fiat lux university of liverpool school of engineering department of c
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FIAT LUX
UNIVERSITY OF
LIVERPOOL
School of Engineering
Department of Civil Engineering and Industrial Design
CIVE342: Earthquake Engineering UNIVERSITY OF
LIVERPOOL
A three-storey residential (ordinary) building is shown in Figure 1, where the value next to each
column indicates the corresponding lateral stiffness. The mass of each whole floor is 2000 tonnes.
The building is situated in a region with a reference PGA of 25%g (TNCR = 475 years) and where
seismic hazard is dominated by events with a surface wave magnitude less than Ms 5.5.
The shear wave velocity of the site is estimated to be 510m/s.
The sample structure is a shear-type building.
Assume a damping ratio of 5% and a behaviour factor of 3.0.
Determine:
3m 800kN/mm
600kN/mm
3m 700kN/mm
500kN/mm
4m 600kN/mm
400kN/mm
TI
Figure 1 - Shear-type multi-storey building (bay width 4.5m).
Number and values of frequencies of vibration;
-
Modes of vibration and their shape;
-
Participating masses for modes of vibration.
Using the equivalent static approach and the seismic input provided above, determine:
-
Seismic horizontal base shear;
Seismic horizontal forces at each storey;
Bending moment and shear distributions in beams and columns
Inter-storey drifts at each storey.
2 Appendix. Excerpts from EN 1998-1:2004
3.2.2.2 Horizontal elastic response spectrum
UNIVERSITY OF
LIVERPOOL
T
0≤T≤TB: Se(T) = ag · S +
(n.2.5-1)
(3.2)
TB
TB≤T≤Tc : Se(T)=αg·S⋅n·2.5
(3.3)
Tc≤T≤TD: Se(T) =ag ·S.n.2.5
2.5√
(3.4)
Tɲ≤T≤4s: Se(T) = ag · S · n ⋅ 2.5|
TCTD
(3.5)
T2
n=10/(5+)≥0.55
(3.6)
(= viscous damping ratio in percent)
3.2.2.5 Design spectrum for elastic analysis
(For 5% damping)
0≤T≤TB: Sɖ(T) = ag · S
2
T 2.5
+
(3.13)
TB q
TBST≤TC: Sa(T) = a
2.5
(3.14)
q
2.5 TC
·S.
Tc≤T≤Tp: Sd(T) = ·
q
T
(3.15)
≥ẞ-ag
S
2.5 TcTo
TD≤T: Sα(T) =
9T2
(3.16)
≥ẞ.ag
3 UNIVERSITY OF
LIVERPOOL
Table 3.1 Ground types
Ground
type
Description of stratigraphic profile
Parameters
Vs,30 (m/s)
NSPT
Cu (kPa)
(blows/30cm)
A
B
Rock or other rock-like geological formation, including
at most 5 m of weaker material at the surface.
Deposits of very dense sand, gravel, or very stiff clay,
at least several tens of metres in thickness,
> 800
360-800
> 50
> 250
characterised by a gradual increase of mechanical
properties with depth.
C
Deep deposits of dense or medium dense sand, gravel
or stiff clay with thickness from several tens to many
hundreds of metres.
180-360
15-50
70-250
Ꭰ
Deposits of loose-to-medium cohesionless soil (with or
without some soft cohesive layers), or of
< 180
< 15
< 70
predominantly soft-to-firm cohesive soil.
E
S₁
A soil profile consisting of a surface alluvium layer
with vs values of type C or D and thickness varying
between about 5 m and 20 m, underlain by stiffer
material with vs > 800 m/s.
Deposits consisting, or containing a layer at least 10 m
thick, of soft clays/silts with a high plasticity index (PI
> 40) and high water content
S2
Deposits of liquefiable soils, of sensitive clays, or any
other soil profile not included in types A – E or Si
< 100
(indicative)
10-20
Table 3.2 Values of the parameters describing the recommended Type 1 elastic response spectra
Ground type
S
TB (S)
Tc (s) TD (S)
A
1.0
0.15
0.4
2.0
B
1.2
0.15
0.5
2.0
C
1.15
0.20
0.6
2.0
D
1.35
0.20
0.8
2.0
E
1.4
0.15
0.5
2.0
Table 3.3 Values of the parameters describing the recommended Type 2 elastic response spectra
Ground type
S
TB (S)
Tc (s)
TD (s)
A
1.0
0.05
0.25
1.2
B
1.35
0.05
0.25
1.2
C
1.5
0.10
0.25
1.2
D
1.8
0.10
0.30
1.2
E
1.6
0.05
0.25
1.2