ASTM D5311-1992(2004)e1 Standard Test Method for Load Controlled Cyclic Triaxial Strength of Soil《土壤的负荷控制三向疲劳强度的标准试验方法》.pdf
《ASTM D5311-1992(2004)e1 Standard Test Method for Load Controlled Cyclic Triaxial Strength of Soil《土壤的负荷控制三向疲劳强度的标准试验方法》.pdf》由会员分享,可在线阅读,更多相关《ASTM D5311-1992(2004)e1 Standard Test Method for Load Controlled Cyclic Triaxial Strength of Soil《土壤的负荷控制三向疲劳强度的标准试验方法》.pdf(10页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D 5311 92 (Reapproved 2004)1Standard Test Method forLoad Controlled Cyclic Triaxial Strength of Soil1This standard is issued under the fixed designation D 5311; the number immediately following the designation indicates the year oforiginal adoption or, in the case of revision, the year
2、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.1NOTEFig. 4 was editorially corrected in April 2009.1. Scope1.1 This test method covers the determination of the cyclicstrength
3、 (sometimes called the liquefaction potential) of satu-rated soils in either undisturbed or reconstituted states by theload-controlled cyclic triaxial technique.1.2 The cyclic strength of a soil is evaluated relative to anumber of factors, including: the development of axial strain,magnitude of appl
4、ied cyclic stress, number of cycles of stressapplication, development of excess pore-water pressure, andstate of effective stress. A comprehensive review of factorsaffecting cyclic triaxial test results is contained in the literature(1).21.3 Cyclic triaxial strength tests are conducted under und-rai
5、ned conditions to simulate essentially undrained field con-ditions during earthquake or other cyclic loading.1.4 Cyclic triaxial strength tests are destructive. Failure maybe defined on the basis of the number of stress cycles requiredto reach a limiting strain or 100 % pore pressure ratio. SeeSecti
6、on 3 for Terminology.1.5 This test method is generally applicable for testingcohesionless free draining soils of relatively high permeability.When testing well-graded materials, silts, or clays, it should berecognized that pore-water pressures monitored at the speci-men ends to not in general repres
7、ent pore-water pressure valuesthroughout the specimen. However, this test method may befollowed when testing most soil types if care is taken to ensurethat problem soils receive special consideration when testedand when test results are evaluated.1.6 There are certain limitations inherent in using c
8、yclictriaxial tests to simulate the stress and strain conditions of a soilelement in the field during an earthquake.1.6.1 Nonuniform stress conditions within the test specimenare imposed by the specimen end platens. This can cause aredistribution of void ratio within the specimen during the test.1.6
9、.2 A 90 change in the direction of the major principalstress occurs during the two halves of the loading cycle onisotropically consolidated specimens.1.6.3 The maximum cyclic shear stress that can be appliedto the specimen is controlled by the stress conditions at the endof consolidation and the por
10、e-water pressures generated duringtesting. For an isotropically consolidated contractive (volumedecreasing) specimen tested in cyclic compression, the maxi-mum cyclic shear stress that can be applied to the specimen isequal to one-half of the initial total axial pressure. Sincecohesionless soils are
11、 not capable of taking tension, cyclicshear stresses greater than this value tend to lift the top platenfrom the soil specimen. Also, as the pore-water pressureincreases during tests performed on isotropically consolidatedspecimens, the effective confining pressure is reduced, contrib-uting to the t
12、endency of the specimen to neck during theextension portion of the load cycle, invalidating test resultsbeyond that point.1.6.4 While it is advised that the best possible undisturbedspecimens be obtained for cyclic strength testing, it is some-times necessary to reconstitute soil specimens. It has b
13、eenshown that different methods of reconstituting specimens to thesame density may result in significantly different cyclicstrengths. Also, undisturbed specimens will almost always bestronger than reconstituted specimens.1.6.5 The interaction between the specimen, membrane, andconfining fluid has an
14、 influence on cyclic behavior. Membranecompliance effects cannot be readily accounted for in the testprocedure or in interpretation of test results. Changes inpore-water pressure can cause changes in membrane penetra-tion in specimens of cohesionless soils. These changes cansignificantly influence t
15、he test results.1.6.6 The mean total confining pressure is asymmetricduring the compression and extension stress application whenthe chamber pressure is constant. This is totally different fromthe symmetric stress in the simple shear case of the levelground liquefaction.1.7 The values stated in both
16、 inch-pound and SI units are tobe regarded separately as the standard. The values given inparentheses are for information only.1This test method is under the jurisdiction ofASTM Committee D18 on Soil andRock and is the direct responsibility of Subcommittee D18.09 on Cyclic andDynamic Properties of S
17、oils.Current edition approved Feb. 1, 2004. Published February 2004. Originallyapproved in 1992 as D 5311 92.2The boldface numbers in parentheses refer to a list of references at the end ofthe text.1Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959, U
18、nited States.1.8 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.2.
19、 Referenced Documents2.1 ASTM Standards:3D 422 Test Method for Particle-Size Analysis of SoilsD 653 Terminology Relating to Soil, Rock, and ContainedFluidsD 854 Test Method for Specific Gravity of SoilsD 1587 Practice for Thin-Walled Tube Sampling of SoilsD 2216 Test Method for Laboratory Determinat
20、ion of Water(Moisture) Content of Soil and RockD 2850 Test Method for Unconsolidated, Undrained Com-pressive Strength of Cohesive Soils in Triaxial Compres-sionD 4220 Practice for Preserving and Transporting SoilSamplesD 4253 Test Methods for Maximum Index Density and UnitWeight of Soils Using a Vib
21、ratory TableD 4254 Test Method for Minimum Index Density and UnitWeight of Soils and Calculation of Relative DensityD 4318 Test Method for Liquid Limit, Plastic Limit, andPlasticity Index of SoilsD 4767 Test Method for Consolidated-Undrained TriaxialCompression Test on Cohesive Soils3. Terminology3.
22、1 Definitions:3.1.1 Definitions for terms used in this test method (includ-ing liquefaction) are in accordance with Terminology D 653.Additional descriptions of terms are defined in 3.2 and in 10.2and Fig. 1.3.2 Definitions of Terms Specific to This Standard:3.2.1 full or 100 % pore pressure ratio a
23、 condition inwhich Du equals s83c.3.2.2 peak pore pressure ratiothe maximum pore pressureratio measured during a particular loading sequence.3.2.3 peak (single amplitude) strainthe maximum axialstrain (from the origin or initial step) in either compression orextension produced during a particular lo
24、ading sequence.3.2.4 peak to peak (double amplitude) strain the differ-ence between the maximum axial strain in compression andextension during a given cycle under cyclic loading conditions.3.2.5 pore pressure ratiothe ratio, expressed as a percent-age, of the change of excess pore-water pressure, D
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