使用 Rahardjo (2016) 方法评估 CPTu 的固结度 - 东加里曼丹固结土壤案例研究

Edwin Lie
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引用次数: 0

摘要

在东加里曼丹的一处工地进行了岩土工程勘察,包括 13 次 CPTu 和 23 次消能测试,原因是 75 米高的覆盖层堤坝下 15 至 30 米厚的软粘土引发了滑坡。调查覆盖了堤坝脚下约 250 米 x 275 米宽的区域。从地质图上看,该地点位于巴厘巴板地层(Tmbp)和甘榜巴鲁地层(Tpkb)的交界处,附近还有日利森时期的冲积层(Qa)。渗透测量显示孔隙水压力高于静水压力。耗散测试结果表明,软粘土仍在固结,残余过剩孔隙压力(uf)仍然存在。Rahardjo (2016) 方法以 CPTu 数据为基础,尤其是软粘土数据,用于确定过固结率 (OCR)。不过,该方法也可用于确定固结程度。该方法使用孔隙压力比 (Bq) 值,即过剩孔隙压力除以锥体净阻力 - Bq = Δu/(qt - σv0),该值是在进行 CPTu 试验时获得的。提出的计算公式为 1/(1.2Bq+0.1)。该方法指出,Bq 值=0.75 等于 OCR=1,表明粘土固结正常。Bq 值高于 0.75 将显示固结土壤的固结程度,而 Bq 值低于 0.75 将显示过度固结土壤的 OCR 值。将 Rahardjo(2016 年)方法应用于所执行的耗散数据,结果显示与土壤仍在固结的软粘土一致。然而,当应用于接近地表的过固结土壤时,该方法将显示出更大的 OCR 值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Evaluation of Consolidation Degree from CPTu using Rahardjo (2016) Method – Case Study of Consolidating Soil in East Kalimantan
A geotechnical investigation comprised 13 CPTu and 23 dissipation testing were performed on a site in East Kalimantan due to landslide triggered by 15 to 30m thick soft clay underlying 75m high overburden embankment. The investigation covers an area of about 250m x 275m wide on the area next to the toe of the embankment. From geological map, the site situated at borders of Balikpapan Formation (Tmbp) and Kampung Baru Formation (Tpkb) with Alluvium (Qa) formation from Heliosen period nearby. Measurement from penetration showed high pore-water pressure higher than the hydrostatic pressure. Result from dissipation testing showed that the soft clay is still consolidating with residual excess pore pressure (uf) still exist. Rahardjo (2016) Method was developed using CPTu data as its basis especially soft clay data to determine overconsolidation ratio (OCR). However, it can also be used to determine the degree of consolidation. The method uses Pore Pressure Ratio (Bq) value, excess pore pressure divided by net cone resistance – Bq = Δu/(qt – σv0), which was obtained when performing CPTu test. The formula proposed was 1/(1.2Bq+0.1). The method stated that the value of Bq=0.75 equals to OCR=1 which is showing a normally consolidated clay. Bq value higher than 0.75 will show a degree of consolidation of a consolidating soil and for Bq value lower than 0.75 will show an OCR value of overconsolidated soil. Applying Rahardjo (2016) Method to the dissipation data performed showed an agreement on soft clay where the soil is still consolidating. However, when applied to over consolidated soil near surface this method will show a greater OCR value.
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