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Moreover, the results were analyzed in terms of the vapor volume fraction variation, temperature and vertical velocity at different locations along the thermosyphon.
This part mainly analyzes the effects of temperature variation, temperature curve index, type of TDL, beam height, and beam span on the vertical displacement of rail and track irregularity caused by TDL.
Simultaneous investigations into the different aspects of the electrical contact, such as the conductivity variation, temperature rise, as well as the microstructure characteristics, would be absolutely helpful for a better understanding of the pantograph catenary system.
In this section, a study of the evolution of the UV-vis absorption bands during the fabrication process, thickness variation, temperature effect, or distribution of the AgNPs into the thin films will be presented.
The amplitude of irregularity caused by TDL is largely affected by the temperature variation, temperature curve index, and type of temperature gradient, so it is necessary to monitor the temperature distribution of bridges in different regions to provide accurate calculation parameters.
Active salars (water available) are characterized by high UV radiation, high heavy metals content, wide daily temperature variation (temperature range −20 to 25 °C, approximately), and aquatic systems with variable salt concentration (Dorador et al. 2008; Demergasso et al. 2008; Risacher et al. 2003).
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Thus, although the January average temperature is 14 °F (−10 °C), there can be considerable variation; temperatures have dropped to near −45 °F (−43 °C).
The average annual temperature is 51 °F (10.5 °C), but this conceals a wide variation; temperatures as low as −37 °F (−38 °C) and as high as 113 °F (45 °C) have been recorded.
Different loading conditions are considered, including the uniform temperature variations, temperature gradients, self-weights, and HS-20 live loads.
The variation of temperature was from room temperature to 700 °C.
Like cloud cover, the dominant variation in temperature is the seasonal variation: the temperature peaks once a year in the summer.
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