This edition of the classic text/reference book has been updated and revised to provide balanced coverage of metals, cer
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English Pages 1072 Year 1990
Engin
and Their Applications
PHYSICAL PROPERTIES OF SELECTED ELEMENTS Atomic Element
Aluminum Argon Barium Beryllium
Boron Bromine
Cadmium
Symbol Number Al
A Ba Be B Br
Calcium Carbon Cerium
Cd Ca C Ce
Cesium
Cs
Chlorine
Chromium Cobalt
Copper
Co Cu
Fluorine
F
Germanium
Ge
Gold Helium Hydrogen
Au He H
1
Iodine
13 18
56
Atomic Weight
901
5
10.82 79.92 112.41
4008
6
1201
58 55
140.13
CI
17
Cr
24 27 29
35.46 52 01
1
Iron
Fe
Lead
Pb
Lithium
Li
Magnesium Manganese
Mg Mn
Mercury
Hg
Molybdenum Neon
9
32 79 2 1
53 26 82
132.91
5894 63 54
3
6.94
2432 20061
Mo
25 80 42
Ne
10
95 95 20.18
Nickel
Ni
28
5871
Niobium
Nb
41
92.91
Nitrogen
N
7
14.01
Oxygen Phosphorus 2
8
16.00
P
15
54 94
Platinum Potassium
Pt
K
19
Scandium
Sc
21
30 98 195 09 39 .10 44 96
Silicon
Si
14
Silver
Sodium
Ag Na
Strontium Sulfur 3 Tin
1.85
Ortho.
3 12
Ortho
1.19
1
321
8.65
1
1.55
HCP FCC
1.50
838 3727 804
1.97
1.06
225
Hex
0.71
S
£
i
t. OS -
in CO
c
oo OS
=
U
S
X
c
In
U.
1
E
The Structure of Engineering Materials
TABLE
1.4
31
Bond Energies
(in
kj/mol)* Single Bonds
H H
432
C N
411
346 305 358 272 485 327 285 213
386 459 363 565 428 362 295
O S F
CI Br I
N
O
167 201
—
142
283 313
190
218
—
201 201
C
—
—
F
S
226 284 255 217
CI
Br
/
240 216 208
190 175
149
155
249 249 278
—
Multiple Bonds
C=C
C=N C=N N= o=o
.i).1
C=C
835 418 942
N=C N=N
"Data are taken from Used by permission.
EXAMPLE
J.
E.
Huheey, Inorganic Chemistry. 2nd
1.4
C = =o c= E=0 s= =o s= =o
615 887 607 494 ed.
|New
York: Harper
XA
XB
=
Xc
—
-
Xf
S0 2 S0 3
& Row,
|
|
1978), pp.
842-850.
is
BE(A
to B)
- l/2[BE(A
to A)
(4.0) as a
+ BE(B
reference
to B)]
96.5 kj
485 kj - 1/2(346 +155) kj 96.5 kj
= Therefore, carbon
in
[ES]
Calculate the electronegativity of carbon, using fluorine and the data of Table 1.4.
Answer
in
799 1072 532 469
1.56
1.56
below
which
fluorine, or 2.44,
is
close to the value
of 2.5 given in Table 1.3.
Mixed Ionic and Covalent Bonding We in
rarely encounter cases of perfect ionic or covalent
which the electrons
bonding
— that
are completely donated or equally shared.
is,
cases
Another
Pauling formula can be used to calculate the percent ionic bonding (the rest of the
bonding
is
covalent).
Fraction ionic
where
XA
and
XB
=
1
-
e
^*s)2
- 1/4(;f
are electronegativities of the
two
species.
(1-5)
32
Fundamentals
CRYSTALLINE AND NONCRYSTALLINE GLASS STRUCTURES 1.12
Comparison
of Crystalline
Noncrystalline Structures
and
— General
Now
that we have studied the electronic structures of the atoms and how they lead to bonding into interatomic groups, we are ready to see how these groups are assembled in engineering materials as larger groups that make up crystals, grains, the noncrystalline structures of glasses, including glassy metals, the mixed glass-ceramics, and the glassy and crystalline polymers.
