Overview of Elasticity of Materials/Introducing Stress

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Introduction

We will begin by developing the constitutive equations that describe the relationship between stress, σ, and strain, ε. This is the subset of continuum mechanics that focuses on the purely elastic regime, and in particular, will focus on linear elasticity where Hooke's Law holds true.

Figure 1: (a) The external forces, 𝐏, administered to the body will be transmitted internally. A point on an imaginary slice taken through the body will have force on the surface. (b) The force on this slice can be projected into components acting normal or tangential to the area, A.

The concepts of stress and strain originate by considering the forces applied to a body and its displacement. Beginning with forces, there are two types of forces that can be applied. First, there is surface force which can either be point forces or distributed forces that are applied over a surface. Second, there is body force which is applied to every element of a body, not just a surface (i.e., gravity, electric fields, etc.).

The body of interest has numerous forces acting on it and these are transmitted through the material. At any point inside the body, you can imagine slicing it to observe the forces present on the imagined cut surface, as pictured in Figure 1. These forces are the interactions between the material on either side of the imagined cut. We define the stress at a point in the body as the forces acting on the surface of such an imagined cut.

Figure 2: An infinitesimal cuboid of material with the stresses defined according to the (x1,x2,x3) coordinate system.

As you recall, the stress is defined as the force over the area which it is applied. The force, 𝐏, is a vector quantity, allowing the components to be projected into the normal and tangential directions. As shown in Figure 1, the normal component is defined according to the angle θ, yielding a normal stress σ33=PcosθA. The tangential component of the force, Psinθ, can be further projected into the two orthogonal directions identified in Figure 1 as x1 and x2, yielding two orthogonal shear stresses. This is performed according to the angle ϕ, giving σ31=PsinθcosϕA and σ32=PsinθsinϕA.

Note here that we've defined the coordinate system such that the x3 direction is the direction normal to the cut surface. It is convenient to use (x1,x2,x3) instead of (x,y,z) because it allows us to pass the indexes to the stress and strain quantities. In this example, the normal stress is given by σ33 to specify that the normal stress is applied to the surface with a normal in the x3 direction with a force projected in the x3 direction. The tangential components σ31 and σ32 specify the surface having a normal x3 with forces projected in the x1 and x2 directions, respectively. Cutting an infinitesimal cuboid, the stresses are defined in all three directions as shown in Figure 2. For comparison, the notation used in some textbooks will write normal stresses σx, whereas here we will use σ11. These textbooks also use τ to denote shear stress, such as τxy whereas here we will use σ12. This allows the stress state to be succinctly written in matrix (tensor) form

σ=(σ11σ12σ13σ21σ22σ23σ31σ32σ33)

The imaginary slice taken through point in the body in Figure 1 could have been any plane, but the force would remain the same. This would result in a new definition of the surface normal, and potentially a new expression for the stress. The physical presence of the stress does not change, but the description does, i.e., the coordinate system is modified. The remainder of this section is devoted to expressing the coordinate transformation and analysis of the stresses.

Plane Stress

We will begin by simplifying the picture we are working with. The plane stress condition is observed for a thin 2D object, e.g., a piece of paper, which has no stress out of the plane. This allows us to write σ33=0. Further, there is no shear in the x3 direction such that σ13=σ23=0. For an object in the plane stress condition, our goal is to determine the state of stress at some point for any orientation of the axis.

Figure 3: (a) An area, A, defined for the plane stress condition in which the normal of the area is x1, rotated from x1 by θ. The projection of A into the x1 and x1 directions are shown. (b) The components of the total stress on the area are shown.

For this object, the direction with zero force is x3 coming out of the page and the non-zero stress state in the x1 and x2 directions have components σ11, σ22, and σ12=σ21.

Imagine a new area defined on a plane rotated about x3 such that the normal, defined x1, is related to x1 by θ as shown in Figure 3.

