Point defects
only extend over a few atomic spacing
Point defect occur at the latticepoints or their vicinities.
Increase of electricalresistivity in metals.
Increase of electricalconductivity in ionic crystals.
Diffusion in solids.
Change in mechanical properties.
Elongation due to the defect andthermal lattice expansion.
Kind of point defects
Vacancy
INTERSTITIAL
SUBSTITUTIONS
COLOUR CENTRE
POINT DEFECTS: VACANCY
In a Schottky defect an atom ismissing from one of the latticesites. It leaves a “vacancy”.
A neighbouring atom diffusesinto the vacancy, so the vacancymay diffuse into the crystal.
The surrounding atoms movearound and hence distort thecrystal structure.
Formula Defect concentration
POINT DEFECTS: INTERSTITIAL
When an extra atom is forcedinto the lattice we speak of aninterstitial defect.
The defects can occur afterion or neutron irradiation.
Like in the case of a vacancythe surrounding will react witha distortion of the lattice.
If this atom originally came froma lattice site, leaving a vacancy,it is a Frenkel defect.
POINT DEFECTS: SUBSTITUTIONS
In a Substitutional defect aforeign atom replaces a hostatom on a lattice site.
Again the surrounding distorts.
Usually an atom substitutes at alattice site of similar atomic size.
Substitutional defects can beused to strengthen materials.
A colour centre is a defect that causes a transparent crystalto absorb in the visible region of electromagnetic waves andhence becomes coloured.
STACKING FAULTS
A stacking fault refers to aninterruption in the stackingsequence of a crystal structure.
This may refer to a missing oradditional layer or atoms.
It causes additional strain.
TWINNING
Crystal twinning occurswhen two crystals share the same crystal lattice.
Easily observed by optical microscopy.
Most likely to occurin hcp crystals
EDGE DISLOCATIONS
additional or missing plane ofatoms results in displacement.
The material above the slipplane moves relative to thatbelow, producing strain.
Dislocations run through theentire crystal and eitherterminate at the surface orform a closed loop.
Often denoted by the symbol ⊥
b vertical to displacment
SCREW DISLOCATIONS
In a screw dislocationthe boundary of theslipped region lies parallelto the direction of slip.
The atoms rearrangearound the dislocation inthe form of a helix.
This also causesstrain in the material.
b parallel to Dislocation
A screw dislocation involves shearing oneportion of a perfect crystal with respect toanother portion on one side of a line (AB).
Screw dislocation aid crystal growthbecause the newly arriving atom canattach to two or three atoms instead ofone atom and thereby form more bonds.
BURGERS VECTOR
describes the direction and amount of slip
How to determine the burger vector:
In a perfect crystal trace a closed loopusing multiple of atomic jumps.
Repeat the same steps in a real crystal.
The extra vector needed to close the loopis the Burgers vector
For edge dislocations b is perpendicular to the dislocation line.
For screw dislocations b is parallel to the dislocation line.
DISLOCATION DENSITY
is the total length of dislocation line in a unitvolume
DEFORMATION
Deformation of crystals occurs by multiplication of dislocations.
If the source of a defect lies in the centre of the crystal rather than at the surface it is referred to as a Frank-Read-Source.
PLASTIC DEFORMATION
Plastic deformation is produced by dislocation motion.
The slip systems of the material depend on the type of lattice.
Slip plane FCC
the slip planes are (111) and
the slip directions are <110>
Slip plane HCP
the slip planes are (0001) and
the slip direction is <112_0>
Slip plane BCC
slip planes are (110), (112) and (123) and
the slip direction the body diagonal <111>
ideal strength
is the stress at whichthe atomic bonds break
For glasses and ceramics:
STRESS VS STRAIN CURVE
WORK HARDENING/Cold Working/strain hardening
After elastic deformation materialsreturn to their original length (1).
Further increase in stressresults in plastic deformationafter which the material doesnot return to its original length (2).
When stress is reapplied there is anew short elastic region after whichplastic yielding occurs again (3).
The material is hardened by the initialamount of plastic deformation
WORK HARDENING STAGE 1: EASY GLIDE
In the first stage dislocation movefreely over large distances.
Dislocation multiplication andinteraction lead to an increase instress for further deformation.
At the end of stage 1 dislocationsstart to hinder each other.
Since there is only one glide planein hcp crystals, the basal plane,a hcp crystal continues todeform until it fractures.
WORK HARDENING STAGE 2: LINEAR HARDENING
Resistance to dislocation motionoccurs in stage 2 of work hardening.
This occurs due to dislocationsrepelling each other or piling up.
Vacancies and interstitial defectsoccur when dislocations cutthrough a forest of dislocations.
The process of work hardeningcontinues at this stage
WORK HARDENING STAGE 3: CROSS SLIP
At this stage the stress is highenough top avoid obstacles.
When a screw dislocation movesfrom one slip plane to another itis referred to as cross slip.
Cross slip can occur in FCC and BCC crystals which have several equivalent slip planes.
The rate of work hardening decreases.
WORK HARDENING: THE YIELD DROP
The yield drop in a bcc crystals is notan intrinsic property but depends onthe testing procedure.
Rapid dislocation multiplication leadsextension more quicklythan the tensile machine.
Occurs due to impurity lockingin BCC crystals
OROWAN HARDENING
Precipitates can impedethe motion of dislocations.
The precipitate acts as a pinning pointfor the dislocation.
Hardening by precipitatesis referred to as Orowan hardening.
Examples areAl hardened by Cu,and steel
GRAIN BOUNDARY STRENGTHENING
Metals are polycrystalline,they consist of small crystals called grains.
Grain boundaries obstructthe motion of dislocations.
Grain boundary strengtheningis also referred to as Hall–Petch strengthening
The yield strength is proportionalto the Petch constant k anddepends on the grain size D.
BRITTLE FRACTURE
Some materials, such as glass,do not exhibit plastic deformation.
These brittle materialscrack under stress.
Cracks occur at inclusions,dislocations grain boundaries.
Grain boundaries are obstaclesto fracture propagation.
Therefore materials with smallcrystallites are stronger.
RESISTIVITY
Around room temperature theresistivity 𝜌 of a material increaseslinearly with temperature (T).
The conductivity 𝜎 is proportional tothe mean free path 𝜏 betweencollisions.
At moderate temperatures themean free path is limited bythermal vibrations of the lattice.
At low T the mean free path isdetermined by defects and impurities
LATTICE VIBRATIONS
Thermal energy causes thelattice of a crystal to vibrate.
Only certain energy values areallowed; they are quantized.
A phonon is a quantumof vibrational energy.
This is analogous to a photonbeing the quantum of electro-magnetic radiation.
MATTHIESSEN RULE
It states that the resistivity ρ of a metal is composed of a temperature-dependent term that arises from the scattering of electrons by the lattice vibrations (phonons) and a temperature-independent term that arises from the scattering of electrons by defects.
ρ(T) = ρ[Phononen](T) + ρ[Defekte]
Scattering of electronsoccurs of phonons and impurities
The temperaturedependence of resistivity:ρ[T] = AT
Formular when resistivity increases
where 𝜌𝑝 is the increase in resistivity per point defect.
NORDHEIM‘S RULE
MATTHIESSEN AND NORDHEIM RULES
GRANULAR RESISTIVITY
Zuletzt geändertvor 2 Jahren