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Measures of Central Tendency: Mean, Median and Mode
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2. (a) The state of stress at position x in a fluid at rest (say, a liquid) can be characterized by
where p is the [fluid] pressure at x. Assume that the liquid has a constant mass density,
ρ, and assume further that the fluid is subject to a gravitationallyinduced body force
loading (per unit mass) of magnitude
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3. where the cartesian basis vector e3 points “up.” Let atmospheric [air] pressure at the
surface of the liquid be p0 (elevation of air/liquid surface: x3 = 0) . Using the
appropriate equilibrium equations, show that the pressure at generic elevation x3 < 0 is
given by
(b) A long, straight dam holds the water in place. The dam extends along the e2
direction, and the planar surface of the dam makes an angle of θ with respect to the
vertical, as shown. At a point on the liquid/dam interface that is at elevation x3 < 0: 1.
evaluate the traction vector exerted by the dam on the fluid surface. The outward
normal vector on the liquid is nl, as shown.
2. explain why the traction vector acting on the surface of the dam (that is, the traction
exerted by the fluid on the surface element of the dam) is equal and opposite to the
previouslydetermined traction vector in part (1). The outward normal to the surface of
the dam is nd, as shown.
3. use the traction vector from part (2) to express 3 linear equations involving the
cartesian stress components σij in the dam at elevation x3.
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4. Problem 2 The isotropic linear thermal/elastic constitutive relations can be expressed
in the compact notation
Here the total strain components (�ij ) are expressed in terms of the stress
components (σij ) and the temperature change (ΔT).
Derive a consistent expression for the stress components, σij , in terms of the strain
components and the temperature change. Evaluate those stress components when
the strain tensor is
and the temperature change is ΔT = 100 C. Material properties include E = 210 GP a,
ν = 0.3, and α = 12 × 10−6/ C
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5. Problem 3
The surface x3 = 0 of a large, flat body made of a material having elastic Young’s modulus
E, Poisson ratio ν, and coefficient of thermal expansion α is subjected to a rapid thermal
shock. 1 The results in either case can be summed up by the following observations:
• In a thin layer on and immediately below the surface x3 = 0:
– the temperature rapidly changes by an amount “ΔT”, where ΔT ≡ Tafter −Tbefore ;
– the surface x3 = 0 remains tractionfree.
• In the thick substrate beneath the surface layer: .
– the temperature changes negligibly: ΔT = 0; .
– the total strain remains very small: ij = 0ij .
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6. Assuming that the response of the material during the shock is isotropic linear
thermal/elastic: 1. Argue why the inplane strain components 11, 22, and 12 in the thin
surface layer should match the corresponding values in the substrate; namely, 11 = 22
= 12 = 0. (Hint: what would happen to the displacement field components ui if any of
these strain components were discontinuous across the interface separating surface
layer from substrate?)
2. Evaluate all components of the stress tensor σij in the substrate.
3. Evaluate all components of the stress tensor σij in the thin surface layer. Give
“physical” reasons to justify the sign of any nonzero stress components, relative to the
sign of ΔT.
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7. 4. Evaluate all components of the strain tensor ij in the surface layer. Give “physical”
reasons to justify the sign of any nonzero strain components, relative to the sign of ΔT.
5. Suppose that yielding of the material begins whenever the Mises stress measure σ
reaches the value σy, which is the tensile yield strength of the material. Calculate the
maximum value of Δ| | T which can be applied to the surface layer without having the
Mises stress exceed the value “σy”.
Recall that in an isotropic linear thermal/elastic material, the relation between
temperature change, ΔT, stress components, σij , and strain components, ij , is
You may consult your [correct] answer to Problem 2, above, in order to find an
appropriate “inverted” form giving the stress components σij in terms of the strain
components ij and the temperature change, ΔT
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8. Note: In this and in many other problems, you have information about some (but not
all!) of the stress components, and about some (but not all!) of the strain components.
In this case, you must engage in “handtohand combat” with the set of linear equations
comprising the stress/strain/temp erature relations, obtaining new expressions for those
components that you do not know, a priori, in terms of those components that you do
know .....
Problem 4 (30 Points) The Mises equivalent tensile stress is a nonnegative scalar
measure of a multiaxial stress state, σij , that is used to asses the proximity to yielding in
ductile metals and polymers at sufficiently low temperatures. Let the uniaxial tensile
yield strength of a material be given by σy; then, if that material is under a general multi-
axial stress state σij whose Mises tensile equivalent stress, σ¯, satisfies
no plastic deformation is forthcoming: the material will respond elastically. Should σ¯ = σy,
plastic deformation under the multiaxial stress state is imminent. Thus, it is important to be
able to calculate the Mises tensile equivalent stress. The most fundamental definition of ¯σ
first involves calculation of the stress deviator tensor corresponding to σij . Components of
the stress deviator are defined by
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9. The Mises equivalent tensile stress is given by
Clearly, it is a “root mean square” measure of the stress deviator tensor components
(square root of the sum of the squares of the components).
• Show that, for uniaxial tensile/compressive stress of magnitude “Σ” along any
coordinate axis, σ¯ = Σ . | |
• Show that addition or subtraction of a uniform hydrostatic pressure to a given stress
state, σij , does not affect the value of ¯σ.
