ASTM D7012-2007 Standard Test Method for Compressive Strength and Elastic Moduli of Intact Rock Core Specimens under Varying States of Stress and Temperatures《在变化的应力和温度下完整岩石芯样抗压强度和.pdf
《ASTM D7012-2007 Standard Test Method for Compressive Strength and Elastic Moduli of Intact Rock Core Specimens under Varying States of Stress and Temperatures《在变化的应力和温度下完整岩石芯样抗压强度和.pdf》由会员分享,可在线阅读,更多相关《ASTM D7012-2007 Standard Test Method for Compressive Strength and Elastic Moduli of Intact Rock Core Specimens under Varying States of Stress and Temperatures《在变化的应力和温度下完整岩石芯样抗压强度和.pdf(8页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D 7012 07Standard Test Method forCompressive Strength and Elastic Moduli of Intact RockCore Specimens under Varying States of Stress andTemperatures1This standard is issued under the fixed designation D 7012; the number immediately following the designation indicates the year oforiginal
2、 adoption or, in the case of revision, the year of last revision. A number in parentheses indicates the year of last reapproval. Asuperscript epsilon (e) indicates an editorial change since the last revision or reapproval.1. Scope1.1 This test method covers the determination of thestrength of intact
3、 rock core specimens in uniaxial compressionand confined compression. The tests provide data in determin-ing the strength of rock, namely: the uniaxial strength, shearstrengths at varying pressures and varying temperatures, angleof internal friction, (angle of shearing resistance), and cohesioninter
4、cept. The test method specifies the apparatus, instrumen-tation, and procedures for determining the stress-axial strainand the stress-lateral strain curves, as well asYoungs modulus,E, and Poissons ratio, y. It should be observed that this methodmakes no provision for pore pressure measurements ands
5、pecimens are undrained (platens are not vented). Thus thestrength values determined are in terms of total stress, that is,are not corrected for pore pressures. This test method does notinclude the procedures necessary to obtain a stress-strain curvebeyond the ultimate strength.1.1.1 This standard re
6、places and combines the followingStandard Test Methods for: D 2664 Triaxial CompressiveStrength of Undrained Rock Core Specimens Without PorePressure Measurements; D 5407 Elastic Moduli of UndrainedRock Core Specimens in Triaxial Compression Without PorePressure Measurements; D 2938 Unconfined Compr
7、essiveStrength of Intact Rock Core Specimens; and D 3148 ElasticModuli of Intact Rock Core Specimens in Uniaxial Compres-sion.1.1.2 The original four standards are now referred to asMethods in this standard as follows: Method A TriaxialCompressive Strength of Undrained Rock Core SpecimensWithout Por
8、e Pressure Measurements; Method B ElasticModuli of Undrained Rock Core Specimens in Triaxial Com-pression Without Pore Pressure Measurements; Method C Unconfined Compressive Strength of Intact Rock Core Speci-mens; Method D Elastic Moduli of Intact Rock CoreSpecimens in Uniaxial Compression; and Opt
9、ionA ElevatedTemperatures.1.2 For an isotropic material, the relation between the shearand bulk moduli and Youngs modulus and Poissons ratio are:G 5E21 1y!(1)K 5E31 2 2y!(2)where:G = shear modulus,K = bulk modulus,E = Youngs modulus, andy = Poissons ratio.1.2.1 The engineering applicability of these
10、 equations de-creases with increasing anisotropy of the rock. It is desirable toconduct tests in the plane of foliation, cleavage or bedding andat right angles to it to determine the degree of anisotropy. It isnoted that equations developed for isotropic materials may giveonly approximate calculated
11、 results if the difference in elasticmoduli in two orthogonal directions is greater than 10 % for agiven stress level.NOTE 1Elastic moduli measured by sonic methods (Test MethodD 2845) may often be employed as preliminary measures of anisotropy.1.3 This test method given for determining the elasticc
12、onstants does not apply to rocks that undergo significantinelastic strains during the test, such as potash and salt. Theelastic moduli for such rocks should be determined fromunload-reload cycles, that are not covered by this test method.1.4 The values stated in SI units are to be regarded as thesta
13、ndard.1.5 This standard does not purport to address all of thesafety concerns, if any, associated with its use. It is theresponsibility of the user of this standard to establish appro-priate safety and health practices and determine the applica-bility of regulatory limitations prior to use.1This tes
14、t method is under the jurisdiction ofASTM Committee D18 on Soil andRock and is the direct responsibility of Subcommittee D18.12 on Rock Mechanics.Current edition approved July 1, 2007. Published July 2007. Originally approvedin 2004. Last previous edition approved in 2004 as D 701204e1.1Copyright AS
15、TM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959, United States.2. Referenced Documents2.1 ASTM Standards:2D 2216 Test Methods for Laboratory Determination of Wa-ter (Moisture) Content of Soil and Rock by MassD 2845 Test Method for Laboratory Determination of Pu
16、lseVelocities and Ultrasonic Elastic Constants of RockD 3740 Practice for Minimum Requirements for AgenciesEngaged in the Testing and/or Inspection of Soil and Rockas Used in Engineering Design and ConstructionD 4543 Practices for Preparing Rock Core as CylindricalTest Specimens and Verifying Confor
17、mance to Dimen-sional and Shape TolerancesE4 Practices for Force Verification of Testing MachinesE 122 Practice for Calculating Sample Size to Estimate,With a Specified Tolerable Error, the Average for aCharacteristic of a Lot or Process2.2 ASTM Adjunct:3Triaxial Compression Chamber Drawings (3)3. S
18、ummary of Test Method3.1 A rock core specimen is cut to length and the ends aremachined flat. The specimen is placed in a loading frame andif required, placed in a loading chamber and subjected toconfining pressure. In an elevated temperature test the speci-men is heated to the desired test temperat
19、ure. Axial load isincreased continuously on the specimen, and deformation ismeasured as a function of load until peak load and failure areobtained.4. Significance and Use4.1 The parameters obtained from these procedures are interms of undrained total stress (as already mentioned in 1.1.1.).However,
20、there are some cases where either the rock type orthe loading condition of the problem under consideration willrequire the effective stress or drained parameters be deter-mined.4.2 Unconfined compressive strength of rock is used inmany design formulas and is sometimes used as an indexproperty to sel
21、ect the appropriate excavation technique. Defor-mation and strength of rock are known to be functions ofconfining pressure. The confined compression test is com-monly used to simulate the stress conditions under which mostunderground rock masses exist. The elastic constants are usedto calculate the
22、stress and deformation in rock structures.4.3 The deformation and strength properties of rock coresmeasured in the laboratory usually do not accurately reflectlarge-scale in situ properties because the latter are stronglyinfluenced by joints, faults, inhomogeneities, weakness planes,and other factor
23、s. Therefore, laboratory values for intactspecimens must be employed with proper judgment in engi-neering applications.NOTE 2Notwithstanding the statements on precision and bias con-tained in this test method; the measures of precision of these test methodsare dependent on the competence of the pers
24、onnel performing them, andon the suitability of the equipment and facilities used. Agencies that meetthe criteria of Practice D 3740 are generally considered capable ofcompetent and objective testing. Users of this test method are cautionedthat compliance with Practice D 3740 does not in itself assu
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