Abstract:There are many methods for determining precompression stress (σ p ), whose value is affected by the slope of the soil compression curve. This study was designed to evaluate the hypothesis that for a certain compression curve all methods used to determine σ p present the same value and accuracy. The aim of this study was to compare the accuracy and the relationship among seven of these methods by computational simulation of soil compression curves under nine scenarios. The following methods were used: Casagrand… Show more
“…Pearson correlation coefficient. *p-value < 0.01 by t-test The linear and positive impacts of BD on σ p have also been observed by Imhoff et al (2004), Saffih-Hdadi et al (2009, Lima et al (2015Lima et al ( , 2016 and Schjønning & Lamandé (2018). Imhoff et al (2004) attributed the positive effect of BD to the increase of the frictional forces in the soil mass and explained that these forces impede the displacement and separation of the particles under stress, increasing the load-bearing capacity of the soil.…”
Section: Resultsmentioning
confidence: 65%
“…The resistance of soil to compaction is assumed as the precompression stress (σ p ) (Stettler et al, 2014;Schjønning & Lamandé, 2018), which can be obtained via the compression curve. The determination of σ p is complex and time-consuming (Lima et al, 2016;Schjønning & Lamandé, 2018), and therefore, pedo-transfer functions have been used to estimate σ p as a function of soil physical parameters, which can be easily obtained in the field (Schjønning & Lamandé, 2018). Water content (Oliveira et al, 2011;Severiano et al, 2013) and soil bulk density (Lima et al, 2015) are significantly correlated with σ p .…”
Compressive soil properties are typically used for the understanding of compaction process. As an alternative to laboratory tests, pedo-transfer functions have been used to estimate the mechanical behaviour of soil as a function of soil physical parameters. The impact of soil bulk density (BD) and gravimetric water content (w) was examined on soil strength and pedo-transfer functions were proposed to predict the precompression stress (σp) in an Ultisol cultivated with sugarcane. Undisturbed soil cores were sampled at the depths of 0-0.20 and 0.20-0.40 m, subjected to different water contents, and subsequently, compression tests were performed to determine σp. The data were subjected to analysis of variance and regression analysis. Bulk density and w affected σp positively and negatively, respectively. Approximately 70% of the variation of the σp could be explained as a function of BD and w through an accessible multiple regression model. Comparisons with other pedo-transfer functions showed that estimates of σp may be rather sensitive to soil management and textural classes. Variations imposed by soil management and cohesive character into depth suggest that independent models should be considered to characterise compressive behaviour of soil by horizon or layer.
“…Pearson correlation coefficient. *p-value < 0.01 by t-test The linear and positive impacts of BD on σ p have also been observed by Imhoff et al (2004), Saffih-Hdadi et al (2009, Lima et al (2015Lima et al ( , 2016 and Schjønning & Lamandé (2018). Imhoff et al (2004) attributed the positive effect of BD to the increase of the frictional forces in the soil mass and explained that these forces impede the displacement and separation of the particles under stress, increasing the load-bearing capacity of the soil.…”
Section: Resultsmentioning
confidence: 65%
“…The resistance of soil to compaction is assumed as the precompression stress (σ p ) (Stettler et al, 2014;Schjønning & Lamandé, 2018), which can be obtained via the compression curve. The determination of σ p is complex and time-consuming (Lima et al, 2016;Schjønning & Lamandé, 2018), and therefore, pedo-transfer functions have been used to estimate σ p as a function of soil physical parameters, which can be easily obtained in the field (Schjønning & Lamandé, 2018). Water content (Oliveira et al, 2011;Severiano et al, 2013) and soil bulk density (Lima et al, 2015) are significantly correlated with σ p .…”
Compressive soil properties are typically used for the understanding of compaction process. As an alternative to laboratory tests, pedo-transfer functions have been used to estimate the mechanical behaviour of soil as a function of soil physical parameters. The impact of soil bulk density (BD) and gravimetric water content (w) was examined on soil strength and pedo-transfer functions were proposed to predict the precompression stress (σp) in an Ultisol cultivated with sugarcane. Undisturbed soil cores were sampled at the depths of 0-0.20 and 0.20-0.40 m, subjected to different water contents, and subsequently, compression tests were performed to determine σp. The data were subjected to analysis of variance and regression analysis. Bulk density and w affected σp positively and negatively, respectively. Approximately 70% of the variation of the σp could be explained as a function of BD and w through an accessible multiple regression model. Comparisons with other pedo-transfer functions showed that estimates of σp may be rather sensitive to soil management and textural classes. Variations imposed by soil management and cohesive character into depth suggest that independent models should be considered to characterise compressive behaviour of soil by horizon or layer.
“…Other studies have focused on investigating the methods applied in determination of σ p and pedotransfer functions (Dias Junior and Pierce, 1996;Imhoff et al, 2004;Cavalieri et al, 2008;Suzuki et al, 2008;Severiano et al, 2011;Silva and Lima, 2016).…”
ABSTRACT:In irrigated soils, a continuous state of high moisture reduces resistance of the soil to applied external forces, favouring compaction. The aim of this study was to evaluate the susceptibility to compaction of developed calcareous soils in irrigated annual and perennial cropping systems of the Apodi Plateau, located in the Brazilian semi-arid region. Four areas of irrigated crops were evaluated: banana after two (B2) and 15 (B15) years cultivation, pasture (P), and a corn and beans succession (MB), as well as the reference areas for soil quality and corresponding natural vegetation (NVB2, NVB15, NVP and NVMB). Samples were collected at layers of 0.00-0.10 and 0.20-0.30 m; and for B2 and B15, samples were collected in the row and inter-row spaces. The following properties were determined: degree of compactness (DC), preconsolidation pressure (σ p ), compression index (Cc), maximum density (ρ max ), critical water content (WC crit ), total organic carbon (TOC) and carbon of light organic matter (C lom ). Mean values were compared by the t-test at 5, 10, 15 and 20 % probability. An increase was seen in DC at a layer of 0.20-0.30 m in MB (p<0.15), showing the deleterious effects of preparing the soil by ploughing and chiselling, together with the cumulative traffic of heavy machinery. The TOC had a greater influence on ρ max than the stocks of C lom . Irrigation caused a reduction in Cc, and there was no effect on σ p at field capacity. The planting rows showed different behaviour for Cc, ρ max , and WC crit, , and in general the physical properties displayed better conditions than the inter-row spaces. Values for σ p and Cc showed that agricultural soils display greater load-bearing capacity and are less susceptible to compaction in relation to soils under natural vegetation.
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