Mechanics, Materials Science & Engineering, May 2017
ISSN 2412-5954
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Ahmed Abdelmoamen Khalil 1 Assistant Professor of Railway Engineering, Civil Engineering Department, Shoubra Faculty of Engineering, Benha University, Postal Code: 11629 Egypt a
ahmed.khalil@feng.bu.edu.eg DOI 10.2412/mmse.39.59.615 provided by Seo4U.link
Keywords: railway, embankment, track contamination, wind, sand, FLUENT.
ABSTRACT. Railway lines in deserts suffer from risks of migration of sand dunes, transport of sand by wind and its accumulation over the tracks. This paper focuses on causes, types, and different characteristics of sand movement in desert that affecting safety and performance of running trains. Risk and potential impact of accumulation of sand on Bahariya railway line located in Western Desert of Egypt such as; several derailments and contamination of track components are analysed. The purpose of this paper is to study the impact of embankment height on sand accumulation. Thus, ANSYS FLUENT software is used to simulate the blown wind on the railway embankment to obtain the wind velocity vectors and contours. Hence, embankment height that reduces deposition and accumulation of sand over the track is obtained and recommended to 6 m. Cost analysis has been conducted to compare between the recent and the recommended embankments. It is concluded that cost of the recommended embankment is about 63% of the overall cost of the recent case.
Introduction. Wind is the main cause of sand movements, therefore; attention to the direction and the velocity of the winds is also of importance. Needs for attention to this issue is especially important when considering various preventive methods such as designing a wall [1]. In Egypt, sand deposits and other aeolian forms cover about 27% of the whole country [2]. Morphologically these landforms are subdivided into sand seas (ergs), isolated dunes and dune fields and sandy plains and sheets [2]. At several localities in Egypt, sand encroachment causes hazards to farmlands, highways, population centers and other infrastructures. According to [3], sand encroachment over the inhabitable areas of Egypt is classified into the following categories; (i) Severe dune migration ( > 15 m/year); it occurs in South Al-Bardaweil (North Sinai) and Kharga-Baris and Dakhla in the South Western Desert, (ii) Moderate dune migration (5 15 m/year); it prevails in Central Sinai, east of the Suez Canal, Siwa, Abu Mongar, Farafra, Bahariya and El Rayan; (iii) Slight dune migration ( < 5 m/year); it occurs on both sides of the Nile Delta, northern coast of the Nile Delta and along the Mediterranean Coastal Zone. Source of the sand in the Sahara Desert is attributed to the fluvial processes which thereafter reworked and deposited elsewhere by wind in later dryer ages [4]. Climate of western desert is too dry to have any rains. However the average value of rains is 3.6 mm/year. The average temperature is 29o C in the period from May to September in the north, but it raises up to 32o C in the south. Maximum temperature reaches 50o C. January is the coldest month in the year where the temperature reaches 13o C. However the minimum temperature lies between 0o C and 5o C. Wind blows from the north most of the year but it diverts to blow from the west in winter. The wind speed reaches 20 m/s and it is usually high in the spring, hence sandstorms are caused due to the high intensity of wind [5]. Railways had been established in the west desert of Egypt in 1900 when the government offered the Company of the Oases of West Deserts a concession to construct a railway line to connect the Oases with the Nile Valley. However, the company went 24
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