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Strain Chapter 12

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Title: Strain Chapter 12


1
StrainChapter 12
2
Components of homogeneous strain of a square (A)
(straight lines remain straight parallel lines
remain parallel strain the same at all
points)change in area (B) change in shape (C,
D).E and F show inhomogeneous deformation
3
Relationship of s, e, and ? to the geometry of
the strain ellipseR 1sn r/R ren
(r-R)/R ?R/R ?R
4
The area and volume strains - Deformation of a
unit circlee1 ? e2 ? e3 and s1 ? s2 ? s3Area
stretch sA a/A and vA v/V Area extension
eA(a-A)/A sA-1 and eV (v-V)/V sV-1 Initial
rectangle of sides L1 L3 deforms to l1 l3sA
a/A l1l3 /L1L3 s1s3 (1e1)(1e3)sV l1l2l3
/L1L2L3 s1 s2s3 (1e1)(1e2)(1e3)eA
sA-1(1e1)(1e3)1 e1e3e1e3 e1e3 (small
strain)eV sA-1 (1e1)(1e2)(1e3)1
e1e2e3 (small strain)
5
Strain ellipse and Inverse strain ellipse
6
Undeformed and deformed oolitic limestone
7
Structures depend on the orientation of the layer
relative to the principal stretches and value of
s2
8
Uniaxial strainTwo principal stretches are equal
to 1
9
Pure ShearConstant volume, plane strain in which
the principal axes of strain do not rotate by
deformations1gt1 s2 1 s3lt1sV 1 s1 1/s3
10
Simple ShearConstant volume, plane strain in
which the principal axes of strain rotate by
deformation. The displacement of all material
particles is strictly parallel to the shear
planes1gt1 s2 1 s3lt1sV 1 s1 1/s3
11
Types of homogeneous deformation of a cube,
circle, and sphere
12
Decomposition of an arbitrary homogeneous strain
into a pure strain, a rigid rotation, and a rigid
translation
13
Particle motions during progressive pure shear
and simple shear
14
States of strain during a steady progressive pure
shear
15
States of strain during steady progressive simple
shear
16
Geometry of finite and instantaneous strain
ellipses
17
The histories of progressive deformation for
competent layers oriented within the different
sectors of the strain ellipse (see last slide)
18
Shortened boudins
19
Distributions of sectors of stretch and stretching
20
Folding of a layer and simultaneous boudinage of
a perpendicular layer
21
Flinn Diagram for constant volume
deformationk(a-1)/(b-1)
22
Flinn Diagram plots of the line for plane strain
at various values of he volumetric stretch
23
Logarithmic Flinn diagram for various amounts of
volumetric stretch sV s1s2s3 strain
eVsA-1e1e2e3
24
Strain Tensor Components in 3D
25
Displacement vector connects the position X of a
material particle in the undeformed state to its
position in the deformed state. (B) The vectors
for neighboring points are different
26
Components of the infinitesimal strain for
two-dimensional strain
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