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CRITICAL RESOLVED SHEAR STRESS

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Al Baehaqi Aliyan Rami

Academic year: 2024

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SLIP SYSTEMS

Dislocations do not move with the same degree of ease on all crystallographic planes and directions

There are preferred planes (slip planes) and preferred directions (slip directions)

Slip planes are planes with high planar density of atoms, and slip directions are lines with high linear density

Slip system: the combination of slip plane and slip direction

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SLIP SYSTEM: EXAMPLES

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• FCC (Al, Cu, Ni, Ag, Au)

– Close packed planes: {111}, e.g., ADF

– Close packed directions: <110>, e.g., AD, DF, AF

– Slip system: {111}<110> (12 independent slip systems)

• BCC (Fe, W, Mo): {110}<111> (12 independent slip systems)

• HCP (Zn, Cd, Mg, Ti, Be): 3 independent slip systems

• FCC & BCC metals: ductile, HCP metals: brittle

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• Single crystals easy to treat; can generalize to polycrystals later

• Regardless of what type of external stress is applied to a material, plastic deformation or dislocation motion occurs due to a shear stress

• Some component of the applied stress has to be a shear stress on a slip plane and along a slip direction

• This component is called the resolved shear stress

SLIP IN SINGLE CRYSTALS

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 All plastic deformation by slip is due to shear stresses

 The shear stress resolved onto the slip plane is responsible for slip

 When the Resolved Shear Stress (RSS) reaches a critical value →

Critical Resolved Shear Stress (CRSS) →

plastic deformation starts (The actual Schmid’s law)

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Schmid’s law

Slip is initiated when CRSS is a material parameter Yield strengh of a single crystal

RSS CRSS

  

CRSS y

Cos Cos

 

 

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RESOLVED SHEAR STRESS

Applied tensile stress:  = F/A

A F

F

slip

direction

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Resolved shear stress: R=Fs/As

As

 R

 R

Fs

slip

direction slip plane normal, ns

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Relation between

 and  R

 R = Fs/As

Fcos  A /cos 

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F 

Fs

slip

direction

ns 

As A

 

  cos cos

cos /

cos 

 A F

R

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CRITICAL RESOLVED SHEAR STRESS (CRSS)

• Condition for dislocation motion:

• Crystal orientation can make it easy or hard to move disl.

R

 

CRSS

R

  cos  cos 

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R

= 0

=90°

R

= /2

=45°

=45°

R

= 0

=90°

• Maximum possible R = /2; thus y = 2CRSS

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BCC EXAMPLE

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• Slip system: {110} <111>

 = 45 degrees

 = tan

-1

(a2/a) = 54.7 degrees

• From which  or  can be calculated if one of them is

specified

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DISL. MOTION IN POLYCRYSTALS

• Slip planes & directions (, ) change from one crystal to another.

• R will vary from one crystal to another.

• The crystal with the largest R yields first.

• Other (less favorably oriented) crystals yield later.

• Polycrystalline materials generally stronger than single crystals, due to geometric constraints & the requirement of larger stresses for yielding

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Adapted from Fig. 7.10, Callister 6e.

(Fig. 7.10 is courtesy of C. Brady, National Bureau of Standards [now the National Institute of Standards and Technology, Gaithersburg, MD].)

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• Latihan soal

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Home work

Jelaskan tentang perbedaan SLIP vs TWINNING

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