The components of force on the area is determined by the application of the original stresses to the projection of the new area:

F1=σ11Acosθ+σ12Asinθ=S1AF2=σ22Asinθ+σ12Acosθ=S2A Template:Spaces[1 & 2]

where the elements Acosθ and Asinθ are the projection of the A in the original orientation, shown in Figure 3 (a), and S1 and S2 are the total stresses in the x1 and x2 directions, where σ12=σ21. Then, dividing by A yields:

S1=σ11cosθ+σ12sinθS2=σ22sinθ+σ12cosθ Template:Spaces[3 & 4]

Projecting the total stresses shown in Figure 3 (b) into the normal direction in the x1 coordinate yields

σ11=S1cosθ+S2sinθ Template:Spaces[5]

In a similar fashion, we project tangential to the plane and yield

σ12=S2cosθS1sinθ Template:Spaces[6]

Resulting in

σ11=(σ11cosθ+σ12sinθ)cosθ+(σ22sinθ+σ12cosθ)sinθ=σ11cos2θ+σ22sin2θ+2 σ12sinθcosθ Template:Spaces[7]

and

σ12=(σ22sinθ+σ12cosθ)cosθ(σ11cosθ+σ12sinθ)sinθ=σ12(cos2θsin2θ)+(σ22σ11)sinθcosθ Template:Spaces[8]
Figure 4: A new area that is rotated by π2 from the original shown in Figure 3.

It is known that σ12=σ21 and therefore only σ22 needs determining. To do so, we define a new area that is rotated by π/2 relative to our original plane as shown in Figure 4. In this new orientation,

S1A=σ11Acos(θ+π2)+σ12Asin(θ+π2)S1=σ11sinθ+σ12cosθ Template:Spaces[9]

and

S2A=σ22Asin(θ+π2)+σ12Acos(θ+π2)S2=σ22cosθσ12sinθ Template:Spaces[10]

Projecting the total stress in the normal direction yields

σ22=S1cos(θ+π2)+S2sin(θ+πθ)=Sx1sinθ+Sx2cosθ Template:Spaces[11]

Substituting Equations 9 and 10 for S1 and S2 into Equation 11 for σ22 yields

σ22=(σ11sinθ+σ12cosθ)sinθ+(σ22cosθσ12sinθ)cosθ=σ11sin2θ+σ22cos2θ2 σ12sinθcosθ Template:Spaces[12]

The well-known trigonometric identities

cos2θ=cos2θ+12sin2θ=1cos2θ22sinθcosθ=sin2θcos2θsin2θ=cos2θ

are applied to Equations 7, 8, and 12 for σ11, σ12, and σ22 respectively, resulting in

σ11=σ11+σ222+σ11σ222cos2θ+σ12sin2θ Template:Spaces[13]
σ22=σ11+σ222σ11σ222cos2θσ12sin2θ Template:Spaces[14]

and

σ12=σ22σ112sin2θ+σ12cos2θ Template:Spaces[15]

Principal Stress

There are numerous immediate results that come from this derivation, from which we can gain greater insights. One result that comes from the equations for σ is σ11+σ22=σ11+σ22, for all θ. This means that the trace of the stress tensor σ is invariant.

A second result is that the maximum normal stresses and shear stresses vary as a sine wave with period π. Within this oscillation, the normal and shear stresses are shifted by a phase factor that results in (1) the maximum and minimum normal stresses occur when the shear is zero, (2) the maximum and minimum shear stresses are shifted from each other by π/4, (3) the maximum and minimum normal stresses are shifted from each other by π/2, and (4) the maximum and minimum shear stresses are shifted by π/4 from the minimum and maximum normal stresses.

Any stress state can be rotated to yield σ12=σ21=0. This diagonalizes the stress tensor and gives normal stresses that are extreme. In this orientation, the planes are called the principal planes and the normal stresses are called the principal stresses. The directions that give these principal stresses are called the principal axis. As a matter of convention, we define the first principal stress σp1 to be the largest and the sequentially smaller principal stresses to be σp2 and σp3, although here we have limited ourselves to 2D plane stress and only enumerate σp1 and σp2.

