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首页> 外文期刊>Journal of geotechnical and geoenvironmental engineering >Interpretation of Cone Penetration Testing in Silty Soils Conducted under Partially Drained Conditions
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Interpretation of Cone Penetration Testing in Silty Soils Conducted under Partially Drained Conditions

机译:在部分排水条件下进行的粉质土壤中的锥形渗透测试的解释

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The standard penetration rate used in cone penetration tests (CPTs) is 20 mm/s, regardless of soil type, which yields fully drained penetration in sand and fully undrained penetration in clay. However, for silty soils that represent an intermediate grain size composition and unique characteristics compared with sand and clay, the standard rate of penetration results in partially drained penetration, often leading to misinterpretation of this soil type. In this study, 15 CPTs, with penetration rates varying from 0.5 to 60 mm/s, were performed at a test site in northern Denmark, where the subsoil consisted primarily of sandy silt with clay bands. The results illustrated that when the penetration rate is reduced, the cone resistance increases, but the pore pressure decreases. The transition between undrained and fully drained penetration was determined by converting the results into a normalized penetration rate. Also evaluated and presented in this paper is how cone resistance obtained under partially drained conditions underestimates the interpreted relative density D_r and friction angle φ. Triaxial test results on undisturbed silt samples were applied for this analysis.
机译:圆锥渗透测试(CPT)中使用的标准渗透速率为20 mm / s,与土壤类型无关,这会导致在沙子中完全排水,而在粘土中完全排水。但是,对于代表中等粒度组成和与沙子和粘土相比具有独特特征的粉质土壤,标准的渗透速率会导致部分排水的渗透,通常会导致对这种土壤类型的误解。在这项研究中,在丹麦北部的一个测试地点进行了15次CPT,渗透速率从0.5到60 mm / s不等,该地下土壤主要由带黏土带的粉砂淤泥组成。结果表明,当渗透率降低时,耐锥性增加,但孔隙压力降低。通过将结果转换为归一化的渗透率,可以确定不排水和完全排水之间的过渡程度。本文还评估并提出了在部分排水条件下获得的锥阻力如何低估了解释的相对密度D_r和摩擦角φ。将原状粉砂样品的三轴试验结果用于此分析。

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