Sunday 28 July 2013

Solid Solution glass formation

Solid Solution




When atoms or ions are approximately the same size, they may substitute for another in the structure.
For example, Cu and Au have similar radii and at high temperature form a complete solid solution,

Simple Structures

Simple Structures

If atoms or ions are considered to be spheres, then the most efficient packing of the spheres in space
will form their most stable structure. However, the type of bonding—in particular, directional
bonding—may affect the structure formed. In two dimensions, there is only one configuration that
most efficiently fills space, the close-packed layer  . If similar layers are stacked to form
a three-dimensional structure, an infinite number of configurations is possible. Two are important. In both, the first two layers are the same. In the first layer (A), the point at the center of three spheres
provides a hollow for a fourth sphere to rest. A second close-packed layer (B) then can be placed
on the first layer, with each sphere occupying the hollow. With the addition of a third layer to these
two layers, two choices are possible. A sphere in the third layer can be placed above a sphere in the
first layer in the spaces marked (•)   or above a hollow not occupied by a sphere spaces
marked (x) in the second layer. If the first stacking arrangement is continued, that is, the first and
third layers in registry with each other (denoted ABABA . . .), the hexagonal close-packed (hep)
structure is generated, so called because of the hexagonal symmetry of the structure. If the second
stacking arrangement is continued, that is, the first and third layers are not on top of each other
(denoted ABCABC . . .), the cubic close-packed or face-centered cubic (fee) structure is generated,
so called because the structure formed is a face-centered cube. Both structures are shown in Fig. 1.3.
In both structures, 74% of the volume is occupied and each sphere is contacted by 12 spheres (or
12 nearest neighbors), although the arrangement is different. Another common structure is the bodycentered
cubic (bcc) structure shown in Fig. 1.3. Here, each sphere has eight nearest neighbors, with
another six at a slightly greater distance. The volume fraction occupied is 68%. In the hep and fee
structures, the stacking of a fourth sphere on top of three in any close-packed layer generates a
tetrahedral site or void, as shown in Fig. 1.4. Into such a site a smaller sphere with a coordination
number of four could fit. Three spheres from each of two layers generate an octahedral site or void,
 . Into such a site a smaller sphere with a coordination number of six could fit.
In the hep and fee structures, there are two tetrahedral and one octahedral sites per packing sphere;
however, the arrangement of these sites is different.

Crystallography

All possible crystallographic structures are described in terms of 14 Bravais space lattices—only 14
different ways of periodically arranging points in space. . Each of the positions in a given space lattice is equivalent and an atom or ion or group of atoms or ions can be
centered on each position. Each of the lattices is described by a unit cell,  The seven crystallographic systems

States of Matter

Matter can be divided into gases, liquids, and solids. In gases and liquids, the positions of the atoms
are not fixed with time, whereas in solids they are. Distances between atoms in gases are an order
of magnitude or greater than the size of the atoms, whereas in solids and liquids closest distances
between atoms are only approximately the size of the atoms. Almost all engineering materials are
solids, either crystalline or noncrystalline.

Crystalline Solids

In crystalline solids, the atoms or ions occupy fixed positions and vibrate about these equilibrium
positions. The arrangement of the positions is some periodic array, as discussed in Section 1.1.5. At
O0K, except for a small zero-point vibration, the oscillation of the atoms is zero. With increasing
temperature the amplitude and frequency of vibration increase up to the melting point. At the melting
point, the crystalline structure is destroyed, and the material melts to form a liquid. For a particular
single crystal the external shape is determined by the symmetry of the crystal class to which it
belongs. Most engineering materials are not single crystals but poly crystalline, consisting of many
small crystals. These crystals are often randomly oriented and may be of the same composition orof different composition or of different structures. There may be small voids between these grains.
Typical sizes of grains in such poly crystalline materials range from 0.01 to 10 mm in diameter.

