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These are the Lecture Slides of Material Science for Engineers which includes Structure of Wood, Moisture Content, Density of Wood, Mechanical Properties of Wood, Expansion and Contraction of Wood, Concrete Materials, Properties of Concrete etc. Key important points are: v
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mechanical (MEMS)
systems-Airbag sensors
Figure 2.
Section 2.
The Structure of Materials:
Technological Relevance
Level of Structure Example of Technologies
Atomic Structure Diamond – edge of cutting tools
Atomic Arrangements: Lead-zirconium-titanate Long-Range Order [ Pb ( Zr x Ti 1-x )] or PZT – (LRO) gas igniters
Atomic Arrangements: Amorphous silica - fiber Short-Range Order optical communications (SRO) industry
Figures 2.2 – 2.
Table 2.1 Levels of Structure
Section 2.
The Structure of the Atom
The atomic number of an element is equal to the number of electrons or protons in each atom.
The atomic mass of an element is equal to the average number of protons and neutrons in the atom.
The Avogadro number of an element is the number of atoms or molecules in a mole.
The atomic mass unit of an element is the mass of an atom expressed as 1/12 the mass of a carbon atom.
Calculate the number of atoms in 100 g of silver.
Example 2.1 SOLUTION
The number of silver atoms is =
mol g
=5.58 1023
Example 2.
Calculate the Number of Atoms in Silver
Example 2.2 SOLUTION
The radius of a particle is 1.5 nm.
Volume of each iron magnetic nano-particle
= (4/3)(1.5 10 -7^ cm)^3
= 1.4137 10 -20^ cm^3
Density of iron = 7.8 g/cm^3. Atomic mass of iron is 56 g/mol.
Mass of each iron nano-particle
= 7.8 g/cm^3 1.4137 10 -20^ cm^3
= 1.102 10 -19^ g.
One mole or 56 g of Fe contains 6.023 1023 atoms, therefore, the number of atoms in one Fe nano-particle will be 1186.
Example 2. Dopant Concentration In Silicon Crystals
Silicon single crystals are used extensively to make computer chips. Calculate the concentration of silicon atoms in silicon, or the number of silicon atoms per unit volume of silicon. During the growth of silicon single crystals it is often desirable to deliberately introduce atoms of other elements (known as dopants) to control and change the electrical conductivity and other electrical properties of silicon. Phosphorus (P) is one such dopant that is added to make silicon crystals n -type semiconductors. Assume that the concentration of P atoms required in a silicon crystal is 10^17 atoms/cm^3. Compare the concentrations of atoms in silicon and the concentration of P atoms. What is the significance of these numbers from a technological viewpoint? Assume that density of silicon is 2.33 g/cm^3.
Example 2.3 SOLUTION (Continued)
Significance of comparing dopant and Si atom concentrations: If we were to add phosphorus (P) into this crystal, such that the concentration of P is 1017 atoms/cm^3 , the ratio of concentration of atoms in silicon to that of P will be
(5 1022 )/(10^17 )= 5 105. This says that only 1 out of 500,000 atoms of the doped crystal will be that of phosphorus (P)! This is equivalent to one apple in 500,000 oranges! This explains why the single crystals of silicon must have exceptional purity and at the same time very small and uniform levels of dopants.
Section 2.3 The Electronic Structure
of the Atom
© 2003 Brooks/Cole Publishing / Thomson Learning™
Figure 2.9 The complete set of quantum numbers for each of the 11 electrons in sodium
Using the electronic structures, compare the electronegativities of calcium and bromine.
Example 2.4 SOLUTION
The electronic structures, obtained from Appendix C, are:
Ca: 1 s^22 s^22 p^63 s^23 p^6 4 s^2
Br: 1 s^22 s^22 p^63 s^23 p^63 d^10 4 s^24 p^5
Calcium has two electrons in its outer 4 s orbital and bromine has seven electrons in its outer 4 s 4 p orbital. Calcium, with an electronegativity of 1.0, tends to give up electrons and has low electronegativity, but bromine, with an electronegativity of 2.8, tends to accept electrons and is strongly electronegative. This difference in electronegativity values suggests that these elements may react readily to form a compound.
Example 16. Comparing Electronegativities
Section 2.4 The Periodic Table