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ESTIMATING RELATIVE DENSITY OF SANDY SOILS

机译:估算沙土的相对密度

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The applicability of three previous empirical correlations proposed for estimating relative density of sandy soils based on the SPT TV-value, effective overburden stress and soil gradation characteristics was investigated in the present study by using a data base of relative density obtained from high quality undisturbed samples of fine to medium sand with F_c ≦ 20%, D_(50) ≦ 1.0 mm and D_(max) ≦ 4.75 mm. All undisturbed samples were recovered by in-situ freezing method. The relative density estimated by Meyerhof's method (1957) was in the range of +15% ~ -45% of the measured values. Meyerhof's method (1957) was modified by Tokimatsu and Yoshimi (1983) by considering the effect of fines content on the SPT TV-value. The relative density estimated by Tokimatsu and Yoshimi's method (1983) is in the range of + 25% ~ - 20% of the measured values. The underestimation of relative density of Meyerhof's method (1957) was modified. On the contrary, the overestimation of relative density is more significant than Meyerhof's method. The relative density estimated by the method proposed by Kokusho et al. (1983) is in the range of + 20% to - 35% of the measured values even for dense sand with a relative density larger than 60%. Meyerhof's method (1957) and the method proposed by Kokusho et al. (1983) have a common disadvantage that they will extremely underestimate the relative density of fine to medium sand for SPT N-value lower than about 8. The errors in estimation of relative density by these methods are large. A simple empirical correlation (Eq. (10)) was proposed in the present study to estimate the relative density of fine to medium sand based on the normalized SPT N-value, N_1. The relative density estimated by the proposed method is in the range of + 15% to - 30% of the measured values for N_1 in the range between 0 and 50. As a whole, the proposed method is less in errors for estimating relative density compared with those estimated by Meyerhof's method (1957) and the method proposed by Kokusho et al. (1983). Based on a data base of undisturbed samples with data of fines content obtained from the SPT spoon samples, the method proposed by the authors is again compared with the three previous methods. The relative density estimated by the proposed method based on the above data base is in the range of + 15% to - 10% of the measured values. Among four methods, as a whole, the proposed method shows the least errors in estimation of relative density. The proposed method was also modified (Eq. (16)) by taking into account of the effect of fines content of SPT samples. The relative density estimated by the modified method based on the fines content is almost in the range of + 10% to - 10% of the measured values. Two empirical correlations proposed in the present study are less in errors of estimating relative density compared with three previous methods. The range of relative density estimated by the proposed method is well consistent with the range of the measured values (40% to 90%). The empirical correlations proposed in the present study should be applied to fine to medium sand with F_c ≦ 20%, D_(50) ≦ 1.0 mm and D_(max) ≦ 4.75 mm.
机译:本研究利用高质量无扰动样本获得的相对密度数据库,研究了基于SPT TV值,有效上覆应力和土壤等级特征估算沙质土壤相对密度的先前三个经验相关性的适用性。 F_c≤20%,D_(50)≤1.0 mm和D_(max)≤4.75 mm的细砂至中砂。所有原状样品均采用原位冷冻法回收。用Meyerhof方法(1957年)估算的相对密度在测量值的15%〜-45%范围内。 Meyerhof的方法(1957年)由Tokimatsu和Yoshimi(1983年)通过考虑罚款含量对SPT TV值的影响进行了修改。用Tokimatsu和Yoshimi方法(1983)估算的相对密度在测量值的+ 25%〜-20%范围内。修正了对Meyerhof方法(1957年)的相对密度的低估。相反,相对密度的高估比Meyerhof的方法更重要。用Kokusho等人提出的方法估算相对密度。 (1983年)即使在相对密度大于60%的致密砂土中,也处于测量值的+ 20%至-35%范围内。 Meyerhof的方法(1957年)和Kokusho等人提出的方法。 (1983)有一个共同的缺点,那就是当SPT的N值低于8时,它们将大大低估细砂与中砂的相对密度。用这些方法估算相对密度的误差很大。在本研究中,提出了一种简单的经验相关性(等式(10)),以基于标准化的SPT N值N_1估算细砂与中砂的相对密度。通过所提出的方法估计的相对密度在N_1的测量值的+ 15%到-30%的范围内,介于0到50之间。总体而言,所提出的方法与估计的相对密度相比误差较小用Meyerhof的方法(1957年)和Kokusho等人提出的方法进行估算。 (1983)。基于未扰动样本的数据库以及从SPT勺子样本中获得的细粉含量数据,作者提出的方法再次与之前的三种方法进行了比较。通过提出的方法基于上述数据库估算的相对密度在测量值的+ 15%至-10%的范围内。总体而言,在四种方法中,所提出的方法在估计相对密度方面显示出最小的误差。考虑到SPT样品细度的影响,对提出的方法也进行了修改(式(16))。通过改进的方法基于细粉含量估算的相对密度几乎在测量值的+ 10%到-10%的范围内。与以前的三种方法相比,本研究提出的两个经验相关性在估计相对密度方面的误差较小。通过提出的方法估算的相对密度范围与测量值的范围(40%至90%)非常一致。在本研究中提出的经验相关性应适用于F_c≤20%,D_(50)≤1.0 mm和D_(max)≤4.75 mm的中细砂。

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