• Show that, in plane stress, where the only nonzero components of the stress tensor are
σ11, σ22, and σ12 = σ21, the Mises tensile equivalent stress satisfies
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10. • In 2.001, you may have considered an alternative criterion for the onset of plastic flow
under multiaxial stress states, termed the maximum shear stres, or Tresca yield criterion.
In the special case of plane stress given above, the Tresca yield condition comprises the
following sets of constraints:
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11. Show that, in the case of pure shear, σij = 0 except σ12 = σ21 = τ = 0, the Mises yield
criterion predicts that yield will occur when |τ | = σy/ √3, while the Tresca yield criterion
predicts yielding when | | τ = σy/2. Thie difference is only ∼ 15%, and is the largest
possible difference in the predictions of yielding between the Tresca and Mise criteria.
In general states of stress, computation of the Mises equivalent tensile stress measure is
straightforward, but the generalization of the Tresca yield criterion to general states of
strees requires more calculations. Also, careful experimentation under multiaxial stress
(e.g., using thinwalled tubes under combinations of tension/compression, torsion, and
internal pressure) gives results generally closer to the Mises criterion.
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12. All shear stresses are zero. Furthermore, the gravitational body force loading b has one
non-zero component only, in the direction of e3. Therefore, from the third equilibrium
equation we get:
We also know that σ33(x) = −p(x) and b3 = −g. We can substitute these into Equation 4
and integrate both sides with respect to x3
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13. Note that p is only a function of x3.
(b) 1. The traction vector on a surface can be found by multiplying the stress with the unit
outward normal vector on that surface. In this case, the normal vector is
The traction vector is then
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14. 2. Action and reaction, forces need to balance at the interface.
which gives 3 linear equations involving σij
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15. Problem 2
The procedure is similar to what was discussed in class for elastic constitutive relations
without thermal effects. The idea is to eliminate 3 from the given equation and k=1 σkk
solve for σij . To do this, take the sum of both sides of the given equation as follows
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16. The indexes can be anything in this case (i, j, or k) and don’t affect the result. j 3 =1 δjj is
simply the sum of the diagonal elements of the (3x3) identity matrix. Thus, j 3 =1 δjj = 3.
Therefore, the equation becomes
Solving for 3 yields
We can now substitute this expression into Equation 14 and solve for σij to get
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17. To evaluate the stress components for the given data, use any commercially available
software to carry out the matrix operations, such as MATLAB. The stress tensor is
This equation can be inverted to give
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18. 1. The strain components are determined by the derivatives of displacement
components. Since the displacement should be continuous in the interface
separating surface layer from substrate, the in-plane strain components in the thin
surface layer should correspond to those in the substrate, too. Therefore, 11 = 22 =
12 = 0.
2. The problem stipulates that the thick substrate undergoes negligible total strain and
. . temperature change. It means ΔT = 0 and ij(substrate) = 0ij . The constitutive
equation (3) gives the relation between stress components and strain components. In
the equation, σij(substrate) can be calculated by substituting ij(substrate) and
ΔT(which are all zeros).
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19. 3. We know that the surface layer has a boundary condition at surface x3 = 0 which
remains traction-free (tn = 0).
The in-plane components 11, 22, and 12 are zero. By the equation (3),
Invoking the symmetry of the stress tensor, σij = σji
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20. In order to justify the sign of the non-zero stress components, σ11 and σ22, we can
imagine that, when the temperature increases, the surface layers tends to extend while
the substrate tends to prevent it from deforming by shrinking it. Therefore the non-zero
stress components would be compression stresses. And similarly, when the temperature
decreases, the two in-plane components are tensile stresses. The non-zero components
σ11 and σ22 always have opposite sign from that of the change of temperature(ΔT).
4. By the equation (2) and the in-plane strain continuity( 11 = 22 = 12 = 0 ),
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21. On solving equation (9) and (10),
Since all the components of the stress tensor in equation (8) are known, the strain
tensor can be calculated by the equation (2).
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22. 5. The Mises equivalent stress σ is given by
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23. To prevent yielding, it is required that σ < σy.
Problem 4
In uniaxial loading, only one stress component is non-zero. Let’s assume uniaxial
loading in the 1-direction. The stress tensor is then
The stress deviator tensor is then
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24. The double summation in the Mises stress equation is calculated by squaring each
component of the deviatoric stress tensor and adding them all up. More specifically,
Therefore, the Mises stress becomes
Hydrostatic pressure only has normal components, ie it doesn’t have shear
components. As a result, the stress components that are affected by the
addition/subtraction of a uniform hydrostatic pressure p are σ11, σ22 and σ33, which
become in the case of addition, σ11 + p, σ22 + p and σ33 + p accordingly. The
deviatoric stress components are then
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25. which is equal to the original stress deviator tensor. In plane stress
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26. Thus, the stress deviator tensor is
Then, the Mises stress becomes
After some manipulation, we get
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27. Finally, in the case of pure shear, the stress tensor is
The stress deviator tensor is identical to the stress tensor since pure shear does not
cause volumetric changes (only shape changes). Thus, σ = σdev. The Mises stress is
As mentioned in the problem statement, yielding occurs when σ¯ = σy. Therefore, τ
= σy √ . 3 | Furthermore, the only non-zero variable in the Tresca condition is σ12 =
τ . Thus, the first inequality yields |τ | ≤ σ 2 y and the second one τ ≤ σy. Thus, the
Tresca condition predicts yielding when |τ | = σ 2 y .
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