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The Science and Engineering of Materials, 4 th ed Donald R. Askeland – Pradeep P. Phulé Chapter 3 – Atomic and Ionic Arrangements

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Page 1: The Science and Engineering of Materials, 4th ed 3 - Atomic and Ionic... · 2020. 4. 22. · 3 Chapter 3 Outline 3.1 Short-Range Order versus Long-Range Order 3.2 Amorphous Materials:

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The Science and Engineering of Materials, 4th edDonald R. Askeland – Pradeep P. Phulé

Chapter 3 – Atomic and Ionic Arrangements

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Objectives of Chapter 3

To learn classification of materials based on

atomic/ionic arrangements

To describe the arrangements in crystalline solids

based on lattice, basis, and crystal structure

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Chapter 3 Outline

3.1 Short-Range Order versus Long-Range Order

3.2 Amorphous Materials: Principles and Technological Applications

3.3 Lattice, Unit Cells, Basis, and Crystal Structures

3.4 Allotropic or Polymorphic Transformations

3.5 Points, Directions, and Planes in the Unit Cell

3.6 Interstitial Sites

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No Order - In monoatomic gases, such as argon (Ar) or plasma

created in a fluorescent tubelight, atoms or ions have no orderly

arrangement.

Section 3.1

Short-Range Order versus Long-Range Order

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Short-range order (SRO) - The regular and predictable arrangement

of the atoms over a short distance - usually one or two atom spacings

(water vapor, nitrogen gas, amorphous silicon, silicate glass, and

many polymers).

Long-range order (LRO) - A regular repetitive arrangement of atoms

in a solid which extends over a very large distance (metals, alloys,

many ceramics, and some polymers).

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Basic Si-0 tetrahedron in silicate glass.

In a glass, individual tetrahedral units are joined together in a random manner.

These tetrahedra may share corners, edges, or faces, there is no periodicity in

arrangement of the basic unit of a (SiO4)4- tetrahedron.

In contrast, in quartz or other forms of crystalline silica, the (SiO4)4- tetrahedrals

are indeed connected in different periodic arrangements.

Short-range order example

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(a) Photograph of a silicon single crystal. (Single crystal: a crystalline material consists of only one

large crystal.) Single crystals are useful in many electronic and optical applications.

(b) Micrograph of a polycrystalline stainless steel showing grains and grain boundaries. A

polycrystalline material is composed of many small crystals with varying orientations in space.

Grain boundaries are the borders between crystals where the crystals are in misalignment.

Long-range order example

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Classification of materials based on the type of atomic order.

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Amorphous materials - Materials, including glasses, that have no long-range

order, or crystal structure.

In general, most materials want to form periodic arrangements since this

configuration maximizes the thermodynamic stability of the material.

Amorphous materials tend to form when, for one reason or other, the

kinetics of the process by which the material was made did not allow for the

formation of periodic arrangements.

Section 3.2

Amorphous Materials: Principles and Technological

Applications

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Atomic arrangements in crystalline silicon and amorphous silicon. (a) Amorphous

silicon. (b) Crystalline silicon.

Note the variation in the inter-atomic distance for amorphous silicon.

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Lattice - A collection of points that divide space into smaller equally sized

segments.

Lattice points - Points that make up the lattice. The surroundings of each

lattice point are identical.

Lattice parameters - The lengths of the sides of the unit cell and the angles

between those sides. The lattice parameters describe the size and shape of

the unit cell.

Section 3.3

Lattice, Unit Cells, and Crystal Structures

A one-dimensional lattice.

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Unit cell - A subdivision of the lattice that still retains the overall

characteristics of the entire lattice.

A two-dimensional crystal

The crystal with an overlay

of a grid that reflects the

symmetry of the crystal.

The repeat unit of the grid

known as the unit cell.

Each unit cell has its own

origin.

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Atomic radius - The apparent radius of an atom, typically calculated from

the dimensions of the unit cell, using close-packed directions (depends upon

coordination number).

Close-packed directions - Directions in a crystal along which atoms are in

contact.

