1987
DOI: 10.1016/0148-9062(87)90526-2
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Sandblast testing of rock

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Cited by 21 publications
(13 citation statements)
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“…They differ from lateral cracks formed in isotropic brittle materials (see Table 4, upper row). This particular feature agrees with observations reported in [12] for a number of rock materials; this author attributed it to the existence of pre-existing cracks. Lateral vent cracks do not grow to the free surface immediately, but follow either weak mineral interfaces or pre-existing cracks.…”
Section: Resultssupporting
confidence: 91%
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“…They differ from lateral cracks formed in isotropic brittle materials (see Table 4, upper row). This particular feature agrees with observations reported in [12] for a number of rock materials; this author attributed it to the existence of pre-existing cracks. Lateral vent cracks do not grow to the free surface immediately, but follow either weak mineral interfaces or pre-existing cracks.…”
Section: Resultssupporting
confidence: 91%
“…As can be seen in Fig. 3d, the calcitic matrix between impact sites is exposed, and the material is removed [12,13]; "L" -Laterally cracked sections. (d) Fracture marks in quartz.…”
Section: Resultsmentioning
confidence: 99%
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“…He reviewed the qualitative relationship between petrography and the polishing of both natural and artificial aggregates. Verhoef [3] between petrographic properties and mechanical behavior of aggregates during re-texturing treatment.…”
Section: Introductionmentioning
confidence: 99%
“…Verhoef [10] attempted to use grit-blasting as a method to determine the resistance of rocks against abrasive wear. The author installed a so-called 'Sandblast Index' that may allow direct comparison of 204 A. W. Momber grit-blasting data.…”
Section: Introductionmentioning
confidence: 99%