
6.3 Unsymmetrical sections 311
6.3 Unsymmetrical sections
So far, we have considered only sections with at least one axis of symmetry. The
generalization to unsymmetrical sections is routine, but leads to significantly more
complicated algebra. The principal reason for performing these calculations is to de-
termine the location of the shear centre, since the moment resulting from shear load-
ing of an open section away from its shear centre [see e.g. Figure 6.29 (b)] can cause
significant torsional stresses and twist, as will be discussed in §6.7 below. By con-
trast, the shear stresses associated with shear loading acting through the shear centre
are often sufficiently small to be neglected, or estimated by simple approximations
as discussed in §6.1.2.
6.3.1 Shear stress for an unsymmetrical section
The derivation of §6.1 can be generalized to unsymmetrical sections, using equation
(4.20) in place of (6.2) to define the bending stress. We obtain
q =
τ
t =
(V
x
I
x
−V
y
I
xy
)A
∗
¯x
∗
−(V
x
I
xy
−V
y
I
y
)A
∗
¯y
∗
(I
x
I
y
−I
2
xy
)
, (6.19)
where (¯x
∗
, ¯y
∗
) are the coordinates of the centroid of A
∗
relative to the centroid of the
whole section and we have used the relations
V
x
= −
dM
y
dz
; V
y
=
dM
x
dz
, (6.20)
obtained by similar arguments to equation (6.1), using the sign convention of Figures
4.1, 6.1.
If the coordinate system Oxy is chosen to coincide with the principal axis system
as in §4.4.3, the product inertia I
xy
will be zero and equation (6.19) reduces to
q =
τ
t =
V
x
A
∗
¯x
∗
I
y
+
V
y
A
∗
¯y
∗
I
x
, (6.21)
which is of course equivalent to the superposition of two applications of equation
(6.9) about orthogonal axes.
6.3.2 Determining the shear centre
Suppose that the shear centre of the unsymmetrical thin-walled section of Figure
6.31 is at the point C(a, b). As before, the shear flow q defined by equation (6.19)
corresponds to an elemental force dF =
τ
tdS = qdS. The moment of the complete
stress distribution about O can then be equated to the moment of the two shear force
components V
x
,V
y
, giving
aV
y
−bV
x
=
Z
S
nqdS . (6.22)