The Sharbyan river is located in the Sharbyan village, Sarab, East Azarbaijan province. This river alluvials are supplied from rock units belonging to Oligo-miocene and Miocene, including conglomerate, sandy lime, limestone, marl and shale. These deposits are used as raw materials of producing hot asphalt in two asphalt plants that have been built in the vicinity of this river, and the produced asphalt is used mainly in the neighbor provinces that have rather cold climate. Combined analysis of the sediments indicate high level of silica, around 60 percent, for which the prepared asphalt is prone to stripping phenomenon in the cold seasons. During this process, the moisture penetration in aggregates and asphalt mixtures, causes weakening bitumen-asphalt materials bounding and finally asphalt demolition. The role of sediments and its impact on the quality of asphalt has not been studied in this area, therefore, the solutions for dealing with this phenomenon is also examined and presented. This study is based on the conventional sedimentology methods, different standards of ASTM, AASHTO and Ministry of Roads and Urban Development guidelines. In this study, the combined effects of hydrated lime (lime filler) and natural filter materials with different proportions was used to deal with the stripping phenomenon, and the parameters of strength, softness, indirect tensile strength, asphalt quality and durability criteria, have been appraised. The results show that these parameters are improved using additives in various proportions and the produced asphalt quality and durability is better. The results illustrate, when the lime is used in its maximum ratio of 3%, stripping score is 1 and is disappeared by other parameters improvement
Komrud village of located on the slope is particularly susceptible to landslides. The slope stability analysis is of special importance because of landslides or slope failures can cause major damages life and financial. In studies to determine the factors and parameters affecting the slope is unstable. According to studies, one of the most important factor affecting landslides in this area is the force exerted by the acceleration of the earthquake. With this approach, the maximum possible acceleration of earthquakes in a 50-year period is estimated at the site. On the other hand, based on studies of the geological is determined profile of the slope geometry, physical and resistance parameters to the landslide susceptible. Then using the modeling software in FLAC 2D 5.00 elasto-plastic structural models, with failure criteria Mohr – Coulomb, stress-strain behavior of the soil has been examined to pseudo-dynamic method. A base position at the top of the slope is considered and displacement it horizontally to reach the maximum possible acceleration is calculated and recorded. The results of this study indicate that Horizontal displacement followed the landslide, can be occur below the maximum acceleration estimates.
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