
Borehole seismic surveys, including down-hole and cross-hole methodologies (in 2D and 3D configurations), are high-resolution geophysical techniques used to characterize the elastic properties of soils and rocks in situ.
These methods make it possible to accurately determine the propagation velocities of elastic waves (P-waves and S-waves) along known depths, as well as to calculate key geotechnical parameters, such as shear modulus, Young’s modulus, and compressibility modulus.
The investigation is based on the insertion of a seismic source and triaxial geophones inside one or more boreholes. In the down-hole configuration, the source is placed at the surface, while the geophones are lowered progressively in depth; in contrast, in the cross-hole configuration, both the source and the sensors are inserted in separate holes at the same depth, allowing direct velocity measurement between two known points. In the 3D cross-hole variant, the use of multiple holes arranged in complex geometric configurations allows for a three-dimensional reconstruction of the volume being investigated, which is particularly useful in advanced engineering and the design of strategic works.
Fields of Application:
Computation of dynamic parameters of soils
Seismostratigraphic reconstruction
Searching for cavities
Verification of soil consolidation effectiveness
Definition of water-table depth
Verification of elastic properties of artificial fills, embankments, and levees
Fields of Application:
Computation of dynamic parameters of soils
Seismostratigraphic reconstruction
Searching for cavities
Verification of soil consolidation effectiveness
Definition of water-table depth
Verification of elastic properties of artificial fills, embankments, and levees
Discover the other seismic methods:
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