. Pour liquid sulfur into filter paper cone. As soon as a crust forms, open the filter paper to original shape. Slide44
Slide45
Slide46

What did we see? Forming crystals from a melted substanceLong skinny pointy crystalsSlide47
Slide48
Slide49

Part C: Amorphous Sulfur

What did we do?

Heat

sulfur slowly. It will pass through

stages.

Pour

hot sulfur into beaker of cold water. (quench

)

What did we see?

melt to yellow liquid

individual rings of 8

red liquid

short chains of 8 – 16 sulfur atoms

dark reddish-brown thick syrup

longer chains of sulfur atoms that entangle

dark runny liquid

longer chains of sulfur atoms that have enough energy to flowSlide50

Ring of

8 sulfur atoms

Chain

of sulfur

atomsSlide51

Amorphous SulfurSlide52

Crystalline balls

of sulfurSlide53

What does crystalline mean?How easy is it to grow a perfect crystal?What types of defects are possible?

Crystal DefectsSlide54

CRYSTAL TERMS

Grains

individual crystals

They grow in different directions and meet up with each other

 

Grain Boundary

boundaries where grains meetSlide55
Slide56

Crystal Grains

“Crystal grains

are regions of regularity. At the grain

boundaries,

atoms have become misaligned. Slide57

Crystal Defects and Imperfections

I

mpurities

and disruptions in the pattern of atoms

A

ffect

many physical properties

T

hree

main typesSlide58

1. Interfacial Defects

grain boundaries

affected by size of grainsSlide59
Slide60

By cooling more quickly, a smaller grain size results and this has the effect of making the resulting solid stronger. Figure

2 and Figure 3 are examples of metals with different grain size – the one exhibited in Figure 3 will be significantly stronger than its counterpart in Figure 2.

Figure 2

Figure 3Slide61

Application in IndustryCreepHigh temperatures with less grain boundaries

(30-50% of melting temperature)

Stronger

Stretching

Low temperatures with more grain boundaries

Increases tensile strength – more stretch

Read Case Study on “Creep of Turbine Blades”Slide62

Phenyl Salicylate Demo

freezing a liquid to grow crystals

nucleation

site – location where a crystal starts growing

watch

for grains and grain boundariesSlide63

2. Dislocation – Line Defects

regions in crystals where atoms are not perfectly aligned – an extra partial plane

can

move

a small number make a metal more workable

a large number make a metal harder to work

dislocations can get “jammed” or “pinned”

makes the metal harder =

work-hardening

Becomes so strong it becomes brittle and breaksSlide64
Slide65
Slide66
Slide67
Slide68
Slide69

Dislocation MovementSlide70

3. Point Defects

single atom

defectsSlide71

Substitutional

replace some of the original atoms with different atoms

used in making alloys

examples – brass and bronzeSlide72

Interstitial extra atoms inserted in the gaps between the regular atomsused in making alloys

example - steelSlide73

Vacancyatom is missing (void)move around in crystal by diffusionSlide74

Silver Nitrate onCopper Wire

Growing CrystalsSlide75

Growing Silver Crystals

Place a flattened 1” piece of Cu wire on a microscope slide.

Focus one end of wire under stereoscope.

Have the teacher drop AgNO

3

(silver nitrate) on the wire.

Make observations:

Low and high power

Light from above and belowSlide76

Crystal Definitions

Dendrites

crystal branches

crystal growth pattern – directional

grow until they eventually become large enough to impinge upon (interfere with) each other

spaces between the dendrite arms

crystallize to make a more regular

crystalSlide77

Once nucleated, the dendrites spread sideways and the secondary arms generate further tertiary arms and so on. When solidification is complete, all the dendrites that have formed knit together to form grains (or crystals).Slide78
Slide79

Snow - IceSlide80

Dendritic copper crystals