Scholarly record
ESTIMATION OF COMPRESSIVE STRENGTH LIMIT AND MODULUS OF DEFORMATION OF LAYERED ARTIFICIAL AND NATURAL GEOMATERIALS USING REGRESSION RELATIONSHIPS
Abstract
Rocks can be structurally represented as layered bodies, whereby the layers can be located at different orientation angles with respect to the original ground. Such angles are usually called the bedding angles. To avoid mistakes in the calculations of the stress-strain state of rock massifs, it is very important to take into account the dependencies of mechanical properties of layered rocks on the bedding angle. Also, rocks are at a certain depth under hydrostatic compression conditions. For an adequate simulation of the mechanical behavior of rocks, a triaxial compression test is used. Depending on the depth at which the core was selected, a confining pressure is applied to the wall of the cylindrical rock sample. Previously, the authors worked on this topic. This research is a continuation of the last one. On the basis of experimental data on the study of the mechanical properties of artificial geomaterials, meta-siltstone and schist, multiple nonlinear regression relationships were constructed. As the regression factors for assessing the strength and modulus of deformation of the examined geomaterials, the bedding angles and the confining pressure values were used.
Publication Impact Profile
Publication details
References0
Structured references will appear here after the reference import pass. The count is preserved now so the scholarly record is not incomplete.
View or Download full articleAccess options
SWS access login
Login as SWS Scientific CommitteeLogin as SWS Scientific PartnerLogin as SWS AuthorAuthors and approved SWS contributors will read and export their own linked papers after identity matching by SWS profile, email and SGEM GlobalID.
For librarian assistance: [email protected]
Purchase Instant Access
- Article can be downloaded after successful payment.
- Article may be used according to SWS library access terms.
- Article cannot be redistributed.