Noncrystalline Solids

Noncrystalline solids (glasses) are solids in which the arrangement of atoms is periodic (random)
and lacks any long-range order. The external shape is without form and has no defined external faces
like a crystal. This is not to say that there is no structure. A local or short-range order exists in the
structure. Since the bonding between atoms or ions in a glass is similar to that of the corresponding
crystalline solid, it is not surprising that the local coordination, number of neighbors, configuration,
and distances are similar for a glass and crystal of the same composition. In fused SiO2, for example,
four O's surround each Si in a tetrahedral coordination, the same as in crystalline SiO2.
Glasses do not have a definite melting point, crystals do. Instead, they gradually soften to form
a supercooled liquid at temperatures below the melting point of the corresponding crystal. Glass
formation results when a liquid is cooled sufficiently rapidly to avoid crystallization. This behavior
is summarized in Fig. 1.6, where the volume V is plotted as a function of temperature T.Crystalline materials of the same composition exhibit more than one crystalline structure called
polymorphs. Fe, for example, exists in three different structures: a, y, and 5 Fe. The a phase, ferrite,
a bcc structure, transforms at 91O0C to the y phase, austenite, an fee structure, and then at 140O0C
changes back to bcc structures 6-iron or 6-ferrite. The addition of C to Fe and the reactions and
transformations that occur are extremely important in determining the properties of steel.
SiO2 exhibits many polymorphs, including a- and /3-quartz, a- and /3-tridymite, and a- and /3-
cristobalite. The SiO4 tetrahedron is common to all the structures, but the arrangement or linking of
these tetrahedra varies, leading to different structures. The a —> /3 transitions involve only a slight
change in the Si-O-Si bond angle, are rapid, and are an example of a phase transformation called
displacive. The quartz —> tridymite —> cristobalite transformations require the reformation of the new
structure, are much slower than displacive transformations, and are called reconstructive phase transformations.
The a —> y —> 8 Fe transformations are other examples of reconstructive transformations.
A phase diagram gives the equilibrium phases a function of temperature, pressure, and composition.
More commonly, the pressure is fixed at 1 atm and only the temperature and composition are
varied.

Defects
The discussion of crystalline structures assumes that the crystal structures are perfect, with each site
occupied by the correct atoms. In real materials, at temperatures greater than O0K, defects in the
crystalline structure will exist. These defects may be formed by the substitution of atoms different
from those normally occupying the site, vacancies on the site, atoms in sites not normally occupied
(interstitials), geometrical geometrical alterations of the structure in the form of dislocations, twin boundaries, or grain boundaries.








Saturday 27 July 2013

Different Type of Bonding.......

 Effects of Structure on Properties

Physical properties of metals, ceramics, and polymers, such as ductility, thermal expansion, heat
capacity, elastic modulus, electrical conductivity, and dielectric and magnetic properties, are a direct
result of the structure and bonding of the atoms and ions in the material. An understanding of the
origin of the differences in these properties is of great engineering importance.
In single crystals, a physical property such as thermal expansion varies with direction, reflecting
the crystal structure; whereas in polycrystalline and amorphous materials, a property does not vary
with direction, reflecting the average property of the individual crystals or the randomness of the
amorphous structure. Most engineering materials are polycrystalline, composed of many grains, and
thus an understanding of the properties requires not only a knowledge of the structure of the single
grains but also a knowledge of grain size and orientation, grain boundaries, and other phases present;
that is, a knowledge of the microstructure of this material.

Atomic Structure

Atoms consist of electrons, protons, and neutrons. The central nucleus consists of positively charged protons and electrically neutral neutrons. Negatively charged electrons are in orbits about the nucleus
in different energy levels, occupying a much larger volume than the nucleus.
In an atom, the number of electrons equals the number of protons and, hence, an atom is neutral.
The atomic number of an element is given by the number of protons, and the atomic weight is given
by the total number of protons and neutrons. (The weight of the electrons is negligible.) Thus,
hydrogen, H, with one proton and one electron, has an atomic number of 1 and an atomic weight of
1 and is the first element in the periodic chart. Oxygen, O, with atomic number 8, has eight protons
and eight neutrons and, hence, an atomic weight of 16.
Completed electronic shells have a lower energy than partially filled orbitals when bonded to
other atoms. As a result of this energy reduction, atoms share electrons to complete the shells, or
gain or lose electrons to form completed shells. In the latter case, ions are formed in which the
number of electrons is not equal to the number of protons. Thus, O by gaining two electrons, has a
charge of -2 and forms the oxygen ion O2-.
The periodic chart arranges elements in columns of the same electronic configuration. The first
column consists of the alkalies Li, Na, K, Cs, Rb; each has one electron in the outer shell that can
be lost. Similarly, the second column of alkaline-earths can form Mg2+, Ca2+, Sr2+, Ba2+ by losing
two electrons. The seventh column consists of the halogens Fl, Cl, Br, I, which by gaining one
electron become the halides, all with a charge of -1. The eighth column consists of the inert gases
He, Ne, Ar, K, Xe, with completed shells. The bonding of the elements and ions with similar electronic
configurations is similar. Moving down a column increases the number of electrons and, hence,
the atom's size increases even though the outer electronic configuration remains the same.
The outer electrons that are lost, gained, or shared are called valence electrons, and the inner
electrons are called core electrons. For the most part, the valence electrons are important in determining
the nature of the bonding and, hence, the structure and properties of the materials.

