How Flexibility of
Buildings Affects Their Earthquake Response? |
Oscillations of Flexible
Buildings
When the ground shakes, the base of a building moves with the ground,
and the building swings back-and-forth. If the building were rigid, then
every point in it would move by the same amount as the ground. But, most
buildings are flexible, and different parts move back-and-forth by
different amounts.
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(a) Building pulled with a
rope tied at its roof |
(b)Oscillation of building on
cutting the rope |
Figure 1: Free
vibration response of a building: the back and -forth motion
is periodic |
Take a fat coir rope and tie one end of
it to the roof of a building and its other end to a motorized vehicle
(say a tractor). Next, start the tractor and pull the building; it will
move in the direction of pull (Figure1a). For the same amount of pull
force, the movement is larger for a more flexible building. Now, cut the
rope! The building will oscillate back-and-forth horizontally and after
some time come back to the original position (Figure 1b); these
oscillations are periodic. The time taken (in seconds) for each
complete cycle of oscillation (i.e., one complete
back-and-forth motion) is the same and is called Fundamental
Natural Period T of the building. Value of T depends on the
building flexibility and mass; more the flexibility, the longer is the
T, and more the mass, the longer is the T. In general,
taller buildings are more flexible and have larger mass, and therefore
have a longer T. On the contrary, low- to medium-rise buildings
generally have shorter T (less than 0.4 sec).
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Figure
2:fundamental natural periods of structures doffer over a large
range.the natural period values are only indicative; depending on
actual properties of the structure, natural period may vary
considerably |
Fundamental natural period T is
an inherent property of a building. Any alterations made to the building
will change its T. Fundamental natural periods T of normal
single storey to 20 storey buildings are usually in the range
0.05-2.00 sec. Some examples of natural periods of different
structures are shown in Figure 2.
Importance of Flexibility
The ground shaking during an earthquake contains a mixture of many
sinusoidal waves of different frequencies, ranging from short to long
periods (Figure 3). The time taken by the wave to complete one cycle of
motion is called period of the earthquake wave. In general,
earthquake shaking of the ground has waves whose periods vary in the
range 0.03-33sec. Even within this range, some earthquake waves
are stronger than the others. Intensity of earthquake waves at a
particular building location depends on a number of factors, including
the magnitude of the earthquake, the epicentral distance,
and the type of ground that the earthquake waves traveled through before
reaching the location of interest.
In a typical city, there are buildings of many different sizes and
shapes. One way of categorizing them is by their fundamental natural
period T. The ground motion under these buildings varies across the
city (Figure 4a). If the ground is shaken back-and-forth by earthquake
waves that have short periods, then short period buildings will
have large response. Similarly, if the earthquake ground motion has long
period waves, then long period buildings will have larger
response. Thus, depending on the value of T of the buildings and
on the characteristics of earthquake ground motion (i.e., the
periods and amplitude of the earthquake waves), some buildings will be
shaken more than the others.
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figure 3: Strong earthquake
Ground Motion is transmitted by waves of different periods. |
Different Buildings respond
differently to same ground vibration |
During the 1967 Caracas earthquake in
South America, the response of buildings was found to depend on the
thickness of soil under the buildings. Figure 4b shows that for
buildings 3-5 storeys tall, the damage intensity was higher in areas
with underlying soil cover of around 40-60m thick, but was minimal in
areas with larger thickness of soil cover. On the other hand, the damage
intensity was just the reverse in the case of 10-14 storey buildings;
the damage intensity was more when the soil cover was in the range
150-300m, and small for lower thickness of soil cover. Here, the soil
layer under the building plays the role of a filter, allowing some
ground waves to pass through and filtering the rest.
Flexible buildings undergo larger relative horizontal displacements,
which may result in damage to various nonstructural building components
and the contents. For example, some items in buildings, like glass
windows, cannot take large lateral movements, and are therefore damaged
severely or crushed. Unsecured shelves might topple, especially at upper
stories of multi-storey buildings. These damages may not affect safety
of buildings, but may cause economic losses, injuries and panic among
its residents.
Related IITK-BMTPC Tip
IITK-BMTPC Earthquake Tip 2: How the Ground Shakes?
IITK-BMTPC Earthquake Tip 5: What are the Seismic Effects on Structures?
Resource Material
Wiegel,R., (1970),
Earthquake Engineering,
Prentice Hall Inc., USA.
Chopra,A.K., (1980), Dynamics of Structures – A Primer,
Earthquake Engineering Research Institute, USA.
Authored by:
C.V.R. Murty
Indian Institute of Technology Kanpur, Kanpur, India
Sponsored by:
Building
Materials and Technology Promotion Council, New Delhi.
Suggestions/comments may be sent to
eqtips@iitk.ac.in
To see previous IITK-BMTPC Earthquake Tips, visit
www.nicee.org
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