Transcript Document

Finite strain II
We have learned how to quantify the strain of each individual line.
Often, there are several material lines, oriented at different
directions. In that case we would like to describe the changes of
the body as a whole.
Finite strain II: The strain ellipse
A simple geometric object that describes the orientation of lines at
all directions is a circle. A circle undergoing homogeneous strain
becomes an ellipse. Likewise, a sphere becomes ellipsoid
following deformation.
Finite strain II: The strain ellipse
The principal axes of strain: Are the long and the short axes of the
strain ellipse. Lines parallel to the principal axes undergo no shear
strain.
Principal strains: Are the stretch along the principal axes.
In 2D : S1> S3
In 3D : S1 > S2 > S3
The principal axes and the principal strains are the Eigenvectors
and the Eigenvalues (squared) of DTD, respectively.
Finite strain II: The strain ellipse
• Principal axes are
perpendicular lines that were
perpendicular prior to the
deformation.
• Lines parallel to the principal
axes undergo no shear strain.
Finite strain II: The strain ellipse
Non-unique strain path: Different strain paths may produce
identical strain ellipse. For example:
Finite strain II: The strain ellipse
Non-commutability of strain: In general, the order at which strains
and rotations are superposed makes a difference in terms of the
final product. For example:
Finite strain II: Infinitesimal versus finite strain ellipses
The finite strain may be thought as the sum of many infinitesimal
strains. At any stage in the deformation, there are two strain
ellipses that represent the strain of the rock.
• The finite strain ellipse: represents the total deformation.
• The infinitesimal strain ellipse: represents the instantaneous
strain that the particle feels.
(show a computer simulation)
Finite strain II: Infinitesimal versus finite strain ellipses
• Coaxial deformation: If the axes of the finite and infinitesimal
strain ellipse remain parallel throughout the deformation.
• Non-coaxial deformation: if the axes of the finite and infinitesimal
strain ellipse are not parallel.
We have seen that while progressive pure shear is coaxial,
progressive simple shear is non-coaxial.
Finite strain II: Infinitesimal versus finite strain ellipses
Lines of no finite elongation (LNFE): Two lines for which the final
and initial lengths are equal.
• f+ : lines within that sector are longer in the final state.
• f-: lines within that sector are shorter in the final state.
Finite strain II: Infinitesimal versus finite strain ellipses
Lines of no infinitesimal elongation (LNIE): Two lines for whose
lengths remain unchanged during the next increment of
infinitesimal strain.
• i+ : lines within that sector will become infinitesimally longer
during the next infinitesimal strain.
• i-: lines within that sector will become infinitesimally shorter
during the next infinitesimal strain.
Finite strain II: Infinitesimal versus finite strain ellipses
Note that:
• The LNIE are perpendicular.
• The angle between the LNIE and the principal axes of the
infinitesimal strain ellipse is equal to 45 degrees.
Finite strain II: Infinitesimal versus finite strain ellipses
In the most general case, the superposition of the finite and the
infinitesimal strain ellipse may form 4 fields:
• (f-,i-) lines are shorter than they started, and they will continue to
shorten in the next increment.
• (f-,i+) lines are shorter than they started, but will begin to
lengthen in the in the next increment.
• (f+,i+) lines are longer than they started, and they will continue to
lengthen in the next increment.
• (f+,i-) lines are longer than they started, but will begin to shorten
in the next increment.
Finite strain II: Infinitesimal versus finite strain ellipses
Finite strain II: Infinitesimal versus finite strain ellipses
So far we have dealt with straight lines. Let's examine the case of
curved lines and lines of finite thickness (i.e., beds).
(show computer animation)
Finite strain II: homogeneous versus heterogeneous strains
The deformation is homogeneous if:
• Straight lines remain straight.
• Parallel lines remain parallel.
Finite strain II: homogeneous versus heterogeneous strains
Otherwise, the deformation is heterogeneous.
Often it is a matter of scale, i.e. the deformation may be
homogeneous on a small scale, but heterogeneous on a broader
scale (e.g., a fold).
Finite strain II: Continuous versus discontinuous
Continuous: when strain vary smoothly throughout the volume.
Discontinuous: abrupt changes in the strain distribution, i.e.,
faults, joints, etc.
Mathematically, the treatment of discontinuous deformation is
much more complicated.