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Shear stress in beams Dr Alessandro Palmeri Senior Lecturer in Structural Engineering <[email protected]>
2/30
Learning Outcomes When we have completed this unit (2 lectures + 1
tutorial), you should be able to: ◦ Gain a broad understanding of shear stress in
beams ◦ Apply the Jourawski’s formula to solid rectangular
sections and web of T and I sections
Schedule: ◦ Lecture #1: Jourawski’s formula, with application
to solid rectangular sections ◦ Lecture #2: Application to web of T and I
sections ◦ Tutorial
3/30
JOURAWSKI’S FORMULA, WITH APPLICATION TO SOLID RECTANGULAR SECTIONS
Lecture #1
4/30
Shear Force & Bending Moment At a given cross section of the beam, we
have generally both Bending Moment (BM) My and Shear Force (SF) Vz
The SF gives the slope of the BM diagram:
That is, the larger is the rate of variation of the BM along the beam, the larger is the SF
Vz =dMy
dx
5/30
Shear Force & Bending Moment
W
W
x
x
−
+
W W
54W
34W
x
x
+
−
+
My
Vz
6/30
Shear Force & Bending Moment
2W L
W
W
x
x−
+
W W
W
W
x
x−
+
+ +
My
Vz
7/30
Normal stress (Sigma) The bending moment M sets up
(longitudinal) normal stress σx, which varies linearly with the distance from the neutral axis:
where ◦ Iyy is the second moment of the cross sectional
area ◦ z is the distance from the neutral axis (positive if
downward)
σ x =My z
I yy
8/30
Shear stress (Tau)
Key point: As the SF depends on the variation of the BM along the beam, similarly the shear stress τxz depends on the variation of the direct stress σx over the cross section
M M
Side View
tension
compression
Cross Section
t 0σ >
c 0σ <
Bending Stress
σ x < 0
σ x > 0
My My
x
M M
Side View
tension
compression
Cross Section
t 0σ >
c 0σ <
Bending Stress
σ x < 0
σ x > 0x
z
y x
9/30
Jourawski’s formula An engineering solution for the shear stress
distribution over the beam’s cross section can be obtained by using simple equilibrium considerations
Since the elasticity theory will be not involved, this is just an approximate solution
You must recognize the intrinsic limitations of this formula:
τ xy(P) =
Vz Qy(P)I yy b(P)
10/30
Jourawski’s formula Without lack of
generality, let us consider two cross sections 1 and 2 very close together, i.e. the distance is infinitesimal (dx), so that under a distributed load the BM experiences an infinitesimal variation (dMy)
dx1 2
My My + dMy
Vz =dMy
dx
11/30
Jourawski’s formula
MdM M+
M
dM M+
FdF F+
cσ c cdσ σ+
dx
A A
Ab
Fx + dFx
b(P)
σ xFx σ x + dσ x
My
My + dMy
My + dMy
My
dx
x
P P
12/30
Jourawski’s formula Looking closely to the equilibrium of the top
“slice” of the beam between sections 1 and 2, i.e. above the ideal horizontal cut P-P, one can observe that a force difference dFx exists between these two sections, which must be balanced by a shear stress of resultant dRx
Fx Fx + dFx
dRxA A
τ zx (P)1 2
P P
13/30
Jourawski’s formula The forces Fx and Fx+dFx applied to sections 1
and 2, respectively, can be determined from the direct stress σx, which in turn depends on the BM at these sections, along with second moment of the cross sectional area Iyy and distance z from the neutral axis
Fx Fx + dFx
dRxA A
τ zx (P)1 2
P P
14/30
Jourawski’s formula It can be shown that the force acting on the plane P-P
is given by:
where Qy(P) is the first moment of the cross sectional area above (or below) P-P with respect to the neutral axis, which can be computed as:
AP being the area above (or below) P-P, while yA is
the distance of the centroid of AP with respect to the neutral axis
dFx =dMy Qy (P)
I yy
Qy (P) = AP × zP
zP
15/30
Jourawski’s formula Approximation! Under the assumption that the
shear stress τxz is uniformly distributed over the area P-P, we have that the difference force dFx is given by:
where b(P) is the width of the beam’s cross section at the level of P-P
Rearranging the above equations, and taking into account that Vz= dMy/dx, we get the Jourawski’s formula for shear stress distribution
dFx =dMy Qy (P)
I yy= τ zx (P)b(P)dx
τ zx (P)horizontal
= τ xz (P)vertical
=dM y
dx
Qy (P)
I yy b(P)=Vz
Qy (P)
I yy b(P)
16/30
