ASTM D4623-2008 Standard Test Method for Determination of In Situ Stress in Rock Mass by Overcoring Method&x2014 USBM Borehole Deformation Gauge《用钻套法-美国矿务局(USBM)钻孔变形计现场测定岩石质量的标准试验方.pdf
《ASTM D4623-2008 Standard Test Method for Determination of In Situ Stress in Rock Mass by Overcoring Method&x2014 USBM Borehole Deformation Gauge《用钻套法-美国矿务局(USBM)钻孔变形计现场测定岩石质量的标准试验方.pdf》由会员分享,可在线阅读,更多相关《ASTM D4623-2008 Standard Test Method for Determination of In Situ Stress in Rock Mass by Overcoring Method&x2014 USBM Borehole Deformation Gauge《用钻套法-美国矿务局(USBM)钻孔变形计现场测定岩石质量的标准试验方.pdf(14页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D 4623 08Standard Test Method forDetermination of In Situ Stress in Rock Mass by OvercoringMethodUSBM Borehole Deformation Gauge1This standard is issued under the fixed designation D 4623; the number immediately following the designation indicates the year oforiginal adoption or, in the
2、 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 determination of the ambi-ent local stresses in a rock mas
3、s and the equipment required toperform in situ stress tests using a three-component boreholedeformation gauge (BDG). The test procedure and method ofdata reduction are described, including the theoretical basis andassumptions involved in the calculations. A section is includedon troubleshooting equi
4、pment malfunctions.NOTE 1The gauge used in this test method is commonly referred to asa USBM gauge (U.S. Bureau of Mines three-component borehole defor-mation gauge).21.2 The values stated in inch-pound units are to be regardedas standard. No other units of measurement are included in thisstandard.1
5、.3 This standard does not purport to address all of thesafety problems, 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.2. Referenced Do
6、cuments2.1 ASTM Standards:3D 653 Terminology Relating to Soil, Rock, and ContainedFluidsD 3740 Practice for Minimum Requirements for AgenciesEngaged in Testing and/or Inspection of Soil and Rock asUsed in Engineering Design and ConstructionD 4394 Test Method for Determining the In Situ Modulusof Def
7、ormation of Rock Mass Using the Rigid PlateLoading MethodD 4395 Test Method for Determining In Situ Modulus ofDeformation of Rock Mass Using Flexible Plate LoadingMethodD 6026 Practice for Using Significant Digits in Geotechni-cal DataD 7012 Test Method for Compressive Strength and ElasticModuli of
8、Intact Rock Core Specimens under VaryingStates of Stress and Temperatures3. Terminology3.1 Definitions: See Terminology D 653 for general defini-tions.3.2 Definitions:3.2.1 deformationdisplacement change in dimension ofthe borehole due to changes in stress.3.2.2 in situ stressthe stress levels and o
9、rientations exist-ing in the rock mass before excavation.4. Summary of Test Method4.1 The overcore test measures the diametral deformation ofa small-diameter borehole as it is removed from the surround-ing stress field by coaxially coring a larger diameter hole.Deformation is measured across three d
10、iameters of the smallhole, spaced 60 apart, using a deformation gauge developedby the U.S. Bureau of Mines. With knowledge of the rockdeformation moduli, the measured borehole deformation canbe related to the change in stress in a plane perpendicular to theborehole. This change in stress is assumed
11、to be numericallyequal, although opposite in sense to the stresses existing in theparent rock mass. Deformation measurements from threenonparallel boreholes, together with rock deformation moduli,allow calculation of an estimate of the complete three-dimensional state of stress in the rock mass.5. S
12、ignificance and Use5.1 Either virgin stresses or the stresses as influenced by anexcavation may be determined. This test method is writtenassuming testing will be done from an underground opening;however, the same principles may be applied to testing in arock outcrop at the surface.5.2 This test met
13、hod is generally performed at depths within50 ft (15 m) of the working face because of drilling difficultiesat greater depths. Some deeper testing has been done, but1This test method is under the jurisdiction ofASTM Committee D18 on Soil andRock and is the direct responsibility of Subcommittee D18.1
14、2 on Rock Mechanics.Current edition approved July 1, 2008. Published July 2008. Originally approvedin 1986. Last previous edition approved in 2005 as D 4623 05.2Considerable information presented in this test method was taken from Bureauof Mines Information Circular No. 8618, and Hooker, V.E., and B
15、ickel, D.L.,“Overcoring Equipment and Techniques Used in Rock Stress Determination,”Denver Mining Research Center, Denver, CO, 1974.3For referenced ASTM standards, visit the ASTM website, www.astm.org, orcontact ASTM Customer Service at serviceastm.org. For Annual Book of ASTMStandards volume inform
16、ation, refer to the standards Document Summary page onthe ASTM website.1*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.should be considered developmental. It is also u
17、seful forobtaining stress characteristics of existing concrete and rockstructures for safety and modification investigations.5.3 This test method is difficult in rock with fracturespacings of less than 5 in. (130 mm). A large number of testsmay be required in order to obtain data.5.4 The rock tested
18、 is assumed to be homogeneous andlinearly elastic. The moduli of deformation and Poissons ratioof the rock are required for data reduction. The preferredmethod for determining modulus of deformation values in-volves biaxially testing the recovered overcores, as describedin Section 8. If this is not
19、possible, values may be determinedfrom uniaxial testing of smaller cores in accordance with TestMethod D 7012. However, this generally decreases the accu-racy of the stress determination in all but the most homoge-neous rock. Results may be used from other in situ tests, suchas Test Method D 4394 an
20、d Test Method D 4395.5.5 The physical conditions present in three separate drillholes are assumed to prevail at one point in space to allow thethree-dimensional stress field to be estimated. This assumptionis difficult to verify, as rock material properties and the localstress field can vary signifi
21、cantly over short distances. Confi-dence in this assumption increases with careful selection of thetest site.5.6 Local geologic features with mechanical propertiesdifferent from those of the surrounding rock can influencesignificantly the local stress field. In general, these features, ifknown to be
22、 present, should be avoided when selecting a testsite location. It is often important, however, to measure thestress level on each side of a large fault. All boreholes at asingle test station should be in the same formation.5.7 Since most overcoring is performed to measure undis-turbed stress levels
23、, the boreholes should be drilled from aportion of the test opening at least three excavation diametersfrom any free surface. The smallest opening that will accom-modate the drilling equipment is recommended; openings from8 to 12 ft (2.4 to 3.6 m) in diameter have been foundsatisfactory.5.8 Aminimum
24、 of three nonparallel boreholes is required todetermine the complete stress tensor. The optimum angle eachhole makes with the other two (trihedral arrangement) is 90.However, angles of 45 provide satisfactory results for deter-mining all three principal stresses. Boreholes inclined upwardare general
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