Civil Engineering Reference
In-Depth Information
4
orientation of the bridge axis, latitude and altitude of the location;
5
time of the day and the season;
6
diurnal variations of ambient air temperature and wind speed;
7
degree of cloudiness and turbidity of the atmosphere.
In daytime, especially in summer, heat gain is greater than heat loss, result-
ing in a rise of temperature. The reverse occurs in winter nights and the
temperature of the structure drops. Figure 10.1 is a schematic representation
of heat
ow for a bridge deck during daytime in summer. Incident solar
radiation is partly absorbed and the rest is re
fl
ected. The absorbed energy
heats the surface and produces a temperature gradient through the deck. The
amount of absorbed radiation depends upon the nature and colour of the
surface: the absorptivity is higher in a dark rough surface compared to a
smooth surface of light colour. Some of the absorbed heat of radiation is lost
to the air by convection and re-radiation from the surface. The amount of
convection depends upon wind velocity and the temperatures of the air and
the surface.
fl
10.3 Shape of temperature distribution in bridge
cross-sections
Bridges are generally provided with bearings which allow free longitudinal
translation of the superstructure. A change in temperature, which varies lin-
early over the cross-section of a simply supported bridge, produces no
stresses. When the temperature variation is non-linear, the same bridge will be
subjected to stresses, because any
fi
bre, being attached to other
fi
bres, cannot
Figure 10.1 Heat transfer processes for a bridge deck in daytime in summer.
 
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