ASTM D2845-08
(Test Method)Standard Test Method for Laboratory Determination of Pulse Velocities and Ultrasonic Elastic Constants of Rock (Withdrawn 2017)
Standard Test Method for Laboratory Determination of Pulse Velocities and Ultrasonic Elastic Constants of Rock (Withdrawn 2017)
SIGNIFICANCE AND USE
The primary advantages of ultrasonic testing are that it yields compression and shear wave velocities, and ultrasonic values for the elastic constants of intact homogeneous isotropic rock specimens (3). Elastic constants are not to be calculated for rocks having pronounced anisotropy by procedures described in this test method. The values of elastic constants often do not agree with those determined by static laboratory methods or the in situ methods. Measured wave velocities likewise may not agree with seismic velocities, but offer good approximations. The ultrasonic evaluation of rock properties is useful for preliminary prediction of static properties. The test method is useful for evaluating the effects of uniaxial stress and water saturation on pulse velocity. These properties are in turn useful in engineering design.
The test method as described herein is not adequate for measurement of stress-wave attenuation. Also, while pulse velocities can be employed to determine the elastic constants of materials having a high degree of anisotropy, these procedures are not treated herein.
Note 2—The quality of the result produced by this standard is dependent on the competence of the personnel performing it, and the suitability of the equipment and facilities used. Agencies that meet the criteria of Practice D 3740 are generally considered capable of competent and objective testing and sampling. Users of this standard are cautioned that compliance with Practice D 3740 does not in itself assure reliable results. Reliable results depend on many factors; Practice D 3740 provides a means of evaluating some of those factors.
SCOPE
1.1 This test method describes equipment and procedures for laboratory measurements of the pulse velocities of compression waves and shear waves in rock (1) and the determination of ultrasonic elastic constants (Note 1) of an isotropic rock or one exhibiting slight anisotropy.
Note 1—The elastic constants determined by this test method are termed ultrasonic since the pulse frequencies used are above the audible range. The terms sonic and dynamic are sometimes applied to these constants but do not describe them precisely (2). It is possible that the ultrasonic elastic constants may differ from those determined by other dynamic methods.
1.2 This test method is valid for wave velocity measurements in both anisotropic and isotropic rocks although the velocities obtained in grossly anisotropic rocks may be influenced by such factors as direction, travel distance, and diameter of transducers.
1.3 The ultrasonic elastic constants are calculated from the measured wave velocities and the bulk density. The limiting degree of anisotropy for which calculations of elastic constants are allowed and procedures for determining the degree of anisotropy are specified.
1.4 The values stated in inch-pound units are to be regarded as standard. The values given in parentheses are mathematical conversions to SI units that are provided for information only and are not considered standard.
1.5 This standard does not purport to address all of the safety concerns, if any, associated with its use. It is the responsibility of the user of this standard to establish appropriate safety and health practices and determine the applicability of regulatory limitations prior to use.
WITHDRAWN RATIONALE
This test method describes equipment and procedures for laboratory measurements of the pulse velocities of compression waves and shear waves in rock and the determination of ultrasonic elastic constants of an isotropic rock or one exhibiting slight anisotropy.
Formerly under the jurisdiction of Committee D18 on Soil and Rock, this test method was withdrawn in January 2017 in accordance with section 10.6.3 of the Regulations Governing ASTM Technical Committees, which requires that standards shall be updated by the end of the eighth year since the last approval date.
General Information
Standards Content (Sample)
NOTICE: This standard has either been superseded and replaced by a new version or withdrawn.
Contact ASTM International (www.astm.org) for the latest information
Designation: D2845 − 08
Standard Test Method for
Laboratory Determination of Pulse Velocities and Ultrasonic
1
Elastic Constants of Rock
This standard is issued under the fixed designation D2845; the number immediately following the designation indicates the year of
original adoption or, in the case of revision, the year of last revision.Anumber in parentheses indicates the year of last reapproval.A
superscript epsilon (´) indicates an editorial change since the last revision or reapproval.
