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There are two main factors that contribute to pavement heat intake: solar radiation of
the asphalt concrete surface
layer and geothermal heat flux; and two factors that
contribute to heat extraction: surface convection and radiation emissions (Hermansson,
2000; Doré and Zubeck, 2008). Heat may also be induced into or extracted from the
pavement system due to condensation/evaporation, latent heat of fusion if pavement
material pores contain moisture or ice lenses and heat exchange due to precipitation.
Pavement temperature monitoring
In many countries in the northern hemisphere
where pavements experience
considerable seasonal frost conditions, load restrictions are commonly imposed during
the spring-thaw period to prevent severe pavement deterioration. During this period,
the pavement structures are usually exposed to excess moisture content which results in
reduced bearing capacity in unbound layers and therefore high resilient and permanent
deformations. Monitoring a pavement’s environmental conditions such as frost zone
(temperature) and moisture content can help road authorities to decide where and when
to apply and enforce or to remove load restriction.
In Sweden, monitoring pavement temperature profiles is carried out. The pavement
temperature monitoring program consists of continuous
pavement temperature
measurements from sites that are spread over the country’s road network using the
Tjäl2004 equipment. The Tjäl2004 is a frost rod that was developed at the Swedish
National Road and Transport Research Institute, VTI (Wilhelmson et al., 2004). It
consists of a series of temperature sensors mounted along a metal rod which are placed
in a casing. The temperature sensors are located at 50
mm intervals throughout the
pavement profile and down to a depth of 2 m. These temperature sensors register data
at determined time intervals (usually every 30 minutes) using a data logger that is
supplied with a battery. The temperature sensors are calibrated at 0º C to have the
highest accuracy in detecting the frost zone. The data are then distributed online via the
internet (http://www3.vv.se/tjaldjup). This database assists the local road authorities to
give permission or forbid heavy axle load passages during certain periods by controlling
the frost zone condition in the pavement structure. Figure 2 shows typical registrations
from November 2010 to April 2011 from the station along county road 126 near
Torpsbruk in southern Sweden. The overall formation of the frost zone,
repeated
frost-thaw cycles in the upper part of the pavement, and the thaw penetration can be
seen in Figure 2.