Asphalt concrete was used for the first time in Syria as a tightening material for dam
Sourani. It was used in this dam as a surface facing on the front slope.
Use of asphaltic concrete under climatic conditions prevailing in Syria, particularly
h
igh temperatures, is discussed in the paper. To achieve this goal, a number of bituminous
concrete mixes, designed using the same constituent components in Sourani dam, were
experimentally tested and analyzed. To determine the effect of the expected maximum
temperatures for Sourani dam, a program depending on Energy balance was developed.
Possible methods of reducing the effect of the high temperature in order to increase
the stability of the asphalt surface facing are analyzed. In this context, the facing was
plastered by a light-color, which led to a decrease in the temperature of the asphalt surface
facing by about 20 degrees Celsius. The facing was also plastered by placing a concrete
layer above it, which led to a decrease in the temperature of the asphalt surface facing by
about 25 degrees Celsius.
Continuous calculations of evapotranspiration (LE) using eddy covariance
method and energy budget were performed over more than one year above the
heterogeneous canopy of an arid oasis ecosystem in the central Syrian desert.
Irrigation practice wa
s traditional flooding with a 28 days turn of water
delivery. The work focuses on seasonal variations of energy budget over a 2
years period with emphasis on effects of rainfall, wind speed and radiative
budget on evapotranspiration. Maximum evapotranspiration was only
5mm/day. Even under irrigation practices, winter rainfall seems to have an
important impact on LE: comparisons of two situations in June 2002 and June
2003 showed an increase of 13% in values of LE/Rn-G. Maximum averaged
hourly values of evapotranspiration were found for wind speed values closed to
3m/s. This suggests that when the evaporative demand from the air (or vapour
pressure deficit (vpd) ) is increasing above a certain limit, the vegetation closes
its stomata and reduces transpiration. Results from the energy balance closure
showed significant differences in the slope of H+LE against Rn-G relationships
between cold and hot month which was explained by specific radiative budget
of desert areas.