 Bonding

When two atoms or ions are within atomic distances of each other, distances of 0.5-3.OA, bonding
may occur between the atoms or ions. The resulting reduction in energy due to an attractive force
leads to the formation of polyatomic gas molecules, liquids, and solids. If the energy of the bonds
is large (75-275 kcal/mol), primary bonds are formed—metallic, ionic, or covalent. If the energy of
the bond is smaller (1-10 kcal/mol), secondary bonds are formed—van der Waals and hydrogen. In
addition, combinations of bond types, such as a mixture of ionic and covalent bonds, may occur.

Metallic Bonding

In a metallic crystal, an ordered arrangement of nuclei and their electrons is embedded in a cloud of
valence electrons, which are shared throughout the lattice. The resulting bonding is a nondirectional
primary bond. Since the binding energy of the valence electrons is relatively small, the mobility of
these electrons is high and creates high electrical and thermal conductivity. The atoms are approximately
spherical in shape as a result of the shape of completed inner shell. Examples of metals are
Cu, Au, Ag, and Na.

Ionic Bonding

The strongest type of bonding between two oppositely charged particles is called ionic bonding. The
positively charged ions (cations) attract as many negatively charged ions (anions) as they can and
form ionic bonds. The primary bond formed is nondirectional if the bonding is purely ionic. Li+ and
F~ in LiF form predominately ionic bonds. In general, since the electrons are strongly bonded,
electrical and thermal conductivities are much smaller than in metals and, thus, ionic bonded materials
are classified as insulators or dielectrics.

Covalent Bonding

Covalent bonding results from an overlap or sharing, not from gain or loss of valence electrons. A
net reduction of energy as a result of each atom's completing the other's orbital also results in a
primary bond, but it is directional. The directionality is a result of the shape of the orbitals involved
in the bonding. When C is covalently bonded to four other C's in diamond, the bonding is purely
covalent and the configuration of these four bonds is tetrahedral. When B, however, is bonded to
three other B's, a triangular configuration is formed. Organic polymers and diatomic gases such as
Cl2 are typical examples of covalent bonding. As a result of the strong bonding of the valence
electrons, these materials, for the most part, have low electrical and thermal conductivity.

Van der Waals and Hydrogen Bonding

Van der Waals bonds are secondary bonds, the result of fluctuating dipoles, due to the fact that at an
instant of time the centers of positive and negative charge do not coincide. An example is an inert
gas such as Ar, which below -19O0C forms a solid as a result of these weak attractive forces. Similar
weak forces exist in molecules and solids. Hydrogen bonds are also secondary bonds, but they are
the result of permanent dipoles. For example, the water molecule, H2O, is nonlinear and the bonding
between H and an adjacent O in water results in H2O being a liquid above O0C a 1 ami pressure
rather than a gas, as is the case for other molecules of comparable molecular weight....................

