Title:

A Fully Integrated EGS Evaluation Workflow

Authors:

Baptiste LEPILLIER, Alexandros DANIILIDIS, Francesco PARISIO, Keita YOSHIOKA, Pierre-Olivier BRUNA, David BRUHN

Key Words:

hydraulic fracture propagation, phase-field, stimulation, natural fracture, scanline, discrete fracture network, gemex

Conference:

Stanford Geothermal Workshop

Year:

2020

Session:

Enhanced Geothermal Systems

Language:

English

Paper Number:

Lepillier

File Size:

1835 KB

View File:

Abstract:

The development of an EGS is one of the goals of the GEMex project, an international collaboration of two consortia, one from Europe and one from Mexico. The research is based on exploration, characterization and assessment of two geothermal systems located in the Trans-Mexican volcanic belt, Los Humeros and Acoculco. Los Humeros has been a producing field for several years, but Acoculco is yet to be developed. Thanks to surface manifestations of hydrothermal activities, the existence of a geothermal system is evident. However, two wells reached very high temperatures, but did not find any fluids. For that reason, the Acoculco Caldera is foreseen as EGS development site, hoping to connect existing wells to a productive zone. In this study, we develop a workflow that aims at assessing the feasibility of this EGS. The approach aims at generating a realistic predictive mechanical model for fracture stimulation from the well borehole. The strength of the method stands in the combination of reliable data obtained from field work and experimental measurements on mechanical properties of the target rocks, used together to populate a numerical model. The workflow starts with the identification and description of the surface discontinuities using the scanline survey method. These surveys are interpolated and extrapolated using the multiple point statistics method to generate geological discrete fracture networks. These discrete fracture networks, together with the mechanical properties measured in the rock physics laboratory are then used to analyze the fracture propagation and its interaction with the pre-existing natural fractures. The results of the hydraulic fracture propagation simulations are then used in a finite element method program to evaluate the heat and fluid flow transfer, comparing reservoir properties before and after treatment. The method offers a physically sound prediction of the reservoir flow characteristics as well as an accurate mechanical model of the fracture propagation and the pressure distribution for well borehole stimulation. Because the workflow is based on easily accessible data and thanks to its simplicity, this approach could be applied in most EGS case studies.


ec2-3-135-202-224.us-east-2.compute.amazonaws.com, you have accessed 0 records today.

Press the Back button in your browser, or search again.

Copyright 2020, Stanford Geothermal Program: Readers who download papers from this site should honor the copyright of the original authors and may not copy or distribute the work further without the permission of the original publisher.


Attend the nwxt Stanford Geothermal Workshop, click here for details.

Accessed by: ec2-3-135-202-224.us-east-2.compute.amazonaws.com (3.135.202.224)
Accessed: Friday 26th of April 2024 02:23:13 PM