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Water Flow Impedance through a Fracture Made by Hydraulic Pressure

Hideo Kobayashi, Yasuki Oikawa and Isao Matsunaga

Key words
flow impedance, hydraulic fracture, fracture aperture, hot dry rock
Location
Hijiori, Japan; Inada, Japan
Conference
World Geothermal Congress
Year
1995
Session
SECTION 12 - Advanced Technologies (HDR - Magma - Geopressur
Language
English
Paper number
4-Kobayashi

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Abstract

The of these studies are collect basic data on the deformation of rock samples during the extension of a hydraulic fracture and on the fracture deformation during injection of water into a fracture. Inada granite was used for the tests. The deformation of the rock samples were measured by several LVDTs and pai-gauges in order to estimate initial fracture width and the mean aperture of hydraulic fractures The Rock deformations during the hydraulic fracturing considered to be equal to the fracture aperture were about 209 independent whether the fractures were created parallel to the rift plane or parallel to the hardway plane During cyclic loading of the fractures the amplitude of fracture displacement decreased and flow impedance in the fracture increased

Copyright 1995, International Geothermal Association. Readers who download papers from this site should honour the copyright of the original authors, and may not copy or distribute the work further without the permission of the original publisher.

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