Before getting into the details of these
two groups,
let
us compare their prin-
cipal features.
atoms occupy regular positions describe by using a space lattice. Metals, for example, are crystalline under normal conditions. We developed a rather striking example by acIn the typical crystalline material, the
we can
that
cident (Figure 1.15). We were attempting to dissolve magnesium in liquid cast iron using a pressure chamber with an argon atmosphere. After cooling we fine, brilliant crystals of magnesium on the inside of the cover. (At these temperatures magnesium vaporized from the melt and condensed on the cover.) The hexagonal faces were quite evident; they are manifestations of the hexagonal arrangement of magnesium atoms within. In the usual case, as
found
magnesium, we would expect to find not crystal faces but a number of grains (Figure 1.16, page 34). However, if we examine the structures of the individual grains, we find the atoms arranged in an independent space latin a bar of
tice in
This
is
each grain, with the same hexagonal structure as in the single crystals. called long-range order.
As an example quartz.
page
We
of a
ceramic crystal, we may consider the structure of network of Si and O atoms (Figure 1.17a,
find a regular, hexagonal
34).
By
is no regular space lattake a crystal of quartz, melt it, and cool the melt in air, we obtain a glassy mass called fused silica (Figure 1.17b). We still find that each silicon atom is surrounded by four oxygen atoms, forming a tetrahedron, but there is no regular repetition of this structure on a space lattice. Another major differ-
tice. If
contrast, in the noncrystalline materials there
we
ence from the original quartz, which exhibits a definite melting point, is that the noncrystalline mass gradually softens upon heating and finally turns to a viscous liquid. In addition to the ceramic glasses, the polymers are entirely or partly glassy*
'Sometimes the word amorphous is used to describe the lack of crystallinity. However, we have no long- or short-range order for it to be called amorphous.
will require that a material
33
The Structure of Engineering Materials
FIGURE
1.15
Magnesium condensed from
the vapor: approximately l,000x
|Stephen Krause, Department of Mechanical Engineering, Arizona State University]
(Figure 1.18, page 35). For example, in the case of the phenol
resin (often called "bakelite") encountered in a bowling ball,
formaldehyde
we have
a single,
three-dimensional network that is essentially a giant molecule but lacks the long-range order of a crystal (Figure 1.18a). In another type of polymer in which the giant molecules are linear, and which is made up of a backbone of a chain of carbon atoms, some crystallization may occur when the chain is bent back and forth regularly (Figures 1.18i>, c). With those distinctions in mind, let us review the crystalline structures
and some ceramics and then consider the noncrystalline structures encountered in other ceramics and polymers. typically encountered in metals
34
Fundamentals
FIGURE
1.16
Grain structure in bar
FIGURE
1.17
Schematic representation of {a) ordered crystalline form and of the same composition
network glassy form
of
magnesium
[b]
random-
35
The Structure of Engineering Materials
Folded-chain theory
Giant noncrystalline molecule of phenol formaldehyde, [b] Crysby the folding back of chains. The growth mechanism involves the folding over of the planar zigzag chain on itself at intervals of about every 100 chain atoms. A single crystal may contain many individual molecules, (c) Spherulites (spherelike areas of crystallinity) in polycarbonate polymer; transmission electron mi-
FIGURE
1.18
{a)
tallinity created
crograph, 66, 000 x. [Parts (a)
and
New York,
University of
1.13
(b)
from
L. E.
Nielsen, Mechanical Properties of Polymers. Litton Educational Publishing, Inc., Van Nostrand Reinhold Company. Part (c) courtesy Jim de Rudder,
1962. Reprinted by permission of
Michigan]
Crystalline Structures We
— Metals
have already agreed that the hallmark of a crystal structure is the regular repeating arrangement of atoms. It will be very useful to us in the next chapter, when we investigate the effects of stress on crystal structure, to have a clear, simple mathematical model of the atoms' positions. To create one, we begin with a space lattice to suit our particular metal. For example, if the crystal is
36
Fundamentals
we choose
cubic,
called a unit cell,
module
By describing
of cubes.
can specify the entire
scribing just one office
1.14
made up
a lattice
we
in a skyscraper
a single cube, analogous to deup of identical modules.
