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where the last step made use of the small angle approximation, tan
≅ .
Comparing equations (D-21) and (D-10),
)
εε
θθ
r
=
r
is seen to be one-half of the
angle change between two perpendicular lines initially lying along the
and r
coordinate directions.
D.3 Stress and Equilibrium
The counterpart to strain, the measure of the deformation experienced by a
material, is stress, the imposed load causing the deformation. Two types of loads
or forces will be considered here: surface forces, or tractions, and body forces.
For these two types of loads, the load intensity can be defined respectively in
terms of the stress vector,
, and the body force vector,
σ
~
~
,
σ
~
~
lim=
→
F
A
A
i
∆
∆ 0
(D-22)
χ
χ
~
~
lim=
→
i
V
V
∆
∆ 0
(D-23)
In other words, the stress vector,
, is a measure of the local intensity of contact
forces acting on the surface of a body, and is determined by taking the limit of the
resultant contact force,
σ
~
FF
i
~~
=
, acting on a small area
∆
A as the dimensions
of the area become infinitesimal. In a similar vein, the body force vector,
~
, is a
measure of the volumetric intensity of field forces acting on an infinitesimal
volume element
3
.
D.3.1 Decomposition of the Stress Vector
For reasons that will become apparent shortly, it is usually not convenient to work
with the stress vector. Rather, common practice is to decompose the stress into
nine components roughly corresponding to the components of strain (i.e., a
θ
r
stress will result in an
θ
r
strain). In order to formally introduce the components
of stress, consider Figure D-3. The left-hand drawing in Figure D-3 shows a body
B subjected to contact forces such as to place the body in static equilibrium. Only
the surface tractions acting on surface element
∆
A have been shown in order to
avoid cluttering the figure. The right-hand drawing in Figure D-3 is an expanded
view of the area
∆
A and a portion of the body interior to the surface
∆
A. Internal
stress vectors
, , and , acting on the respective coordinate faces, when
combined with the external surface traction,
, render the differential body
σ
~
r
σ
θ
~
σ
~
z
σ
~
3
Although the complexion of the body force vector can be quite involved, the only body
force to be considered here will be that due to the earth's gravitational field.
Casing/Tubing Design Manual D-9
October 2005