We know σ12=0 in the principal orientation, which means we can use Equation 8 for σ12 to determine the angle (θ) needed to rotate the tensor σ into σ which is principal,

0=σ12=σ210=σ12(cos2θsin2θ)+(σ22σ11)sinθcosθ(σ22σ11)sinθcosθ=σ12(cos2θsin2θ)sinθcosθcos2θsin2θ=σ12σ11σ22

Resulting in

tan2θ=2 σ12σ11σ22 Template:Spaces[16]

It is observed graphically by plotting tan2θ in Figure 5 that adjacent roots are each separated by π/2. Furthermore, we can now utilize the Pythagorean Theorem to solve for our principal stresses.

Figure 5: Graphical demonstration that the roots of tan2θ are separated by π2.

For a simple right triangle with hypotenuse c and sides a and b we know

sinξ=bccosξ=actanξ=ba

which can be combined with the Pythagorean Theorem, a2+b2=c2 and Equation 16,

a=σ12b=12(σ11σ22)c=±(14(σ11σ22)2+σ122)12

These can be further combined which yields

sin2θ=±σ12(14(σ11σ22)2+σ122)12 Template:Spaces[17]

and

cos2θ=±12(σ11σ22)(14(σ11σ22)2+σ122)12 Template:Spaces[18]

These equations tell us for a given stress state, σ, what rotation is needed to align σ with the principal axis.

Substituting these equations into Equation 13 for σ11, determines the principal stresses

σp=σ11+σ222+σ11σ222(±12(σ11σ22)(14(σ11σ22)2+σ122)12)+σ12(σ12±(14(σ11σ22)2+σ122)12)=σ11+σ222+14(σ11σ22)2±(14(σ11σ22)2+σ122)12+σ122±(14(σ11σ22)2+σ122)12=σ11+σ222±(14(σ11σ22)2+σ122(14(σ11σ22)2+σ122)12)

Resulting in

=σ11+σ222±(14(σ11σ22)2+σ122)12 Template:Spaces[19]

Use Equation 19 in Equation 16 to find θ for 0<θ<π4.

To find the maximum shear stress, we take the derivative with respect to theta of our simplified Equation 15 for σ12 and set it equal to 0.

0=ddθ(σ22σ112sin2θ+σ12cos2θ)=2σ22σ112cos2θ2σ12sin2θ=(σ22σ11)cos2θ2σ12sin2θ

Resulting in an expression for 2θ:

σ22σ112 σ12=sin2θcos2θ=tan2θ Template:Spaces[20]

Notice that Equation 20 and Equation 16 are negative reciprocals which means that 2θp and 2θMAX are shifted by π/2. This is indicative of

tanϕ=abtanϕ+π2=ba

which implies that 2θp and 2θMAX are separated by π/4. Through substitution of Equation 20 into Equation 15, we arrive at an expression for σ12MAX:

σ12MAX=±[(σ11σ222)2+σ122]12 Template:Spaces[21]

Mohr's Circle

A convenient means of visualizing angular relationships is through Mohr's circle, which we derive here. Rearrange Equation 13 for σ11 and Equation 15 for σ12,

σ11σ11+σ222=σ11σ222cos2θ+σ12sin2θ Template:Spaces[22]
σ12=σ22σ112sin2θ+σ12cos2θ Template:Spaces[23]

Square both expressions,

(σ11σ11+σ222)2=(σ11σ222cos2θ+σ12sin2θ)2
(σ12)2=(σ22σ112sin2θ+σ12cos2θ)2

Next, add them together to yield

(σ11σ11+σ222)2+σ122=(σ11σ222)2(cos22θ+sin22θ)+σ122(cos22θ+sin22θ)(σ11σ11+σ222)2+σ122=(σ11σ222)2+σ122

The resulting expression is the equation for a circle: (xh)2+y2=r2

Figure 6: Mohr's circle for the plane stress condition. The initial stress state is σ and rotation of the system by θ to σ corresponds to rotating by 2θ on the diagram.
(σ11σ11+σ222)2(xh)2+σ122y2=(σ11σ222)2+σ122r2 Template:Spaces[24]

