Integrating Geotechnical Investigation with Hydrological Modeling for Mitigation of Expansive Soil Hazards in Tabuk City, Saudi Arabia

A. Embaby, A. A. Halawa, M. Ramadan
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引用次数: 8

Abstract

Due to global climatic changes, flash floods are followed as a yearly disaster with high magnitude of influence. During the years 1981, 1988, 2010, 2012 and in January 2013, Tabuk city, northwest of Saudi Arabia suffered huge flash floods. These are major factors affecting on the swelling behavior of expansive Tabuk shale. The examined geotechnical properties of the surface and subsurface lithology of the sedimentary deposits distinguished Tabuk city into three zones. The expansive zone is spread in the middle and the non-expansive zones are distributed in the east and west of the city. The Watershed Modeling System (WMS) and Hydrologic Engineering Center (HEC-1) models were used to delineate and identify the drainage system and basin morphometry, where flash floods and accumulation of water might take place. Integration between geotechnical distribution maps of the expansion soil and surface hydrological data in terms of runoff maps was done. It has been identified the whereabouts the soils which have expansion characteristics and areas prone to flooding and surface runoff. They are helpful in defining the hazard zones map. Based on this map, it can be avoided constructions on the risk neighborhoods such as Al Qadsiyah, Al Maseif, Arrwdah, Al Nakhil and Al Rajhi. Also, it can suggest that the western side of Tabuk city is suitable for future urban extension. These results will help planners and citizens to create alternative development scenarios and determine their impact on the future urbanization patterns. Moreover, the direction of surface runoff flow or storm water discharge should be away from the expansion soil areas. Therefore, constructing dams on the outlet of the high-risk basins, south of Tabuk city is an important solution to control flash flood events, as well as increase groundwater recharge.
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结合岩土工程调查和水文模型缓解沙特塔布克市膨胀土灾害
由于全球气候变化,山洪灾害每年都会发生,影响程度很高。1981年、1988年、2010年、2012年和2013年1月,沙特阿拉伯西北部的塔布克市遭受了巨大的山洪暴发。这些是影响膨胀塔布克页岩膨胀行为的主要因素。经检查的沉积矿床表面和地下岩性的岩土工程特性将塔布克市分为三个区域。膨胀区分布在城市的中部,非膨胀区分布于城市的东部和西部。流域建模系统(WMS)和水文工程中心(HEC-1)模型用于描绘和识别可能发生山洪暴发和积水的排水系统和流域形态测量。根据径流图,对膨胀土的岩土分布图和地表水文数据进行了整合。已经确定了具有膨胀特征的土壤的位置以及容易发生洪水和地表径流的区域。它们有助于定义危险区域地图。根据该地图,可以避免在Al Qadsiyah、Al Maseif、Arrwdah、Al Nakhil和Al Rajhi等风险社区进行施工。此外,它还可以表明塔布克市的西侧适合未来的城市扩展。这些结果将有助于规划者和公民创造替代发展情景,并确定其对未来城市化模式的影响。此外,地表径流或雨水排放的方向应远离膨胀土区域。因此,在塔布克市南部高风险流域的出水口修建大坝是控制山洪事件以及增加地下水补给的重要解决方案。
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