ASTM D4971-2008 Standard Test Method for Determining In Situ Modulus of Deformation of Rock Using Diametrically Loaded 76-mm (3-in ) Borehole Jack《用径向加载76mm(3in)钻孔顶出装置测量岩石变型模量的标准试验.pdf
《ASTM D4971-2008 Standard Test Method for Determining In Situ Modulus of Deformation of Rock Using Diametrically Loaded 76-mm (3-in ) Borehole Jack《用径向加载76mm(3in)钻孔顶出装置测量岩石变型模量的标准试验.pdf》由会员分享,可在线阅读,更多相关《ASTM D4971-2008 Standard Test Method for Determining In Situ Modulus of Deformation of Rock Using Diametrically Loaded 76-mm (3-in ) Borehole Jack《用径向加载76mm(3in)钻孔顶出装置测量岩石变型模量的标准试验.pdf(7页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D 4971 08Standard Test Method forDetermining In Situ Modulus of Deformation of Rock UsingDiametrically Loaded 76-mm (3-in.) Borehole Jack1This standard is issued under the fixed designation D 4971; the number immediately following the designation indicates the year oforiginal adoption o
2、r, 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 This test method covers the estimation of in situmodulus of a rock mass at va
3、rious depths and orientations.Information on time-dependent deformation may also be ob-tained.1.2 All observed and calculated values shall conform to theguidelines for significant digits and rounding established inPractice D 6026.1.2.1 The method used to specify how data are collected,calculated, or
4、 recorded in this standard is not directly related tothe accuracy to which the data can be applied in design or otheruses, or both. How one applies the results obtained using thisstandard is beyond its scope.1.3 The values stated in SI units are to be regarded as thestandard. The values given in par
5、entheses are mathematicalconversions to inch-pound units that are provided for informa-tion only and are not considered standard.1.4 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
6、 appro-priate safety and health practices and determine the applica-bility of regulatory limitations prior to use.2. Referenced Documents2.1 ASTM Standards:2D 653 Terminology Relating to Soil, Rock, and ContainedFluidsD 3740 Practice for Minimum Requirements for AgenciesEngaged in Testing and/or Ins
7、pection of Soil and Rock asUsed in Engineering Design and ConstructionD 6026 Practice for Using Significant Digits in Geotechni-cal DataD 6032 Test Method for Determining Rock Quality Desig-nation (RQD) of Rock Core3. Terminology3.1 See Terminology D 653 for general definitions.3.2 Definitions of Te
8、rms Specific to This Standard:3.2.1 deformationchange in shape or size, (see Terminol-ogy D 653). In this test method deformation is the change inthe diameter of the borehole.3.2.2 modulus of deformationratio of stress to strain for amaterial under given loading conditions; numerically equal tothe s
9、lope of the tangent or the secant of the stress-strain curve.The use of the term modulus of elasticity is recommended formaterials that deform in accordance with Hookes law, and theterm modulus of deformation is recommended for materialsthat deform otherwise, (see Terminology D 653). In this testmet
10、hod, the modulus of deformation is calculated from theapplied fluid pressure, the relative change in hole diameter, afunction of Poissons ratio, and a constant.3.2.3 jack effciencyratio of the jack plate pressure to theapplied hydraulic pressure.4. Summary of Test Method4.1 The 76 mm (3.0 in.) jacks
11、, (see Fig. 1 and Fig. 2), induceundirectional pressure to the walls of a borehole by means oftwo opposed curved steel platens each covering a 90 sector,over a length of 20.3 cm (8 in.).4.2 Raw data from a test consist of hydraulic-line pressure,Qh, versus readout from linear variable differential t
12、ransform-ers (LVDTs) measuring platen movement. Knowing the dis-placement calibration of the LVDTs, the raw data can betransformed to a test record of hydraulic pressure versus holediameter, D. For each increment of pressure, DQh, and holedeformation, DD, theoretical data analysis (1),3assuming rigi
13、djack plates and full 90 contact, give the theoretical rock massmodulus, E (Etheoretical) as a function E=f (D QhDD T*),where T* is a coefficient dependent upon Poissons ratio. If Eis measured on a linear segment of the loading curve, common1This test method is under the jurisdiction ofASTM Committe
14、e D18 on Soil andRock and is the direct responsibility of Subcommittee D18.12 on Rock Mechanics.Current edition approved July 1, 2008. Published July 2008. Originally approvedin 1989. Last previous edition approved in 2006 as D 4971 02 (2006).2For referenced ASTM standards, visit the ASTM website, w
15、ww.astm.org, orcontact ASTM Customer Service at serviceastm.org. For Annual Book of ASTMStandards volume information, refer to the standards Document Summary page onthe ASTM website.3The boldface numbers in parentheses refer to a list of references at the end ofthe standard.1*A Summary of Changes se
16、ction appears at the end of this standard.Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959, United States.terminology is modulus of deformation. If E is measured on anunloading linear segment, it is referred to as the recoverymodulus.5. Significance
17、and Use5.1 Results of this test method are used to predict displace-ments in rock mass caused by loads from a structure or fromunderground construction. It is one of several tests that shouldbe performed.5.2 Because the jack can apply directed loads, this testmethod can be performed to provide an es
18、timate of anisotropy.5.3 In theory, the analysis of test data is straight forward; themodulus estimate requires a record of applied hydraulicpressure versus borehole diameter change, and a knowledge ofthe rocks Poissons ratio. In practice, the above procedure,using the original theoretical formula,
19、frequently has resultedin computing a material modulus that was demonstrably toolow.5.4 For analyzing the test data it is assumed that the rockmass is linearly elastic, isotropic, and homogeneous. Withinthese assumptions, this test method can provide useful data forrock masses for which equivalent c
20、ontinuous properties can notbe found or estimated.NOTE 1Notwithstanding the statements on precision and bias con-tained in this test method; the precision of this test method is dependenton the competence of the personnel performing it, and the suitability of theequipment and facilities used. Agenci
21、es that meet the criteria of PracticeD 3740 are generally considered capable of competent and objectivetesting. Users of this test method are cautioned that compliance withPractice D 3740 does not in itself assure reliable testing. Reliable testingdepends on many factors; Practice D 3740 provides a
22、means of evaluatingsome of those factors.6. Interferences6.1 It is assumed that the tensile and compressive moduli ofthe rock are equal and there is no tensile cracking induced inthe rock mass because of jack loading. If tensile cracks arecreated at 90 to the loading direction, it has been shown (1)
23、that the calculated modulus values can decrease by up to 29 %.Therefore, tensile cracking would result in a decrease in theslope of the loading curve and test data in the region ofdecreased slope should not be used.6.2 The volume of rock mass involved in the 76 mm (3.0in.) diameter jack test has bee
24、n estimated (2) to be about 0.15m3(5 ft3). This volume may not include enough discontinuitiesto be representative of the rock mass on a larger scale.6.3 Two aspects of jack behavior, discussed in 6.3.1 and6.3.2, require careful consideration in the analysis of test dataand can be compensated for by
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