• Title/Summary/Keyword: contact zone composite sample

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Effect of material mechanical differences on shear properties of contact zone composite samples: Experimental and numerical studies

  • Wang, Weiqi;Ye, Yicheng;Wang, Qihu;Liu, Xiaoyun;Yang, Fan;Tan, Wenkan
    • Structural Engineering and Mechanics
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    • v.76 no.2
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    • pp.153-162
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    • 2020
  • Aiming at the mechanical and structural characteristics of the contact zone composite rock, the shear tests and numerical studies were carried out. The effects of the differences in mechanical properties of different materials and the normal stress on shear properties of contact zone composite samples were analyzed from a macro-meso level. The results show that the composite samples have high shear strength, and the interface of different materials has strong adhesion. The differences in mechanical properties of materials weakens the shear strength and increase the shear brittleness of the sample, while normal stress will inhibit these effect. Under low/high normal stress, the sample show two failure modes, at the meso-damage level: elastic-shearing-frictional sliding and elastic-extrusion wear. This is mainly controlled by the contact and friction state of the material after damage. The secondary failure of undulating structure under normal-shear stress is the nature of extrusion wear, which is positively correlated to the normal stress and the degree of difference in mechanical properties of different materials. The increase of the mechanical difference of the sample will enhance the shear brittleness under lower normal stress and the shear interaction under higher normal stress.

Interaction and mechanical effect of materials interface of contact zone composite samples: Uniaxial compression experimental and numerical studies

  • Wang, Weiqi;Ye, Yicheng;Wang, Qihu;Luo, Binyu;Wang, Jie;Liu, Yang
    • Geomechanics and Engineering
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    • v.21 no.6
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    • pp.571-582
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    • 2020
  • Aiming at the mechanical and structural characteristics of the contact zone composite rock, the uniaxial compression tests and numerical studies were carried out. The interaction forms and formation mechanisms at the contact interfaces of different materials were analyzed to reveal the effect of interaction on the mechanical behavior of composite samples. The research demonstrated that there are three types of interactions between the two materials at the contact interface: constraint parallel to the interface, squeezing perpendicular to the interface, and shear stress on the interface. The interaction is mainly affected by the differences in Poisson's ratio and elastic modulus of the two materials, stronger interface adhesion, and larger interface inclination. The interaction weakens the strength and stiffness of the composite sample, and the magnitude of weakening is positively correlated with the degree of difference in the mechanical properties of the materials. The tensile-shear stress derived from the interaction results in the axial tensile fracture perpendicular to the interface and the interfacial shear facture. Tensile cracks in stronger material will propagation into the weaker material through the bonded interface. The larger inclination angle of the interface enhances the effect of composite tensile/shear failure on the overall sample.

장풍 폐광산의 산성광산폐수에 의한 침출수 유동에 대한 지구물리 및 지화학탐사자료의 상관해석

  • Kim, Ji-Su;Han, Su-Hyeong;Choe, Sang-Hun;Lee, Gyeong-Ju;Lee, In-Gyeong;Lee, Pyeong-Gu
    • Journal of the Korean Geophysical Society
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    • v.5 no.1
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    • pp.19-27
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    • 2002
  • Geophysical surveys(self-potential, electromagnetic, electrical resistivity, and seismic refraction methods) were performed to delineate the flow channel of leachate from a AMD (acid mine drainage) by correlating the anomalies to geochemical characteristics at an abandoned mine (Jangpoong mine). The geophysical responses attempted to be correlated with water sample analysis data(pH, EC, heavy metals, ${SO_4}^{-2}$). Electrical dipole-dipole resistivity sections represent the low-resistivity zone trending northwest, which indicates the leachate flow by AMD along the contact of the mine waste rock dump and the bedrock. From the overall points of geophysical and geochemical anomalies, it is summarized that the flow channel of leachate by AMD can be successfully imaged with composite interpretations on the geophysical and geochemical studies.

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