MASTER IN CIVIL ENGINEERING - Faculdade de Engenharia da ...
MASTER IN CIVIL ENGINEERING - Faculdade de Engenharia da ...
MASTER IN CIVIL ENGINEERING - Faculdade de Engenharia da ...
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Soil Mechanics I<br />
Credits Contact Time Total Time<br />
7 ECTS 75 188<br />
Objectives, Skills and Learning Outcomes<br />
Introduction to the concepts, principles and fun<strong>da</strong>mental theories <strong>de</strong>scribing and<br />
explaining both the mechanical behaviour (in terms of resistance and <strong>de</strong>formability)<br />
and the hydraulic behaviour of soil masses.<br />
Program<br />
Physical properties of soils. Particle size distribution. Clay minerals. Atterberg limits.<br />
Basic features of sedimentary granular soils (sands) and cohesive soils (clays). Residual<br />
soils from granite. Soil classification.<br />
Effective stress principle. At rest stress state. Elastic solutions for stresses induced in<br />
the ground by external loads.<br />
Darcy's law. Coefficient of permeability. Lab and in situ tests to evaluate soil<br />
permeability. Two-dimensional flow nets. Seepage force. Quick condition and critical<br />
hydraulic gradient. Piping and heaving. Filters. Capilarity.<br />
Confined compression of clayey layers. Oedometer test. Parameters <strong>de</strong>fining soil<br />
compressibility. Normally consoli<strong>da</strong>ted and overconsoli<strong>da</strong>ted soils. Estimation of the<br />
consoli<strong>da</strong>tion settlement. Terzaghi theory for vertical consoli<strong>da</strong>tion. Secon<strong>da</strong>ry<br />
consoli<strong>da</strong>tion. Compression of unconfined clay layers. Methods of acceleration of the<br />
consoli<strong>da</strong>tion rate. Observation of embankments on soft ground.<br />
Mohr-Coulomb and Tresca yield criteria. Direct shear, triaxial and simple shear tests.<br />
Shear strength of sands. Liquefaction. Shear strength of clays. Drained and undrained<br />
loading. Effective stress shear strength parameters. Pore pressure parameters.<br />
Undrained shear strength of clays and its <strong>de</strong>pen<strong>de</strong>nce on the effective at-rest stress<br />
and on the stress path. Inherent and induced anisotropy of the undrained shear<br />
strength of clays.<br />
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