Friday 26 July 2013

METRIC - Stud Bolt to Nut Chart




This metric stud bolt to nut table is meant to help determine the correct size bolt or nut for your purpose.  Definitions of terms are located below the chart.  Use the dimensions of your bolt to determine the appropriate size nut.  Have questions? 
See definitions below.
 Bolt
 COARSE Thread
      FINE Thread
NOM.
PITCH
DIAMETER
PER
 NUT
NOM.
PITCH
DIAMETER
PER
 NUT
DIA.
mm
mm
inch
inch
Size
DIA.
mm
mm
inch
inch
Size
M10
1.5
10
.03937
17
17
M16
1.5
16
.6299
17
24
M12
1.75
12
.04724
14-1/2
19
M18
2
18
.7087
12-3/4 
27
M14
2
14
.5512 
12-3/4
22
M18
1.5
18
.7087
17
27
M16
2
16
.6299
12-3/4
24
M20
2
20
.7874
12-3/4
30
M18
2.5
18
.7087
10-1/4
27
M20
1.5
20
.7874
17
30
M20
2.5
20
.7874
10-1/4
30
M22
2
22
.8661
12-3/4
32
M22
2.5
22
.8661
10-1/4
32
M22
1.5
22
.8661
17
32
M24
3
24
.9449
8-1/2 
36
M24
2
24
.9499
12-3/4
36
M27
3
27
1.0630
8-1/2
41
M24
1.5
24
.9499
17
36
M30
3.5
30
1.1811
7-1/4
46
M27
2
27
1.0630
12-3/4
41
M33
3.5
33
1.2992
7-1/4
50
M27
1.5
27
1.0630
17
41
M36
4
36
1.4173
6-1/4
55
M30
2
30
1.1811
12-3/4
46
M39
4
39
1.5354
6-1/4
60
M30
1.5
30
1.1811
17
46
M42
4.5
42
1.6535
5-1/2
65
M33
2
33
1.2992
12-3/4
50
M45
4.5
45
1.7717
5-1/2
70
M33
1.5
33 
1.2992
17
50
M48
5
48
1.8898
5-1/4
75
M36
3
36
1.4173
8-1/2
55
M52
5
52
2.0472 
5-1/4
80
M36
1.5
36
1.4173
17
55
M56
5.5
56
2.2047
4-1/2
85
M39
3
39
1.5354
8-1/2
60
M60
5.5
60
2.3622
4-1/2
90
M42
3
42
1.6535
8-1/2
65
M64
6
64
2.5197 
4-1/4
95
M45
3
45
1.7717
8-1/2
70
M68
6
68
2.6772
4-1/4
100
M48
3
48
1.8898
8-1/2
75
M72
6
72
2.8346
4-1/4
105
M52
3
52
2.0472
8-1/2
80
M76
6
76
2.9921
4-1/4
110
M56
4
56
2.2047
6-1/4
85
M80
6
80
3.1496
4-1/4
115
M60
4
60
2.3622
6-1/4
90
M85
6
85
3.3464
4-1/4
120
M64
4
64
2.5197 
6-1/4
95
M90
6
90
3.5433 
4-1/4
130
M68
4
68
2.6772
6-1/4
100
M100
6
100
3.9370
4-1/4
145
M72
4
72
2.8346
6-1/4
105
M110
6
110
4.3307
4-1/4
155
M76
4
76
2.9921
6-1/4 
110
M125
6
125
4.9212
4-1/4
180
M80
4
80
3.1496
6-1/4
115
M140
6
140
5.5118
4-1/4
200
M85
4
85
3.3464
6-1/4
120
M160
6
160
6.2992 
4-1/4
230
M90
4
90
3.5433
6-1/4
130
M100
4
100
3.9370 
6-1/4
145
M110
4
110
4.3307
6-1/4
155
M125
4
125
4.9212
6-1/4
180
DEFINITIONS
--NOMINAL DIAMETER (NOMINAL BOLT DIAMETER)
The diameter equal to the external diameter of the threads or the overall diameter of the part.  (Nominal diameter is more of a label than a size. For example, a bolt and nut may be described as being ½” diameter. But neither the external threads of the bolt nor the internal threads of the nut are exactly .500 in diameter. In fact, the bolt diameter is a little smaller and the nut diameter a little larger. But it is easier to specify the components by a single size designation since the bolt and nut are mating components.)
--PITCH (THREAD PITCH)
Pitch is the distance from the crest of one thread to the next or the distance from one thread groove to the next, measured from crest to crest.  Pitch is also described as the number of threads per inch.
--DIAMETER (BODY DIAMETER)
The smallest or largest pitch diameter that fits onto a screw or into a nut, including all of the form deviations such as lead, thread angle, taper, and roundness. Functional diameter is a measure of the ability to assemble the thread.
--THREAD (BOLT THREADS)
A raised, helical rib or ridge around the interior or exterior of a cylindrically shaped object. Threads are found on screws, nuts, and bolts.
--THREADS PER INCH
The decimal equivalent of the number of threads in an inch.
--COARSE THREADS & FINE THREADS
Coarse threads are those with larger pitch (fewer threads per axial distance), and fine threads are those with smaller pitch (more threads per axial distance). Coarse threads have a larger threadform relative to screw diameter, whereas fine threads have a smaller threadform relative to screw diamete