1. Scope* 2. Referenced Documents
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1.1 This test method describes equipment and procedures 2.1 ASTM Standards:
for laboratory measurements of the pulse velocities of com- D653Terminology Relating to Soil, Rock, and Contained
2
pression waves and shear waves in rock (1) and the determi- Fluids
nation of ultrasonic elastic constants (Note 1) of an isotropic D2216TestMethodsforLaboratoryDeterminationofWater
rock or one exhibiting slight anisotropy. (Moisture) Content of Soil and Rock by Mass
D3740Practice for Minimum Requirements for Agencies
NOTE 1—The elastic constants determined by this test method are
Engaged in Testing and/or Inspection of Soil and Rock as
termed ultrasonic since the pulse frequencies used are above the audible
Used in Engineering Design and Construction
range. The terms sonic and dynamic are sometimes applied to these
constants but do not describe them precisely (2). It is possible that the
D6026Practice for Using Significant Digits in Geotechnical
ultrasonic elastic constants may differ from those determined by other
Data
dynamic methods.
E691Practice for Conducting an Interlaboratory Study to
1.2 This test method is valid for wave velocity measure-
Determine the Precision of a Test Method
ments in both anisotropic and isotropic rocks although the
3. Terminology
velocities obtained in grossly anisotropic rocks may be influ-
enced by such factors as direction, travel distance, and diam-
3.1 For common definitions of terms in this standard, refer
eter of transducers.
to Terminology D653.
1.3 The ultrasonic elastic constants are calculated from the
3.2 Definitions of Terms Specific to This Standard:
measured wave velocities and the bulk density. The limiting
3.2.1 compression wave velocity—the dilational wave ve-
degreeofanisotropyforwhichcalculationsofelasticconstants
locity which is the propagation velocity of a longitudinal wave
are allowed and procedures for determining the degree of
inamediumthatiseffectivelyinfiniteinlateralextent.Itisnot
anisotropy are specified.
to be confused with bar or rod velocity.
1.4 Thevaluesstatedininch-poundunitsaretoberegarded
4. Summary of Test Method
as standard. The values given in parentheses are mathematical
conversions to SI units that are provided for information only
4.1 Details of essential procedures for the determination of
and are not considered standard. the ultrasonic velocity, measured in terms of travel time and
distance, of compression and shear waves in rock specimens
1.5 This standard does not purport to address all of the
include requirements of instrumentation, suggested types of
safety concerns, if any, associated with its use. It is the
transducers, methods of preparation, and effects of specimen
responsibility of the user of this standard to establish appro-
geometry and grain size. Elastic constants may be calculated
priate safety and health practices and determine the applica-
for isotropic or slightly anisotropic rocks, while anisotropy is
bility of regulatory limitations prior to use.
reported in terms of the variation of wave velocity with
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direction in the rock.
ThistestmethodisunderthejurisdictionofASTMCommitteeD18onSoiland
Rock and is the direct responsibility of Subcommittee D18.12 on Rock Mechanics.
CurrenteditionapprovedJuly1,2008.PublishedJuly2008.Originallyapproved
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in 1969. Last previous edition approved in 2005 as D2845 – 05. DOI: 10.1520/ For referenced ASTM standards, visit the ASTM website, www.astm.org, or
D2845-08. contact ASTM Customer Service at service@astm.org. For Annual Book of ASTM
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Theboldfacenumbersinparenthesesrefertothelistofreferencesattheendof Standards volume information, refer to the standard’s Document Summary page on
this test method. the ASTM website.
*A Summary of Changes section appears at the end of this standard
Copyright © ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959. United States
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D2845 − 08
5. Significance and Use rectangular pulse or a gated sine wave is satisfactory. The
generator shall have a voltage output with a maximum value
5.1 The primary advantages of ultrasonic testing are that it
afteramplificationofatleast50Vintoa50-Ωimpedanceload.
yields compression and shear wave velocities, and ultrasonic
Avariable pulse width, with a range of 1 t
...
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