ASTM D5311-1992(2004) 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测试方法》.pdf
《ASTM D5311-1992(2004) 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测试方法》.pdf》由会员分享,可在线阅读,更多相关《ASTM D5311-1992(2004) 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测试方法》.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)Standard 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 o
2、f 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 the cyclicstrength (sometimes called the liquefaction potential) of sa
3、tu-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 applied cyclic stress, number of cycles of stressapplica
4、tion, 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-rained conditions to simulate essentially undrained fie
5、ld 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. SeeSection 3 for Terminology.1.5 This test method is general
6、ly 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 represent pore-water pressure valuesthroughout the specime
7、n. 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 cyclictriaxial tests to simulate the stress and strai
8、n 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.1.6.2 A 90 change in the direction of the major princip
9、alstress 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 pore-water pressures generated duringtesting. For an is
10、otropically 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 not capable of taking tension, cyclicshear stresses
11、 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 tendency of the specimen to neck during theextension
12、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 beenshown that different methods of reconstituting sp
13、ecimens 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 influence on cyclic behavior. Membranecompliance ef
14、fects 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 the test results.1.6.6 The mean total confining press
15、ure 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 inch-pound and SI units are tobe regarded separatel
16、y as the standard. The values given inparentheses are for information only.1This test method is under the jurisdiction of ASTM Committee D18 on Soil andRock and is the direct responsibility of Subcommittee D18.09 on DynamicProperties of Soils.Current edition approved Oct. 15, 1992. Published January
17、 1993.2The 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, United States.1.8 This standard does not purport to address all of thesafety concerns, if any, associate
18、d 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 Documents2.1 ASTM Standards:3D 422 Test Method for Particle-Size Analysis of SoilsD 653 Ter
19、minology 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 Determination of Water(Moisture) Content of Soil and RockD 2850 Test Method for Unconsolidated, Undrained Com-pre
20、ssive 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 Vibratory TableD 4254 Test Method for Minimum Index Density and UnitWeight of Soils and Calculation of Rel
21、ative DensityD 4318 Test Method for Liquid Limit, Plastic Limit, andPlasticity Index of SoilsD 4767 Test Method for Consolidated-Undrained TriaxialCompression Test on Cohesive Soils3. Terminology3.1 Definitions:3.1.1 Definitions for terms used in this test method (includ-ing liquefaction) are in acc
22、ordance 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 condition inwhich Du equals s83c.3.2.2 peak pore pressure ratiothe maximum pore pressureratio measured
23、 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 loading sequence.3.2.4 peak to peak (double amplitude) strain the differ-ence between the maximum axial s
24、train 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 u,totheeffective minor principal stress, s83c, at the end of primaryconsolidation.4. Summary of Test M
- 1.请仔细阅读文档,确保文档完整性,对于不预览、不比对内容而直接下载带来的问题本站不予受理。
- 2.下载的文档,不会出现我们的网址水印。
- 3、该文档所得收入(下载+内容+预览)归上传者、原创作者;如果您是本文档原作者,请点此认领!既往收益都归您。
下载文档到电脑,查找使用更方便
10000 积分 0人已下载
下载 | 加入VIP,交流精品资源 |
- 配套讲稿:
如PPT文件的首页显示word图标,表示该PPT已包含配套word讲稿。双击word图标可打开word文档。
- 特殊限制:
部分文档作品中含有的国旗、国徽等图片,仅作为作品整体效果示例展示,禁止商用。设计者仅对作品中独创性部分享有著作权。
- 关 键 词:
- ASTMD531119922004STANDARDTESTMETHODFORLOADCONTROLLEDCYCLICTRIAXIALSTRENGTHOFSOIL 土壤 负荷 控制 疲劳强度 测试 方法

链接地址:http://www.mydoc123.com/p-519444.html