Coordination number - The number of nearest neighbors to an atom in its

atomic arrangement.

Packing factor - The fraction of space in a unit cell occupied by atoms.

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Definition of the lattice parameters and their use in cubic, orthorhombic,

and hexagonal crystal systems.

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Crystal Systems

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Crystal Systems

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Crystal Systems

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The models for simple cubic (SC), body centered cubic (BCC), and face-centered cubic

(FCC) unit cells, assuming only one atom per lattice point.

Illustration showing sharing of face and corner atoms.

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Illustration of the coordination number in (a) SC and (b) BCC unit cells. Six atoms touch

each atom in SC, while the eight atoms touch each atom in the BCC unit cell.

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Determine the number of lattice points per cell in the cubic crystal systems. If

there is only one atom located at each lattice point, calculate the number of

atoms per unit cell.

Example 3.1 SOLUTION

In the SC unit cell: lattice point / unit cell = (8 corners)1/8 = 1

In BCC unit cells: lattice point / unit cell = (8 corners)1/8 + (1 center)(1) = 2

In FCC unit cells: lattice point / unit cell = (8 corners)1/8 + (6 faces)(1/2) = 4

The number of atoms per unit cell would be 1, 2, and 4, for the simple cubic,

body-centered cubic, and face-centered cubic, unit cells, respectively.

Example 3.1

Determining the Number of Lattice Points in Cubic

Crystal Systems

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Determine the relationship between the atomic radius and the lattice

parameter in SC, BCC, and FCC structures when one atom is located at

each lattice point.

Example 3.2

Determining the Relationship between Atomic Radius

and Lattice Parameters

ra 20 3

40

ra

2

40

ra

Example 3.2 SOLUTION

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Example 3.3

Calculating the Packing Factor

74.018)2/4(

)3

4(4)(

Factor Packing

24r/ cells,unit FCCfor Since,

)3

4)(atoms/cell (4

Factor Packing

3

3

0

3

0

3

r

r

r

a

a

Calculate the packing factor for the FCC cell.

Example 3.3 SOLUTION

In a FCC cell, there are four lattice points per cell; if there is one atom per lattice

point, there are also four atoms per cell. The volume of one atom is 4πr3/3 and

the volume of the unit cell is .3

0a

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The hexagonal close-packed (HCP) structure (left) and its unit cell (right).

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Allotropy - The characteristic of an element being able to exist in more

than one crystal structure, depending on temperature and pressure.

Polymorphism - Compounds exhibiting more than one type of crystal

structure.

Section 3.4

Allotropic or Polymorphic Transformations

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Example 3.5

Designing a Sensor to Measure Volume Change

To study how iron behaves at elevated temperatures, we would like to design

an instrument that can detect (with a 1% accuracy) the change in volume of a

1-cm3 iron cube when the iron is heated through its polymorphic

transformation temperature. At 911oC, iron is BCC, with a lattice parameter

of 0.2863 nm. At 913oC, iron is FCC, with a lattice parameter of 0.3591 nm.

Determine the accuracy required of the measuring instrument.

Example 3.5 SOLUTION

The volume of a unit cell of BCC iron before transforming is:

VBCC = = (0.2863 nm)3 = 0.023467 nm33

0a

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Example 3.5 SOLUTION (Continued)

The volume of the unit cell in FCC iron is:

VFCC = = (0.3591 nm)3 = 0.046307 nm3

But this is the volume occupied by four iron atoms, as there are

four atoms per FCC unit cell. Therefore, we must compare two BCC

cells (with a volume of 2(0.023467) = 0.046934 nm3) with each FCC

cell. The percent volume change during transformation is:

The 1-cm3 cube of iron contracts to 1 - 0.0134 = 0.9866 cm3

after transforming; therefore, to assure 1% accuracy, the instrument must

detect a change of:

ΔV = (0.01)(0.0134) = 0.000134 cm3

3

0a

%34.11000.046934

0.046934) - (0.046307 change Volume

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Miller indices - A shorthand notation to describe certain crystallographic

directions and planes in a material. Denoted by [ ] brackets. A negative

number is represented by a bar over the number.

