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HDR Reservoir Analysis Incorporating Acoustic Emission Data

J. Willis-Richards, K. Watanabe, T. Yamaguchi, Y. Sato, S. Takasugi

Location
Hijiori, Japan; Cornwall, United Kingdom
Conference
Stanford Geothermal Workshop
Year
1995
Session
Hot Dry Rock
Language
English

Full text

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Abstract

A set of models of HDR systems is presented which attempts to explain the formation and operation of HDR systems using only the in-situ properties of the fractured rock mass, the earth stress field, the engineering intervention applied by way of stimulation and the relative positions and pressures of the well(s). A statistical and rock mechanics description of fractures in low permeability rocks provides the basis for modeling of stimulation, circulation and water loss in HDR systems. The model uses a large number of parameters, chiefly simple directly measurable quantities, describing the rock mass and fracture system. The effect of stimulation (raised fluid pressure allowing slip) on fracture apertures is calculated, and the volume of rock affected per volume of fluid pumped estimated. The total rock volume affected by stimulation is equated with the rock volume containing the associated AE (microseismicity). The aperture and compliance properties of the stimulated fractures are used to estimate impedance and flow within the reservoir. Fluid loss from the boundary of the stimulated volume is treated using radial leak-off with pressure-dependent permeability. The model is applied to HDR stimulation and circulation experiments carried out at Rosemanowes, UK (1983- 1989) and at Hijiori, Japan (1986-1991).

Copyright 1995, Stanford Geothermal Program. 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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