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Qhafor Ameen Hamasur

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Chapter One<br />

Introduction<br />

4- Determining water table level.<br />

5- Transporting the core samples to the laboratory for detailed study.<br />

6- Determining the altitude and fixing the location of the boreholes by<br />

GPSMAP 60CSx.<br />

1-5-2- Laboratory work<br />

Laboratory work included petrographic inspection, determining the strength<br />

properties of the rocks (from surface sections and boreholes), furthermore other<br />

descriptive and numerical studies were done on boreholes.<br />

Petrographic inspection included making thin sections for study under the<br />

microscope, then classifying the carbonate rocks in the dam site according to<br />

Folk’s (1962) classification which is suitable for the Hoek-Brown failure criterion<br />

elements, such as material constant (mi) and modulus ratio (MR) of intact rock.<br />

The strength properties included conducting the point load and the unconfined<br />

(uniaxial) compression tests to find the unconfined compressive strength of the<br />

intact rock.<br />

The descriptive and numerical studies on boreholes comprised information<br />

about GSI and counting the number of discontinuities and measuring their dip<br />

angle with respect to the borehole axis in each rock mass unit.<br />

1-5-3- Office work<br />

The office work included representation and analysis of the field and<br />

laboratory information and measurements, wherein some rock mass classification<br />

parameters which were obtained descriptively were converted into rated<br />

parameters, such as GSI, discontinuities roughness, weathering of the<br />

discontinuity surfaces, infilling material, discontinuity persistence, water condition<br />

and discontinuities orientation.<br />

Other parameters that were obtained numerically were also rated according<br />

to the weight of each one in the classification system, such as uniaxial<br />

compressive strength, RQD and discontinuity spacing. Furthermore some<br />

7

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