Directions of a form (directions of a family) - Crystallographic

directions that all have the same characteristics, although their ‘‘sense’’

is different. Denoted by〈〉brackets.

Section 3.5

Points, Directions, and Planes in the Unit Cell

Coordinates of selected points in

the unit cell. The number refers to

the distance from the origin in

terms of lattice parameters.

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Determine the Miller indices of directions A, B, and C.

Example 3.6

Determining Miller Indices of Directions

Crystallographic directions and coordinates.

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Example 3.6 SOLUTION

Direction A

1. Two points are 1, 0, 0, and 0, 0, 0

2. 1, 0, 0, -0, 0, 0 = 1, 0, 0

3. No fractions to clear or integers to reduce

4. [100]

Direction B

1. Two points are 1, 1, 1 and 0, 0, 0

2. 1, 1, 1, -0, 0, 0 = 1, 1, 1

3. No fractions to clear or integers to reduce

4. [111]

Direction C

1. Two points are 0, 0, 1 and 1/2, 1, 0

2. 0, 0, 1 -1/2, 1, 0 = -1/2, -1, 1

3. 2(-1/2, -1, 1) = -1, -2, 2

2]21[ .4

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Because directions are vectors, a direction and its negative are not

identical; [100] is not equal to [100]. They represent the same line, but

opposite directions.

A direction and its multiple are identical; [100] is the same direction as

[200].

We expect a material to have the same properties in each of these twelve

directions of the form〈110〉.

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Equivalency of crystallographic directions of a form in cubic systems.

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Repeat distance - The distance from one lattice point to the adjacent

lattice point along a direction.

Linear density - The number of lattice points per unit length along a

direction.

Packing fraction - The fraction of a direction (linear-packing fraction) or

a plane (planar-packing factor) that is actually covered by atoms or ions.

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Determine the Miller indices of planes A, B, and C.

Example 3.7

Determining Miller Indices of Planes

Crystallographic planes and intercepts.

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Example 3.7 SOLUTION

Plane A

1. x = 1, y = 1, z = 1

2. 1/x = 1, 1/y = 1 , 1/z = 1

3. No fractions to clear

4. (111)

Plane B

1. The plane never intercepts the z axis, so x = 1, y = 2, and z =

2. 1/x = 1, 1/y =1/2, 1/z = 0

3. Clear fractions:

1/x = 2, 1/y = 1, 1/z = 0

4. (210)

Plane C

1. We must move the origin, since the plane passes through 0, 0, 0. Let’s move the origin one lattice parameter in the y-direction. Then, x = , y = -1, and z =

2. 1/x = 0, 1/y = -1, 1/z = 0

3. No fractions to clear.

)010( .4

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Planes and their negatives are identical (this was not the case for

directions) because they are parallel. Therefore, (020)=(020).

Planes and their multiples are not identical (again, this is the opposite of

what we found for directions).

In each unit cell, planes of a form or family represent groups of

equivalent planes that have their particular indices because of the

orientation of the coordinates. We represent these groups of similar

planes with the notation {}.

In cubic systems, a direction that has the same indices as a plane is

perpendicular to that plane.

The planar density is the number of atoms per unit area with centers that

lie on the plane.

The packing fraction is the fraction of the area of that plane actually

covered by these atoms.

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Calculate the planar density and planar packing fraction for the (010) and (020)

planes in simple cubic polonium, which has a lattice parameter of 0.334 nm.

Example 3.8

Calculating the Planar Density and Packing Fraction

The planer densities of the (010) and (020) planes in SC unit cells are not identical.

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Example 3.8 SOLUTION

The total atoms on each face is one. The planar density is:

2142

2

atoms/cm 1096.8atoms/nm 96.8

)334.0(

faceper atom 1

face of area

faceper atom (010)density Planar

The planar packing fraction is given by:

79.0)2(

)(

)( atom) 1(

face of area

faceper atoms of area (010)fraction Packing

2

2

20

2

r

r

r

a

However, no atoms are centered on the (020) planes. Therefore, the

planar density and the planar packing fraction are both zero. The (010)

and (020) planes are not equivalent!

