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Predicting Shear Strength Properties for Low-Sensitivity Granular-Cohesive Soils from SPT Results

机译:从SPT结果预测低灵敏度颗粒状粘性土的抗剪强度特性

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Several correlations between the standard penetration test (SPT) N-values andinternal friction angle (Φ’) have been developed for granular soils. Some correlationshave also been developed for un-drained shear strength of saturated clays. However,in many instances soils do not behave as either saturated clay or sand. Sometimes itis important to find the contribution of Φ’ in clays with higher silt and sand content;and cohesion in sands that has sufficient clay and silt content. It is incorrect toclassify these soils as cohesive soils with no friction angle, or as granular soils withno cohesion, and is thus the focus of this research. This paper describes a researcheffort to develop practical relationships between Φ’, effective cohesion (c’) and SPTN-values for granular-cohesive soils. Considering the SPT analogous to a miniaturepipe pile, an energy-balance approach was taken to derive a relationship between Φ’,c’, N-values and effective overburden pressure (σ’). A second relationship wasderived between Φ’, c’, σ’ and the liquidity index (LI) of low-sensitivity granularcohesivesoils. The two relationships were then graphically solved to formulate directcorrelations between field N-values and c’ and Φ’.
机译:标准渗透测试(SPT)N值与 内摩擦角(Φ')已开发用于粒状土壤。一些相关性 还开发了用于饱和粘土的不排水剪切强度的材料。然而, 在许多情况下,土壤的行为不像饱和粘土或沙子。有时候 重要的是要发现Φ’在粉砂和沙含量较高的粘土中的作用; 并具有足够的粘土和淤泥含量的沙子的内聚力。这是不正确的 将这些土壤分类为无摩擦角的粘性土壤,或分类为具有 没有凝聚力,因此是本研究的重点。本文介绍了一项研究 努力建立Φ’,有效内聚力(c’)和SPT之间的实用关系 颗粒粘性土壤的N值。将SPT看作是一个缩影 管桩,采用能量平衡的方法来推导Φ’之间的关系, c’,N值和有效上覆压力(σ’)。第二个关系是 取自Φ′,c′,σ′和低灵敏度粒状胶粘剂的流动性指数(LI) 土壤。然后以图形方式解决了这两种关系,以表述直接 字段N值与c’和Φ’之间的相关性。

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