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8 <br /> <br />C U <br />2.~c <br />[9] <br />Consequently, the determination of U and Tan B or k from Equation <br />[7] by linear regression methods and the subsequent calculation <br />of ~' and C using Equation [8] and [9] is perhaps a simpler and <br />more straight forward method than plotting the Mohr envelope. <br />Direct Shear Strength. The direct shear strength of a rock <br />core may be envisioned as the shear strength which results when <br />the normal stress is zero. In other words, the shear strength <br />of a rock could be approximated as the cohesion at zero normal <br />stress. Therefore, an estimate of cohesion may be made by test- <br />ing a rock core in direct shear. The specific test used in the <br />study is known as the double shear test and is defined as follows: <br />D P <br />~ [10] <br />• <br />where P ~ load at failure <br />A ~ cross sectional core area <br />Brazilian Tensile Strength. The Brazilian or indirect <br />tensile strength of a rock is determined by loading a disc of <br />rock in compression across the diameter. The Brazilian tensile <br />strength (B) is then computed as follows: <br />$ 2P [11] <br />4DL <br />where P ~ load at failure <br />D ~ sample diameter <br />L ~ sample thickness <br />Flesural Strength. The flexural or outer fiber tensile <br />strength was determined by a bending test. The test involves <br />,. <br />SEEGMILLER INTERNATIONAL <br />