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Example 3.9

Drawing Some Planes

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Miller-Bravais indices are obtained for crystallographic planes in HCP unit cells by

using a four-axis coordinate system.

Typical directions in the HCP unit cell, using both three-and-four-axis systems. The

dashed lines show that the [1210] direction is equivalent to a [010] direction.

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Determine the Miller-Bravais indices for planes A and B and directions C

and D in Figure 3.25.

Example 3.10

Determining the Miller-Bravais Indices for Planes and

Directions

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Example 3.10 SOLUTION

Plane A

1. a1 = a2 = a3 = , c = 1

2. 1/a1 = 1/a2 = 1/a3 = 0, 1/c = 1

3. No fractions to clear

4. (0001)

Plane B

1. a1 = 1, a2 = 1, a3 = -1/2, c = 1

2. 1/a1 = 1, 1/a2 = 1, 1/a3 = -2, 1/c = 1

3. No fractions to clear

4.

Direction C

1. Two points are 0, 0, 1 and 1, 0, 0.

2. 0, 0, 1, -1, 0, 0 = 1, 0, 1

3. No fractions to clear or integers to reduce.

4.

)1211(

113]2[or ]011[

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Example 3.10 SOLUTION (Continued)

Direction D

1. Two points are 0, 1, 0 and 1, 0, 0.

2. 0, 1, 0, -1, 0, 0 = -1, 1, 0

3. No fractions to clear or integers to reduce.

4. 100]1[or ]101[

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Close-packed (CP) structure - Structures showing a packing fraction

of 0.74 (FCC and HCP).

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The ABABAB stacking sequence of close-packed planes produces the HCP structure.

The coordination number is twelve.

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The ABCABCABC stacking sequence of close-packed planes produces the FCC structure.

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Interstitial sites - Locations between the ‘‘normal’’ atoms or ions in a crystal

into which another - usually different - atom or ion is placed. Typically, the

size of this interstitial location is smaller than the atom or ion that is to be

introduced.

Cubic site - An interstitial position that has a coordination number of eight.

An atom or ion in the cubic site touches eight other atoms or ions.

Section 3.6

Interstitial Sites

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Octahedral site - An interstitial position that has a coordination number of

six. An atom or ion in the octahedral site touches six other atoms or ions.

Tetrahedral site - An interstitial position that has a coordination number of

four. An atom or ion in the tetrahedral site touches four other atoms or ions.

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Example 3.11

Calculating Octahedral SitesCalculate the number of octahedral sites that uniquely belong to one FCC unit cell.

Example 3.11 SOLUTION

The octahedral sites include the 12 edges of the unit cell and the center position.

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Atoms with radii smaller than the radius of the hole are not allowed to fit

into the interstitial site because the ion would “rattle” around in the site.

If the interstitial atom becomes too large, it prefers to enter a site having a

larger coordination number.

Interstitial atoms or ions whose radii are slightly larger than the radius of the

interstitial site may enter that site, pushing the surrounding atoms slightly

apart.

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We wish to produce a radiation-absorbing wall composed of 10,000 lead balls,

each 3 cm in diameter, in a face-centered cubic arrangement. We decide that

improved absorption will occur if we fill interstitial sites between the 3-cm balls

with smaller balls. Design the size of the smaller lead balls and determine how

many are needed.

Example 3.12

Design of a Radiation-Absorbing Wall

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Example 3.12 SOLUTION

First, we can calculate the diameter of the octahedral sites located between the

3-cm diameter balls.

Length AB = 2R + 2r = 2 R

r = R – R = ( - 1)R

r/R = 0.414

Since r/R = 0.414, the radius of the small lead balls is

r = 0.414 * R = (0.414)(3 cm/2) = 0.621 cm.

From Example 3-11, we find that there are four octahedral sites in the FCC

arrangement, which also has four lattice points. Therefore, we need the same

number of small lead balls as large lead balls, or 10,000 small balls.

2

2

2