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Failure mechanism of resin anchored rebar in potash2014 July 1900 (has links)
The use of reinforcing bar (rebar) anchored with resin is a common method of rock support in both hard and soft rock mining. The average bond strength, or the load that the support can sustain for a linear length of bond to the rock, is typically determined through a series of pull tests. The average value of bond strength varies widely, since it is dependent on in-situ rock properties and environment. It is an important value because it allows mine engineers to select the appropriate length and pattern spacing of installation for the support. When a stiff support, like resin-anchored rebar, is placed in a weak, soft material, such as potash, the average bond strength tends to be lower in magnitude than for a typical hard rock installation.
This research was primarily aimed at determining the failure mechanism, in soft rock applications, by which the support loses adhesion and begins to fail by sliding. Results of field pull testing determined that the resin-rock bond strength was the limiting factor controlling when adhesion loss occurred. This study investigated how the bond strength may vary given a number of variables typically found in a potash mine environment. Results reported from testing did not indicate variation in the bond strength of resin anchored rebar, significant for mining applications, given changes in resin cure time, vicinity to active mining areas, or the rock type to which the resin was adjacent.
Using the results of laboratory and field testing, an equation was developed to estimate load on in-situ resin anchored rebar given deformation measurements taken from the field. This equation will help determine safe limits for fracture separations opening in the backs of potash drifts. Investigating the behaviour of resin anchored rebar in potash may lead to methods to improve bond strength and calculation of factors of safety for patterned ground support.
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ANALYSIS OF GEOLOGIC STRUCTURE FOR OPEN PIT SLOPE DESIGNCall, Richard Drake, 1934-, Call, Richard Drake, 1934- January 1972 (has links)
No description available.
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Contribution to the analog simulation of particular dynamic phenomena in rock massGlasspoole, Errol Edward January 2001 (has links)
Dissertation submitted in partial compliance with the requirements for Masters Degree in Technology: Electrical Engineering (Light Current), Technikon Natal, 2001. / M
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A study of the effect of mining induced stresses on a fault ahead of an advancing longwall face in a deep level gold mine23 January 2015 (has links)
No description available.
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Investigations into the mechanism of fracture onset and growth in layered rock using physical and numerical modellingDede, Tufan January 2015 (has links)
Thesis (M.Sc.)--University of the Witwatersrand, Faculty of Engineering, 1996 / One of the major impediments in the field of numerical modelling in rock
mechanics is limited knowledge of the mechanisms of fracture and failure of
brittle rock. One important tool for improving the understanding of rock behaviour
is the use of laboratory experiments under controlled conditions.
The Displacement Discontinuity Method, capable of fracture growth simulation
(DIGS), has been used to model fracturing in samples under punch loading. A
Finite Difference Method, capable of plastic deformations due to its explicit time
marching scheme (FLAC), has also been used to model the punch tests.
By comparing numerical simulations with results from laboratory experiments of
punch tests, it has been possible to define the basic failure mechanism for pillar
foundation failure. Two different test set-ups were used namely, steel jacketed
axisymmetric punch tests and long strip punch tests in the triaxial cell which is
built for these specific tests.
The layered structure of the test specimens and in the test procedure had
significant effects on the fracture pattern as well as the failure load. When the
layer is near to the punch area, then both the layer and the layer conditions had a
strong effect on the failure load. When the layer was frictionless, the failure stress
dropped by about 20 percent. The same result occurred in both the axisymmetry
and strip loading tests.
When shear fractures intersect a layer with either low or high friction it
terminates. This is not the case for the tensile fractures, which can pass through
the layer media. However, it is important to note that the tensile fractures which
originate from near the cone area can not pass through the layers. They stop at the
interface.
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Digital image processing-based numerical methods for mechanics of heterogeneous geomaterialsChen, Sha, January 2005 (has links)
Thesis (Ph. D.)--University of Hong Kong, 2006. / Title proper from title frame. Also available in prined format.
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Acoustic emission and crack development in rocksLiu, Hao, January 2000 (has links)
Thesis (Ph. D.)--University of Hong Kong, 2001. / Includes bibliographical references (leaves 170-180).
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Optimal recovery of elastic properties for anisotropic materials through ultrasonic measurements /Sun, Miao. January 2002 (has links) (PDF)
Thesis (M.S.) in Mechanical Engineering--University of Maine, 2002. / Includes vita. Includes bibliographical references (leaves 59-62).
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Predicting rock mass cavability in block caving mines /Mawdesley, Clare A. January 2002 (has links) (PDF)
Thesis (Ph. D.)--University of Queensland, 2002. / Includes bibliographical references.
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Strain analysis of displacement data from the pos selim landslideWong, Koon-yui., 黃冠睿. January 2010 (has links)
published_or_final_version / Applied Geosciences / Master / Master of Science
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