From this expression, Mohr's circle is drawn in Figure 6. For a given stress state, σ, the center of the circle is h=σ11σ222 and the radius r=((σ11σ112)2+σ122)12. A bisecting line intercepts the circle such that the projection onto the x-axis identifies σ11 and σ22. The projection onto the y-axis identifies σ12. Rotating the bisection is equivalent to transforming the stress state by 2π, i.e., a rotation by ϕ on the diagram is equivalent to rotating by 2π in our equations. This allows the new stress state to be read from the diagram. When the bisector is horizontal, the principal orientation is identified. Rotating the bisection on the diagram by π is equivalent to rotating the system by θ=π/2, which can be imagined as rotating the cuboid faces until the system is back in registry, i.e., it returns to the original stress state. Further, rotating the bisection on the diagram by π/2 is equivalent to rotating by θ=π/4, which is known to be the orientation with maximum shear stress. Thus, from a given initial stress state, σ, all stress states that can be achieved through rotation are visualized on the circle.


Generalizing from 2D to 3D

Generalizing from 2D to 3D, we move from a biaxial plane stress system to a triaxial system. Determining the principal axis and angular relations is similar to the case of 2D and will be shown below. Note as a matter of convention, when two of the three principal stresses are equal, we call the system "cylindrical", and if all three principal stresses are equal, we call the system "hydrostatic" or "spherical".

As in the case of the biaxial system, we begin by defining a plane with area A that passes through our x1, x2, and x3 coordinate system, as shown in Figure 7. The plane intercepts the axis at (J, K, and L) as demonstrated in the figure. To simplify the problem and allow us to make progress toward our derivation, we will say that the plane is one of the principal planes so that the shear stress components are zero. Thus, we only need to consider our principal stress that is normal to the plane.

Define , m, and n to be the direction cosine between x1, x2, and x3 and the normal to the stress. Using the unit vectors i^, j^, and k^ parallel to x1, x2, and x3, we have

Figure 7: Coordinate plane JKL in 3D that passes through the x, y, z coordinate system with positive shear stresses acting on it where O is the origin.
=cosθ1=i^σ|σ|m=cosθ2=j^σ|σ|;n=cosθ3=k^σ|σ|

The projection of stress along x1, x2, and x3 direction give the total stresses S1, S2, and S3:

S1=σp;S2=σpm;S3=σpn

In the biaxial derivation, the area is projected into three directions, producing the triangles in Figure 7 which have areas LOK=A, JOL=Am and JOK=An. We can now equate the forces in the two reference frames:

S1A=σpA=Fx=LOKσ11+JOLσ21+JOKσ31+=Aσ11+Amσ21+Anσ31

So,

σp=σ11+σ21m+σ31n Template:Spaces[25]

By a similar process, the Fx2 and Fx3 components yield

σpm=σ12+σ22m+σ32n Template:Spaces[26]
σpn=σ13+σ23m+σ33n Template:Spaces[27]

These equations rearrange to

0=(σ11σp)+σ12m+σ13n Template:Spaces[28]
0=σ12+(σ22σp)m+σ23n Template:Spaces[29]
0=σ13+σ23m+(σ33σp)n Template:Spaces[30]

This set of equations can be solved for [,m,n] for a particular value of σp. This set of secular equations can be solved for eigenvalues σp and eigenvectors [,m,n]. The non-trivial solutions, when ,m, and n are non-zero, involves setting the determinant

det |σ11σpσ12σ13σ12σ22σpσ23σ13σ23σ33σp|

to zero and solving for the eigenvalues and subsequent eigenvectors.

