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Title: Preliminary results of a seismic borehole test using downhole shaped charges at the DOE Hanford Site

Abstract

Geophysical site characterization studies can be important steps in the process of designing and monitoring remediation at hazardous waste storage facilities. Use of seismic techniques for subsurface characterization at the DOE Hanford Site has been limited. One reason is the lack of borehole velocity control, and low-velocity sediments are highly attenuative. Consequently, standard techniques to provide velocity control are not adequate. Both Vertical Seismic Profiling and reversed VSP surveys are currently being investigated to provide velocity control and for subsurface imaging capabilities. Recently a jet perforating gun was used to perforate a doubled-cased borehole in the 200 West Area. Acoustic emissions were recorded from numerous depths to obtain velocity control for a previous surface survey conducted in the same area. Both P- and S-wave data were recorded simultaneously from multiple horizons using the DAS-1 seismograph and 3-component geophones. The data were analyzed for a variety of uses besides velocity control. Signal attenuation was studied as a function of source depth and offset distance to evaluate formation absorption while vertical resolution was determined from the frequency spectrum. Preliminary results indicate that adequate P-wave velocity control can be obtained even though the near-surface sediments are very attenuative. However, we conclude that themore » perforating gun produces little SH energy. Preliminary velocities indicate that reflection coefficients should be great enough to use surface techniques. Results from the frequency study suggest that a swept source for both surface and borehole surveys may be necessary to obtain required resolutions. Finally, signal attenuation as a function of formation facies suggest that seismic techniques may be useful in mapping perched water zones and for long term vadose zone monitoring.« less

Authors:
 [1];  [2]
  1. Westinghouse Hanford Co., Richland, WA (United States)
  2. Oyo Geospace Corp., Houston, TX (United States). Engineering Geophysics Div.
Publication Date:
Research Org.:
Westinghouse Hanford Co., Richland, WA (United States)
Sponsoring Org.:
USDOE, Washington, DC (United States)
OSTI Identifier:
10133093
Report Number(s):
WHC-SA-2304; CONF-940353-4
ON: DE94008077; BR: 35AF11201/35AF11202
DOE Contract Number:  
AC06-87RL10930
Resource Type:
Conference
Resource Relation:
Conference: Symposium on the application of geophysics to environmental and engineering problems,Boston, MA (United States),27-31 Mar 1994; Other Information: PBD: Feb 1994
Country of Publication:
United States
Language:
English
Subject:
11 NUCLEAR FUEL CYCLE AND FUEL MATERIALS; 54 ENVIRONMENTAL SCIENCES; 58 GEOSCIENCES; HANFORD RESERVATION; SEISMIC SURVEYS; RADIOACTIVE WASTE FACILITIES; REMEDIAL ACTION; SEISMIC P WAVES; SEISMIC S WAVES; ACOUSTIC MEASUREMENTS; SEISMIC SOURCES; SHAPED CHARGES; UNDERGROUND EXPLOSIONS; BOREHOLES; 054000; 540250; 580000; HEALTH AND SAFETY; SITE RESOURCE AND USE STUDIES; GEOSCIENCES

Citation Formats

Narbutovskih, S M, and Michelsen, F. Preliminary results of a seismic borehole test using downhole shaped charges at the DOE Hanford Site. United States: N. p., 1994. Web.
Narbutovskih, S M, & Michelsen, F. Preliminary results of a seismic borehole test using downhole shaped charges at the DOE Hanford Site. United States.
Narbutovskih, S M, and Michelsen, F. 1994. "Preliminary results of a seismic borehole test using downhole shaped charges at the DOE Hanford Site". United States. https://www.osti.gov/servlets/purl/10133093.
@article{osti_10133093,
title = {Preliminary results of a seismic borehole test using downhole shaped charges at the DOE Hanford Site},
author = {Narbutovskih, S M and Michelsen, F},
abstractNote = {Geophysical site characterization studies can be important steps in the process of designing and monitoring remediation at hazardous waste storage facilities. Use of seismic techniques for subsurface characterization at the DOE Hanford Site has been limited. One reason is the lack of borehole velocity control, and low-velocity sediments are highly attenuative. Consequently, standard techniques to provide velocity control are not adequate. Both Vertical Seismic Profiling and reversed VSP surveys are currently being investigated to provide velocity control and for subsurface imaging capabilities. Recently a jet perforating gun was used to perforate a doubled-cased borehole in the 200 West Area. Acoustic emissions were recorded from numerous depths to obtain velocity control for a previous surface survey conducted in the same area. Both P- and S-wave data were recorded simultaneously from multiple horizons using the DAS-1 seismograph and 3-component geophones. The data were analyzed for a variety of uses besides velocity control. Signal attenuation was studied as a function of source depth and offset distance to evaluate formation absorption while vertical resolution was determined from the frequency spectrum. Preliminary results indicate that adequate P-wave velocity control can be obtained even though the near-surface sediments are very attenuative. However, we conclude that the perforating gun produces little SH energy. Preliminary velocities indicate that reflection coefficients should be great enough to use surface techniques. Results from the frequency study suggest that a swept source for both surface and borehole surveys may be necessary to obtain required resolutions. Finally, signal attenuation as a function of formation facies suggest that seismic techniques may be useful in mapping perched water zones and for long term vadose zone monitoring.},
doi = {},
url = {https://www.osti.gov/biblio/10133093}, journal = {},
number = ,
volume = ,
place = {United States},
year = {Tue Feb 01 00:00:00 EST 1994},
month = {Tue Feb 01 00:00:00 EST 1994}
}

Conference:
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