This
lattice.
made
is
The Unit Cell describe the unit cell and later the movement of an atom in the cell, we need a system for specifying (1) atom positions or coordinates, (2) directions in the cell, and (3) planes in the cell.
To
Position position of an atom is described with reference to the axes of the unit and the unit dimensions of the cell. Suppose that a grain or crystal is 1 built of unit cells of dimensions a ' b and c angstroms, as shown in Figure
The cell
,
,
axes are at right angles to each other. To construct the cell, we merely lay out a (the lattice parameter) in the x direction, b in the y direction, and c in the z direction. The figure shows the coordinates of sev1.19. In this case the
eral atoms in the cell. An atom at the center would have coordinates \, \, \, whereas an atom in the center of the face in the xy plane would have coordinates \, \, 0. It is important to note that commas after coordinates in space are a signal that we are referring to points in that space. These coordinates are not enclosed in parentheses; we do not want you to confuse them with
planes,
Up
which we
shall discuss in a later section.
to this point
we have used
a relatively simple cell as an example. In
nature, 14 different types of crystal lattices are found (Figure 1.20). These lat-
and
tices cover the variations in the length of a, b,
tween the
we
Fortunately, in metals
shown
c
and in the angles be-
axes.
find mostly the three simple types of cells
in Figure 1.21 (page 39): body-centered cubic (BCC), face-centered cu-
Some of the other types are encountered occasionally in a few metals, ceramics and polymers.
bic (FCC), and hexagonal close-packed (HCP).
Direction To
specify a direction in the unit
of the direction ray at the origin
cell, we merely place the base of the arrow and follow the shaft until we encounter in-
tegral coordinates (Figure 1.22, page 40). Instead of constructing other cells,
'The subscript ally 68°F (20°C).
'The angstrom meter;
1
A
= 10
specifies that this
When 10
|A)
dimension
is
measured
the unit cell expands with temperature,
=
at a
a, b,
standard temperature, usu-
and c change.
10~ 8 cm. In the SI system of units, the linear unit of measure
meter (m) =
0.1
12
perimenters prefer picometers (10~ sociated with the larger nanometer.
nm
is
the
= 10" m. Both A and nm will should also be noted that some exm) in order to have whole numbers rather than decimals as-
nanometer (nm), where
be used in the following discussion of unit cell dimensions.
1
It
The Structure of Engineering Materials
FIGURE atom
1.19
A shown
37
Coordinates of atoms in the face-centered positions in a unit cell. The would have coordinates T, 0, 1. Note: T is equiva-
in the next unit cell
lent to -1.
we can
use a point that has fractional intercepts in the unit cell and multiply common denominator. Thus direction A is obviously [111], but B has coordinates \,\, at the edge of the cell. These become [210]. Note that in specifying a direction, we put square brackets around the numbers to distinguish direction from the notation for coordinates and parentheses for a plane, described later. Note also that we can have negative-direction indices, as
by the
least
shown by C. We indicate If we wish to find the
we
origin,
these with an overbar. indices of a direction that does not pass through the merely pass a parallel direction through the origin and proceed
as before.
system the dimensions of the unit cell are the same: a = order in a given set of indices, such as [110], depends on which
In the cubic
b = c
The
.
directions
we happened
to choose for x, y,
and z in the crystal, because in the we wish to signify a set of direcand [011]. These are all directions
cubic system the indices are identical. Often
tions that are related, such as [110], [101], across the face diagonal of the cube. To specify these similar directions, we use pointed brackets and the indices of only one direction. Thus