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Geotechnical Evaluation of Miocene Expansive Shale, Jeddah, Saudi Arabia

机译:沙特阿拉伯吉达中新世膨胀页岩的岩土工程评价

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摘要

Expansive shale has been found extensively in all over the world especially in arid and semi-arid regions. The ground heave resulted from shale swelling potential are considered as a multi factorial phenomenon. The Miocene Shale of Bathan Formation composes mainly of shale beds with sandy silt thinly interbedded layers which formed during several cycles of sedimentation. The swelling potentiality of expansive shale of Bathan Formation (Middle to Late Miocene) in NE Jeddah, Saudi Arabia was evaluated based on physico-chemical and mechanical measurements. Its swelling potentiality (free swelling, swelling percent and swelling pressure) has a direct relationship with clay fraction content, plasticity index (PI) and cation exchange capacity (CEC). Furthermore, the clay fraction percent has a strong direct proportional relation to free swelling, plasticity index (PI) and cation exchange capacity (CEC).
机译:膨胀页岩在世界各地特别是干旱和半干旱地区被广泛发现。页岩膨胀潜能导致的地面起伏被认为是一种多因素现象。 an斯坦组的中新世页岩主要由页岩床组成,这些页岩层是砂质粉砂薄互层的层,这些层是在几个沉积周期中形成的。根据理化和力学测量,评估了沙特阿拉伯吉达东北部巴中组(中新世至中新世)膨胀页岩的溶胀潜力。其溶胀潜能(自由溶胀,溶胀百分数和溶胀压力)与粘土含量,可塑性指数(PI)和阳离子交换容量(CEC)直接相关。此外,粘土分数百分比与自由溶胀,可塑性指数(PI)和阳离子交换容量(CEC)有很强的直接比例关系。

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