Title:

The Use of 222Rn to Constrain Fracture Characteristics: Experiments Conducted at the Meso-scale Model Geothermal Reservoir Site at Altona, New York

Authors:

John N. CHRISTENSEN, Adam HAWKINS, Shaun T. BROWN, Eric SONNENTHAL, Neil STURCHIO, Donald J. DEPAOLO

Key Words:

radon, isotope tracers, fracture aperture, fracture surface area

Conference:

Stanford Geothermal Workshop

Year:

2017

Session:

Enhanced Geothermal Systems

Language:

English

Paper Number:

Christensen

File Size:

1082 KB

View File:

Abstract:

222Rn, a noble gas with a half-life of 3.8 days produced in the decay-chain of 238U, has the potential to provide constraints on the aperture and surface area of fractures prior to and after EGS stimulation. In order to test and better understand the use of 222Rn in geothermal settings, we have conducted tests at the Altona, NY model geothermal reservoir. The experimental site is situated on an expanse of exposed quartz-cemented Cambrian sandstone with


ec2-18-222-22-244.us-east-2.compute.amazonaws.com, you have accessed 0 records today.

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

Copyright 2017, 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: ec2-18-222-22-244.us-east-2.compute.amazonaws.com (18.222.22.244)
Accessed: Friday 19th of April 2024 03:18:19 PM