Upon rearranging, we get

0=σp3(σ11+σ22+σ33)σp2+(σ11σ22+σ22σ33++σ33σ11σ122σ232σ312)σp(σ11σ22σ33+2σ12σ23σ31σ11σ232σ22σ132σ33σ122) Template:Spaces[31]

The three roots of this cubic equation give the principal stresses, σp1, σp2, and σp3. The principle stresses, once determined, are substituted back into the secular Equations 28-30 to determine the eigenvectors corresponding to [,m,n], also recognizing that 2+m2+n2=1.

Solving the cubic equation is not the focus of this text, but Equation 31 is important because the coefficients in front of the principal stress must be invariant, i.e., the same principal coordinates must exist no matter the orientation of the coordinate system. From the cubic equation, the three invariants are

I1=(σ11+σ22+σ33) Template:Spaces[32]
I2=(σ11σ22+σ22σ33+σ33σ11σ122σ232σ312) Template:Spaces[33]
I3=(σ11σ22σ33+2σ12σ23σ31σ11σ232σ22σ132σ33σ122) Template:Spaces[34]

This is useful because these invariant relations determine the relationship between stresses in different orientations, i.e. given σ, you can now directly determine σ1, σ2, and σ3.

Now, we will generalize our solution to include not only the principal stresses. Just as we did earlier, we can write out the total forces:

Sx1A=Fx1=σ11A+σ12mA+σ31nA
Sx1=σ11+σ12m+σ33n Template:Spaces[35]
Sx2=σ12+σ22m+σ23n Template:Spaces[36]
Sx3=σ13+σ23m+σ33n Template:Spaces[37]

Which gives the total stress:

S2=Sx12+Sx22+Sx32 Template:Spaces[38]

From this, the projection onto the normal component is:

σ=Sx1+Sx2m+Sx3n Template:Spaces[39]

Substituting Equations 34-36 into Equation 38 gives us:

σ=(σ11+σ12m+σ31n) +(σ12+σ22m+σ31n) m+(σ13+σ31m+σ33n) n

Which simplifies to,

σ=σ112+σ22m2+σ33n2+2σ12m+2σ23mn+2σ31n Template:Spaces[40]

The magnitude of the shear component can be determined utilizing S2=σ2+τ2, but we cannot easily decompose our shear stress into its constituent elements. Fortunately, we are primarily interested in the maximum shear stress. We know that the plane containing the maximum shear stress is located midway between the planes of principal normal stresses. Starting by setting our known stress state as the principal axis such that σ11=σp1, σ22=σp2, and σ33=σp3, our direction cosine is between the principal axis and the normal of the plane with the maximum shear stress. This means that Equation 39 for projection is rewritten as:

σ=σp12+σp2m2+σp3n2 Template:Spaces[41]

Squaring this equation gives us:

σ2=σp124+σp22m4+σp32n4+2σp1σp22m2+2σp1σp32n2+2σp2σp3m2n2p Template:Spaces[42]

We can then use the principal components and substitute Equations 34-36 into Equation 37 to get:

S2=σ1122+σ222m2+σ332n2 Template:Spaces[43]

After much algebra and putting Equations 41 & 42 into Equation 40, we get:

τMAX2=(σ11σ22)22m2+(σ11σ33)22n2+(σ22σ33)2m2n2 Template:Spaces[44]

With this solution, we now have three possible planes. One plane bisects σ11 and σ22, another plane bisects σ11 and σ33, and the final plane bisects σ22 and σ33. (Bisecting means θ=π4, and cosπ4=22). Here are the values of ,m,n, and τ for these three planes:

𝒎 𝒏 τ
0 22 22 12(σ22σ33)
22 0 22 12(σ11σ33)
22 22 0 12(σ11σ22)

By convention, σ11>σ22>σ33, and therefore our maximum shear stress is:

τMAX=σ11σ332
Figure 8: A 3D Mohr's Circle includes three circles, one for each axis, and follows the σ11>σ22>σ33 convention.

Note that we know there are two planes of maximum shear stress, rotated π/2 from each other. Thus, the direction cosine above are actually ±22.

Because these axial rotations are decoupled, we can represent 3D stress states using Mohr's Circles as seen in Figure 8.



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