Soil Mechanics in Engineering Practice Lectures
Pdf Lectures, Solutions & course notes on Soil Mechanics Full Course (Text)
Soil Mechanics Introduction and Definition
Soil mechanics is defined as the application of the laws and principles of mechanics and hydraulics to engineering problems dealing with soil as an engineering material. Soil has many different meanings, depending on the field of study. To a geotechnical engineer, soil has a much broader meaning and can include not only agronomic material, but also broken-up fragments of rock, volcanic ash, alluvium, Aeolian sand, glacial material, and any other residual or transported product of rock weathering.
As the name Soil Mechanics implies the subject is concerned with the deformation and strength of bodies of soil. It deals with the mechanical properties of the soil materials and with the application of the knowledge of these properties to engineering problems. In particular it is concerned with the interaction of structures with their foundation material. This includes both conventional structures and also structures such as earth dams, embankments and roads which are their-selves made of soil.
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Constituents of Soil Sand, Silt, Gravel, Stones Types of Soil Dry, Saturated, Partially saturated, Coarse, Fine, Organic, Gravel, Sand, Clay, Silt, Boulders, Cobbels, Peat Properties Voids ratio, Porosity, Degree of Saturation, Air Content, Water Content, Unit weight, Bulk unit weight, Specific Gravity, saturated unit weight
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The grain-size characteristics of soils that are predominantly coarse grained are evaluated by a sieve analysis A nest of sieves is prepared by stacking sieves one above the other with the largest opening at the top followed by sieves of successively smaller openings and a catch pan at the bottom of all the sieves |
There are two soil classification systems in common use for engineering purposes.
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Both immediate and consolidation settlement analysis requires estimate of increase in pressure (ΔHσ) in the soil layers from the applied loads. Several methods are available to estimate the increase in pressure at any depth z from the applied load. ..... [Read More] We will discuss:
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Compaction is the application of mechanical energy to a soil to rearrange the particles and reduce the void ratio.. [Read More] |
Modes of Shear Failure in Soil | Earth Pressure |
There are three modes of shear failure, i.e. General, Local and Punching shear failures depending upon the compressibility of soil and depth of footing with respect to its breadth (i.e D/B Ratio). When the ultimate bearing capacity of the soil is reached, it may fail in one of the following three failure mode depending upon the type of soil and depth to width ratio of the footing (i.e. D/B)......... [Read More] |
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A soil shear failure can result in excessive building distortion and even collapse. Excessive settlements can result in structural damage to a building frame nuisances such as sticking doors and windows, cracks in tile and plaster, and excessive wear or equipment failure from misalignment resulting from foundation settlements. It is necessary to investigate both base shear resistance (ultimate bearing capacity) and settlements for any structure. In many cases settlement criteria will control the allowable bearing capacity...... [Read More] |
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The soil properties on which their classification and identification are based are known as index properties..... [Read More] The index properties which are used are:
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Plastic saturated soils (silts and clays) usually have lower shear strength than non-plastic cohesion less soil and are more susceptible to bearing capacity failure. For saturated plastic soils, the bearing capacity often has to be calculated for different conditionTotal Stress Analysis (Short term condition) that uses the un-drained shear strength of the plastic soil. Effective stress analysis (Long term condition that uses the drained shear strength parameters (c' & F') of the plastic soil).... [Read More] |
Soils derive their strength from contact between particles capable of transmitting normal as well as shear forces. The contact between soil particles is mainly due to friction and the corresponding stress between the soil grains is called the effective stress s'. Thus, the shear strength of a soil is mainly governed by the effective stress. Besides the effective stress between soil grains, the pore water contained in the void spaces of the soil also exerts pressure which is known as pore pressure, u. [Read More] |
This testing method is used as an integral part of several engineering classifications systems to characterize the fine‑grained fractions of soils and to specify the fine‑grained fraction of construction materials. The liquid limit, plastic limit and plasticity index of soils are also used extensively, either individually or together, with other soil properties to correlate with engineering behavior such as compressibility, permeability, compactibility, shrink‑swell and shear strength..... [Read More] |