2017
DOI: 10.17580/gzh.2017.11.08
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Computer modeling of stress concentration zones for estimation of state of geomaterials

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“…Under the influence of the load in the hole collar of the blast-hole, tensile (up to 506 MPa) and compressive (up to 37 MPa) stresses arise in the hole of the hole. and horizontal (c) sections A similar picture is also observed under the uniaxial quasi-static loading of a rock specimen [19,20]. Since the values of tensile stresses significantly exceed the ultimate tensile strength for ferruginous quartzite ( p = 15 MPa), disturbances can form at the places where these stresses are concentrated, which can lead to the emission of particles that serve as a precursor of the dynamic destruction of the rock.…”
mentioning
confidence: 59%
“…Under the influence of the load in the hole collar of the blast-hole, tensile (up to 506 MPa) and compressive (up to 37 MPa) stresses arise in the hole of the hole. and horizontal (c) sections A similar picture is also observed under the uniaxial quasi-static loading of a rock specimen [19,20]. Since the values of tensile stresses significantly exceed the ultimate tensile strength for ferruginous quartzite ( p = 15 MPa), disturbances can form at the places where these stresses are concentrated, which can lead to the emission of particles that serve as a precursor of the dynamic destruction of the rock.…”
mentioning
confidence: 59%