Jourawski’s formula Note! The Jourawski’s formula gives
the values of both horizontal and vertical shear stress at the level P-P
This expression can be used to find beam’s shear stress in solid sections, e.g. square, rectangular, circular, and etcetera
Adjustments are needed when dealing with ◦ open sections, e.g. I sections, T
sections, C sections, angles and etcetera; ◦ hollow sections, e.g. pipes or hollow
rectangular sections
x y
z
τ zx (P)horizontal
τ xz (P)
vertical
P
17/30
Beam’s shear stress in a solid rectangular section We need to apply the Jourawski’s formula to the
cross section shown below, which is subjected to a vertical shear force Vz
18/30
Beam’s shear stress in a solid rectangular section
The shear stress at a generic level P takes a parabolic (i.e. quadratic) expression:
A(P) = b d2− zP
⎛⎝⎜
⎞⎠⎟
zP =12d2+ zP
⎛⎝⎜
⎞⎠⎟
Qy (P) = A(P) zP =12d 2
4− zP
2⎛⎝⎜
⎞⎠⎟
τ xz (P) =Vz Qy (P)I yy b
=Vz2 I yy
d 2
4− zP
2⎛⎝⎜
⎞⎠⎟
19/30
Beam’s shear stress in a solid rectangular section
At the bottom edge:
At the neutral axis:
zP =d2
τ xz (P) =Vz2 I yy
× 0 = 0
zP = zG = 0
τ xz (G) =Vz2 I yy
× d2
4= max τ xz (G){ }
I yy =bd 3
12⇒ τmax =
128Vzbd
=1.5VzA
50% more than the nominal average shear stress V/A
20/30
APPLICATION TO WEB OF T AND I SECTIONS
Lecture #2
21/30
Wrong results for flanges of T and I sections The Jourawsky’s formula:
cannot be applied to the flanges of T and I sections, since the results so obtained are wrong
τ xz (P) =Vz Qy (P)I yy b(P)
This is not correct, and underestimates the actual shear stress in the flange
The parabolic distribution in the web, although approximate, is acceptable from an engineering point of view
22/30
Wrong results for flanges of T and I sections
Experimental and numerical analyses confirm that the “flow” of the shear stress in the flange of an I section is similar to what depicted below
τ flange
τweb
23/30
Wrong results for flanges of T and I sections
At the free edge of a member, there cannot be a finite component of the stress acting at right angle to the edge, simply because there is nothing to provide a reaction
24/30
Shear stress in the web of T sections 1.0m
20 kN
20 kN
20 kNm
V
M
+
−My
Vz
25/30
Shear stress in the web of T sections
150
XB
16
16
150
43.4
106.6
XB
I yy =150×163
12+ 150×16( )× 43.4− 16
2⎛⎝⎜
⎞⎠⎟
35.4
2
+ 16× (150−16134
)3
12+ 134×16( )× 106.6− 134
2⎛⎝⎜
⎞⎠⎟
39.6
2
= 9.63×106 mm4
neutral axis
35.4
39.6
τ xz (P) =
Vz Qy (P)
I yy b(P)
26/30
Shear stress in the web of T sections
150
XB
16
16
150
43.4
106.6
XB
A(B) = 150×16 = 2,400 mm2
neutral axis
35.4
39.6
zB = − 43.4− 16
2⎛⎝⎜
⎞⎠⎟= −35.4 mm
Q(B) = 2,400× (−35.4) = −85,000 mm3
τ xz (B) =
VzQy (B)
I yy b(B)= 20,000× (−85,000)
9.63×106 ×16= −11.0 MPa
τ xz (P)
Shear stress at the top of the web
We consider here the area above B-B
The negative sign means that the flow of shear stress exits the considered area, i.e. is downward
27/30
Shear stress in the web of T sections
150
XB
16
16
150
43.4
106.6
XB
A(G) =106.6×16 =1,706 mm2
neutral axis
35.4
39.6
zG = 106.62
= 53.3mm
Qy (G) =1,706×53.3 = 90,900 mm2
τ xz (G) =Vz Qy (G)I yy b(G)
= 20,000× 90,9009.63×106 ×16
=11.8 MPa
XXτ
Shear stress at the neutral axis
We consider here the area below G
G
The positive sign means that the flow of shear stress enters the the considered area, i.e. is downward
28/30
Shear stress in the web of T sections
150
XB
16
16
150
43.4
106.6
XB
neutral axis
35.4
39.6
Qy (G) = 150×16( )× (−35.4)
Qy (B)
+ 43.4−16( )×16⎡⎣ ⎤⎦ × − 43.4−162
⎛⎝⎜
⎞⎠⎟= −91,000 mm2
τ xz (G) =Vz Qy (G)I yy b(G)
= 20,000× (−91,000)9.63×106 ×16
= −11.8 MPa
XXτ
We obtain the same result when considering in the calculations the area above the neutral axis
G
The only difference is the negative sign, because this time the flow of shear stress exits area above the neutral axis, i.e. is downward
29/30
Shear stress in the web of T sections
Please note that, if the width b is constant along the web, then: ◦ the maximum shear stress τxz happens at the level of the
neutral axis ◦ the distribution of the shear stress is parabolic
150
XB
16
16
150
43.4
106.6
XB
neutral axis
BB 11.0 MPaτ =XX 11.8MPaτ =G
30/30
Shear stress in the web of other sections