2020
DOI: 10.1061/ajrua6.0001083
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Scale of Fluctuation for Spatially Varying Soils: Estimation Methods and Values

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Cited by 94 publications
(37 citation statements)
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“…As mentioned in the introduction section, an important part of identifying the uncertainty of soil strength parameters in modeling them using a random field is identifying the scale of fluctuation. A typical method of determining the SOF based on CPT results [ 17 , 23 ] includes fitting the assumed theoretical ACF (with the SOF being the fitting parameter) to the so-called experimental ACF. The values of the latter are calculated for subsequent values of the lag distance between observations in CPT profile (multiplication of observation interval Δ τ ) τj = j Δ τ , j εN , as [ 24 ]: where is the single observation of the parameter for which the scale is determined, k is the number of observations in the sample, and μ and ν 2 denote the mean value and variance of the observations.…”
Section: Methodsmentioning
confidence: 99%
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“…As mentioned in the introduction section, an important part of identifying the uncertainty of soil strength parameters in modeling them using a random field is identifying the scale of fluctuation. A typical method of determining the SOF based on CPT results [ 17 , 23 ] includes fitting the assumed theoretical ACF (with the SOF being the fitting parameter) to the so-called experimental ACF. The values of the latter are calculated for subsequent values of the lag distance between observations in CPT profile (multiplication of observation interval Δ τ ) τj = j Δ τ , j εN , as [ 24 ]: where is the single observation of the parameter for which the scale is determined, k is the number of observations in the sample, and μ and ν 2 denote the mean value and variance of the observations.…”
Section: Methodsmentioning
confidence: 99%
“…The values of the latter are calculated for subsequent values of the lag distance between observations in CPT profile (multiplication of observation interval Δ τ ) τj = j Δ τ , j εN , as [ 24 ]: where is the single observation of the parameter for which the scale is determined, k is the number of observations in the sample, and μ and ν 2 denote the mean value and variance of the observations. According to the method [ 17 , 20 , 23 ], before applying Equation (14), all observations need to be initially detrended and normalized (trends and mean values are determined separately for each CPT).…”
Section: Methodsmentioning
confidence: 99%
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“…The single exponential correlation function is utilized in this paper because it is the most frequently used model in characterizing the spatial correlation of soil properties. 38 The choice of the form of covariance function and the values of statistical characteristics (e.g., variance and correlation length) represent the problem-specific prior information. The adopted covariance function does not limit the proposed method.…”
Section: Simulation Of Random Fields Based On the Karhunen-loève Expansionmentioning
confidence: 99%
“…The values of vertical and horizontal correlation length are set to 1 m and 20 m, respectively. 38,51 The exponential correlation function is adopted since it is the most commonly used autocorrelation model for soil. 38 The schematic diagram of the numerical model is shown in Figure 2, including the geometries, loading conditions, boundary conditions, and meshes.…”
Section: Numerical Casementioning
confidence: 99%