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Field and Laboratory Compressibility Characteristics of Soft Organic Soils in Florida

机译:佛罗里达州软有机土壤的田间和实验室可压缩性特征

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A coordinated field and laboratory investigation was conducted to evaluate the primary and long-term secondary compression characteristics of organic soils and peat existing under SR 15/US 98 in northwest Palm Beach County, Florida. The specific objectives were: (ⅰ) to conduct Piezocone Penetration Tests (CPTu) accompanied with porewater dissipation experiments for predicting the Coefficient of Consolidation ( Cv); (ⅱ) to perform consolidation testing on organic silts and peat collected from various depths at each CPTu location; (ⅲ) to conduct secondary compression tests at constant effective stress representing the in-situ conditions; and (iv) to establish the( Cα / Cc) ratios for Florida organic soils following the well-known Time-Stress-Compressibility concepts. The horizontal coefficient of consolidation (Ch) was predicted from porewater dissipation data, which was subsequently used to calculate the vertical coefficient of consolidation (Cv), and compared with laboratoryderived properties. It was found that the primary consolidation process in laboratory specimens is quite rapid, leading to the secondary compression phase. The Secondary Compression Index, Cα was calculated during the first log cycle after the End-of- Primary (EOP) consolidation, and a unique relationship between Cc and Cα was established. Results indicated that for all practical purposes, the ( Cα / Cc) ratio had constant values ranging from 0.03 to 0.05, which were consistent with the values reported in the literature for similar soils.
机译:进行了现场和实验室的协调研究,以评估在佛罗里达州西北棕榈滩县根据SR 15 / US 98标准存在的有机土壤和泥炭的初级和长期次级压缩特性。具体目标是:(ⅰ)进行压电渗透试验(CPTu),并进行孔隙水耗散实验,以预测固结系数(Cv); (ⅱ)对在各个CPTu地点从不同深度收集的有机淤泥和泥炭进行固结测试; (ⅲ)在代表原位条件的恒定有效应力下进行二次压缩试验; (iv)按照众所周知的时间-压力-可压缩性概念建立佛罗里达州有机土壤的(Cα/ Cc)比。根据孔隙水耗散数据预测水平固结系数(Ch),随后将其用于计算垂直固结系数(Cv),并与实验室衍生的特性进行比较。结果发现,实验室标本的初次固结过程非常迅速,导致了二次压缩阶段。二次压缩指数Cα是在一次病末(EOP)合并后的第一个对数周期内计算的,并且建立了Cc和Cα之间的唯一关系。结果表明,出于所有实际目的,(Cα/ Cc)比的恒定值范围为0.03至0.05,这与文献中报道的相似土壤的值一致。

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