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Abstracts Book - IMRC 2018

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• SD2-P001<br />

PHYSICAL ASPECTS AND MODELING OF THE FRACTURE IN ROCKS<br />

AND CEMENTITIOUS MATERIALS<br />

Omar Rodriguez Villarreal 1,2<br />

1 Universidad Autónoma de Nuevo León, Facultad de Ingeniera Civil, Mexico. 2 Universite de pau<br />

et des pays de ladour, Institut Supérieur Aquitain du Bâtiment et des Travaux Publics, France.<br />

The purpose of this research is to study the fracture surfaces of a complex<br />

network of fractures generated by means of hydraulic fracture or hydrostatic<br />

pressure under conditions presented in an Enhanced Geothermal System<br />

(EGS). Fractures generated by hydrostatic pressure are a particular class of<br />

mode I tensile fractures, which grow by the coalescence of micro-cracks. By<br />

studying this type of fracturing process, it is possible to improve the<br />

performance of a geothermal field. The present work will focus on rocks typical<br />

of geothermal reservoirs, shale and limestone rocks, as well as concrete and<br />

mortar since we can refer to these composite materials as synthetic rocks. We<br />

will study the effects of the internal structure of the material, the confinement<br />

stress, temperature and fluid injection flow rate on the mechanical properties<br />

of rock formation, (i.e., tensile and compression strength, fracture energy, etc.),<br />

the geometry of the fracture network generated, the roughness of such<br />

fractures and the acoustic emission during the hydraulic fracture.<br />

Keywords: Fracture, Andesite rock and concrete, Enhanced Geothermal System<br />

Presenting authors email: omar_rdzv@hotmail.com

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