ASTM D7012-2010 0000 Standard Test Method for Compressive Strength and Elastic Moduli of Intact Rock Core Specimens under Varying States of Stress and Temperatures《完整岩芯样本在不同应力和温度条件.pdf
《ASTM D7012-2010 0000 Standard Test Method for Compressive Strength and Elastic Moduli of Intact Rock Core Specimens under Varying States of Stress and Temperatures《完整岩芯样本在不同应力和温度条件.pdf》由会员分享,可在线阅读,更多相关《ASTM D7012-2010 0000 Standard Test Method for Compressive Strength and Elastic Moduli of Intact Rock Core Specimens under Varying States of Stress and Temperatures《完整岩芯样本在不同应力和温度条件.pdf(9页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D7012 10Standard Test Method forCompressive Strength and Elastic Moduli of Intact RockCore Specimens under Varying States of Stress andTemperatures1This standard is issued under the fixed designation D7012; the number immediately following the designation indicates the year oforiginal a
2、doption or, in the case of revision, the year of last revision. A number in parentheses indicates the year of last reapproval. Asuperscript epsilon () indicates an editorial change since the last revision or reapproval.1. Scope*1.1 These test methods cover the determination of thestrength of intact
3、rock core specimens in uniaxial and triaxialcompression. The tests provide data in determining the strengthof rock, namely: the uniaxial strength, shear strengths atdifferent pressures and different elevated temperatures, angleof internal friction, (angle of shearing resistance), and cohesioninterce
4、pt. The test methods specify 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 thesemethods make no provision for pore pressure measurementsand spe
5、cimens are undrained (platens are not vented). Thus thestrength values determined are in terms of total stress, that is,are not corrected for pore pressures. These test methods do notinclude the procedures necessary to obtain a stress-strain curvebeyond the ultimate strength.1.2 This standard replac
6、es and combines the followingStandard Test Methods: D2664 Triaxial Compressive Strengthof Undrained Rock Core Specimens Without Pore PressureMeasurements; D5407 Elastic Moduli of Undrained Rock CoreSpecimens in Triaxial Compression Without Pore PressureMeasurements; D2938 Unconfined Compressive Stre
7、ngth ofIntact Rock Core Specimens; and D3148 Elastic Moduli ofIntact Rock Core Specimens in Uniaxial Compression. Theoriginal four standards are now referred to as Methods in thisstandard.1.2.1 Method A: Triaxial Compressive Strength of Und-rained Rock Core Specimens Without Pore Pressure Measure-me
8、nts.1.2.2 Method B: Elastic Moduli of Undrained Rock CoreSpecimens in Triaxial Compression Without Pore PressureMeasurements.1.2.3 Method C: Uniaxial Compressive Strength of IntactRock Core Specimens.1.2.4 Method D: Elastic Moduli of Intact Rock Core Speci-mens in Uniaxial Compression.1.2.5 Option A
9、: Elevated Temperatures.1.3 For an isotropic material in Test Methods B and D, therelation between the shear and bulk moduli and Youngsmodulus 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.1.3.1 The engineering a
10、pplicability of these 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 a
11、pproximate calculated 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 MethodD2845) may often be employed as a preliminary measure of anisotropy.1.4 Test Methods B and D for deter
12、mining the elasticconstants do 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.1This test method is under the jurisdiction o
13、fASTM Committee D18 on Soil andRock and is the direct responsibility of Subcommittee D18.12 on Rock Mechanics.Current edition approved Jan. 15, 2010. Published March 2010. Originallyapproved in 2004. Last previous edition approved in 2007 as D701207e1. DOI:10.1520/D7012-10.1*A Summary of Changes sec
14、tion appears at the end of this standard.Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959, United States.1.5 The values stated in SI units are to be regarded asstandard. No other units of measurement are included in thisstandard.1.6 All observed and
15、calculated values shall conform to theguidelines for significant digits and rounding established inPractice D6026.1.7 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 s
16、afety and health practices and determine the applica-bility of regulatory limitations prior to use.2. Referenced Documents2.1 ASTM Standards:2D653 Terminology Relating to Soil, Rock, and ContainedFluidsD2216 Test Methods for Laboratory Determination of Wa-ter (Moisture) Content of Soil and Rock by M
17、assD2845 Test Method for Laboratory Determination of PulseVelocities and Ultrasonic Elastic Constants of RockD3740 Practice for Minimum Requirements for AgenciesEngaged in Testing and/or Inspection of Soil and Rock asUsed in Engineering Design and ConstructionD4543 Practices for Preparing Rock Core
18、as CylindricalTest Specimens and Verifying Conformance to Dimen-sional and Shape TolerancesD6026 Practice for Using Significant Digits in GeotechnicalDataE4 Practices for Force Verification of Testing MachinesE122 Practice for Calculating Sample Size to Estimate,With Specified Precision, the Average
19、 for a Characteristicof a Lot or Process2.2 ASTM Adjunct:3Triaxial Compression Chamber Drawings (3)3. Terminology3.1 Refer to Terminology D653 for specific definitions.4. Summary of Test Method4.1 A rock core specimen is cut to length and the ends aremachined flat. The specimen is placed in a loadin
20、g 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 temperature. Axial load isincreased continuously on the specimen, and deformation ismeasured as a function of load until peak load and f
21、ailure areobtained.5. Significance and Use5.1 The parameters obtained from Methods A and B are interms of undrained total stress (as already mentioned in 1.1).However, there are some cases where either the rock type orthe loading condition of the problem under consideration willrequire the effective
22、 stress or drained parameters be deter-mined.5.2 Uniaxial compressive strength (Method C) of rock isused in many design formulas and is sometimes used as anindex property to select the appropriate excavation technique.Deformation and strength of rock are known to be functions ofconfining pressure. T
23、he triaxial compression test (MethodA) iscommonly used to simulate the stress conditions under whichmost underground rock masses exist. The elastic constants(Methods B and D) are used to calculate the stress anddeformation in rock structures.5.3 The deformation and strength properties of rock coresm
24、easured 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 factors. Therefore, laboratory values for intactspecimens must be employed with proper judgment in engi-ne
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