Slope excavation is generally needed when linear infrastructure, such as roads and railways, or other engineering works like canals, pipelines and mining, require the construction of either a level surface on natural slopes or at a pre determined depth below ground level. Slopes are excavated as steeply as ground strength permits while maintaining acceptable stability conditions.
The purpose of site investigations for slopes is to provide a geological and geotechnical description of the area of the proposed excavation, to obtain the parameters needed for stability analysis, slope design and excavation of material, and to design stabilization and drainage measures.
As a general rule, the following aspects should be considered for an excavation:
— Intended dimensions (slope length and depth).
— Position of the water table and hydrogeological conditions, and rainfall.
— Rock and soil types, geological structure and seismicity.
— Project requirements (long or short-term slopes, geometric conditions, etc.)
The site investigations should be adapted to these conditions and take place in stages. Typical procedures include:
The strength properties of materials, soils or rock masses, are obtained from the appropriate in situ and laboratory tests, and the use of empirical criteria and correlations.
Typical laboratory tests used in slope design include those for identification and classification, shear strength in soils and direct shear strength on discontinuities (and paleao-shear surfaces if it is the case), and uniaxial compressive strength.
Where excavation is to be carried out on hilly ground, it is essential to investigate the possible presence of natural landslides, either active or inactive, as engineering work modifies the initial conditions of the slope (geometry, hydrogeology, state of stress, etc.) and may reactivate movement. The presence of pre-existing natural instabilities may modify the excavation design, and if excavation is found not to be feasible, alternative sites must be found. Aspects to be investigated in these cases include the scale and depth of the natural instability, the failure mechanism, the location of slip surfaces and the position of the water table.
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