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Title: Tube-wave seismic imaging

Abstract

The detailed analysis of cross well seismic data for a gas reservoir in Texas revealed two newly detected seismic wave effects, recorded approximately 2000 feet above the reservoir. A tube-wave (150) is initiated in a source well (110) by a source (111), travels in the source well (110), is coupled to a geological feature (140), propagates (151) through the geological feature (140), is coupled back to a tube-wave (152) at a receiver well (120), and is and received by receiver(s) (121) in either the same (110) or a different receiving well (120). The tube-wave has been shown to be extremely sensitive to changes in reservoir characteristics. Tube-waves appear to couple most effectively to reservoirs where the well casing is perforated, allowing direct fluid contact from the interior of a well case to the reservoir.

Inventors:
 [1]
  1. LaFayette, CA
Issue Date:
Research Org.:
Yucca Mountain Project, Las Vegas, NV (United States)
Sponsoring Org.:
USDOE
OSTI Identifier:
988156
Patent Number(s):
7529151
Application Number:
11/058,985
Assignee:
The Regents of the University of California (Oakland, CA)
Patent Classifications (CPCs):
G - PHYSICS G01 - MEASURING G01V - GEOPHYSICS
DOE Contract Number:  
AC03-76SF00098
Resource Type:
Patent
Country of Publication:
United States
Language:
English
Subject:
58 GEOSCIENCES

Citation Formats

Korneev, Valeri A. Tube-wave seismic imaging. United States: N. p., 2009. Web.
Korneev, Valeri A. Tube-wave seismic imaging. United States.
Korneev, Valeri A. Tue . "Tube-wave seismic imaging". United States. https://www.osti.gov/servlets/purl/988156.
@article{osti_988156,
title = {Tube-wave seismic imaging},
author = {Korneev, Valeri A},
abstractNote = {The detailed analysis of cross well seismic data for a gas reservoir in Texas revealed two newly detected seismic wave effects, recorded approximately 2000 feet above the reservoir. A tube-wave (150) is initiated in a source well (110) by a source (111), travels in the source well (110), is coupled to a geological feature (140), propagates (151) through the geological feature (140), is coupled back to a tube-wave (152) at a receiver well (120), and is and received by receiver(s) (121) in either the same (110) or a different receiving well (120). The tube-wave has been shown to be extremely sensitive to changes in reservoir characteristics. Tube-waves appear to couple most effectively to reservoirs where the well casing is perforated, allowing direct fluid contact from the interior of a well case to the reservoir.},
doi = {},
journal = {},
number = ,
volume = ,
place = {United States},
year = {2009},
month = {5}
}

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Works referenced in this record:

Analysis and attenuation of tube waves in crosswell seismic survey
conference, March 2012


Borehole seismic modeling with inclusion of tube waves and other tube‐wave‐related arrivals
conference, March 2012