The present work quantified the laboratory geotechnical variability by repeatability direct shear test (DS) on alluvial fine-grained soils. The effect of laboratory variability of geotechnical parameters (cohesion c' and friction angle ϕ′) on slope stability was investigated. A mixture of compacted fine sand (40%) and clayey silt (60%) taken from a quarry fines stockpile was used: these soils are commonly used to backfill exhausted quarries located in the River Paglia alluvial plain (Central Italy). As knew in the literature, the dry density achieved by a given degree of compaction controls the shear strength parameters affecting the performance of compacted soil. Four direct shear tests were conducted following the ASTM D 3080-72 procedure...
Direct shear test is widely used in soil mechanics experiment to determine the shear strength parame...
This paper studies the reliability of infinite slopes in the presence of spatially variable shear st...
The stability of a slope is governed by the spatial average of the shear strength over the extent of...
Analysis and assessment of the slopes stability are an important in geotechnical engineering for all...
Abstract: The shear strength of soils is essential for any kind of stability analysis. Therefore, it...
Includes bibliographical references (pages 46-47)Previous studies have shown that direct shear tests...
This paper presents a series of direct shear tests performed on a silty sand at three different grav...
Critical and residual states are key soil conditions relevant to slope stability. Evaluating the ava...
Direct shear test is commonly used for research and geotechnical engineering design due to its simpl...
The characteristics of repetitional simple shear test of soils are studied mostly in the case of dyn...
In geotechnical engineering, soil is subject to shear stress, as well as normal stress. In many case...
One of the most important mechanical properties is shear strength. It is conditioned by the value of...
Shear strength of soil is characterized by cohesion, angle of internal friction and dilatation. The ...
The direct shear test using shear box is commonly recommended by practicing geotechnical engineers t...
The usual type of direct shear test apparatus was improved to be sheared repetitionally in order to ...
Direct shear test is widely used in soil mechanics experiment to determine the shear strength parame...
This paper studies the reliability of infinite slopes in the presence of spatially variable shear st...
The stability of a slope is governed by the spatial average of the shear strength over the extent of...
Analysis and assessment of the slopes stability are an important in geotechnical engineering for all...
Abstract: The shear strength of soils is essential for any kind of stability analysis. Therefore, it...
Includes bibliographical references (pages 46-47)Previous studies have shown that direct shear tests...
This paper presents a series of direct shear tests performed on a silty sand at three different grav...
Critical and residual states are key soil conditions relevant to slope stability. Evaluating the ava...
Direct shear test is commonly used for research and geotechnical engineering design due to its simpl...
The characteristics of repetitional simple shear test of soils are studied mostly in the case of dyn...
In geotechnical engineering, soil is subject to shear stress, as well as normal stress. In many case...
One of the most important mechanical properties is shear strength. It is conditioned by the value of...
Shear strength of soil is characterized by cohesion, angle of internal friction and dilatation. The ...
The direct shear test using shear box is commonly recommended by practicing geotechnical engineers t...
The usual type of direct shear test apparatus was improved to be sheared repetitionally in order to ...
Direct shear test is widely used in soil mechanics experiment to determine the shear strength parame...
This paper studies the reliability of infinite slopes in the presence of spatially variable shear st...
The stability of a slope is governed by the spatial average of the shear strength over the extent of...