ASTM D7263-2009 952 Standard Test Methods for Laboratory Determination of Density (Unit Weight) of Soil Specimens《实验室测定土壤样品的密度(单位重量)的标准试验方法》.pdf
《ASTM D7263-2009 952 Standard Test Methods for Laboratory Determination of Density (Unit Weight) of Soil Specimens《实验室测定土壤样品的密度(单位重量)的标准试验方法》.pdf》由会员分享,可在线阅读,更多相关《ASTM D7263-2009 952 Standard Test Methods for Laboratory Determination of Density (Unit Weight) of Soil Specimens《实验室测定土壤样品的密度(单位重量)的标准试验方法》.pdf(7页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D 7263 09Standard Test Methods forLaboratory Determination of Density (Unit Weight) of SoilSpecimens1This standard is issued under the fixed designation D 7263; 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.1. Scope1.1 These test methods describe two ways of determiningthe total/moist and dry densities (unit weights) of intact,distu
3、rbed, remolded, and reconstituted (compacted) soil speci-mens. Density (unit weight) as used in this standard means thesame as “bulk density” of soil as defined by the Soil ScienceSociety of America. Intact specimens may be obtained fromthin-walled sampling tubes, block samples, or clods. Speci-mens
4、 that are remolded by dynamic or static compactionprocedures may also be measured by these methods. Thesemethods apply to soils that will retain their shape during themeasurement process and may also apply to other materialssuch as soil-cement, soil-lime, soil-bentonite or solidifiedsoil-bentonite-c
5、ement slurries. It is common for the density(unit weight) of specimens after removal from sampling tubesand compaction molds to be less than the value based on tubeor mold volumes, or of in-situ conditions. This is due to thespecimen swelling after removal of lateral pressures.1.1.1 Method A covers
6、the procedure for measuring thevolume of wax coated specimens by determining the quantityof water displaced.1.1.1.1 This method only applies to specimens in which thewax will not penetrate the outer surface of the specimen.1.1.2 Method B covers the procedure by means of the directmeasurement of the
7、dimensions and mass of a specimen,usually one of cylindrical shape. Intact and reconstituted/remolded specimens may be tested by this method in conjunc-tion with strength, permeability (air/water) and compressibilitydeterminations.1.2 The values stated in SI units are to be regarded as thestandard.
8、The values stated in inch-pound units are approxi-mate.1.3 All observed and calculated values shall conform to theguidelines for significant digits and rounding established inPractice D 6026.1.3.1 The method used to specify how data are collected,calculated, or recorded in this standard is not direc
9、tly related tothe accuracy with which the data can be applied in design orother uses, or both. How one applies the results obtained usingthis standard is beyond its scope.1.4 This standard does not purport to address all of thesafety concerns, if any, associated with its use. It is theresponsibility
10、 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:2D 653 Terminology Relating to Soil, Rock, and ContainedFluidsD 698 Test Methods for Laboratory Compac
11、tion Character-istics of Soil Using Standard Effort (12 400 ft-lbf/ft3(600kN-m/m3)D 854 Test Methods for Specific Gravity of Soil Solids byWater PycnometerD 1557 Test Methods for Laboratory Compaction Charac-teristics of Soil Using Modified Effort (56,000 ft-lbf/ft3(2,700 kN-m/m3)D 1587 Practice for
12、 Thin-Walled Tube Sampling of Soilsfor Geotechnical PurposesD 2166 Test Method for Unconfined Compressive Strengthof Cohesive SoilD 2216 Test Methods for Laboratory Determination of Wa-ter (Moisture) Content of Soil and Rock by MassD 2487 Practice for Classification of Soils for EngineeringPurposes
13、(Unified Soil Classification System)D 2488 Practice for Description and Identification of Soils(Visual-Manual Procedure)D 3550 Practice for Thick Wall, Ring-Lined, Split Barrel,Drive Sampling of SoilsD 3740 Practice for Minimum Requirements for AgenciesEngaged in Testing and/or Inspection of Soil an
14、d Rock asUsed in Engineering Design and ConstructionD 4220 Practices for Preserving and Transporting SoilSamplesD 4318 Test Methods for Liquid Limit, Plastic Limit, and1These test methods are under the jurisdiction ofASTM Committee D18 on Soiland Rock and are the direct responsibility of Subcommitte
15、e D18.03 on Texture,Plasticity and Density Characteristics of Soils.Current edition approved March 15, 2009. Published April 2009.2For referenced ASTM standards, visit the ASTM website, www.astm.org, orcontact ASTM Customer Service at serviceastm.org. For Annual Book of ASTMStandards volume informat
16、ion, refer to the standards Document Summary page onthe ASTM website.1Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959, United States.Plasticity Index of SoilsD 4753 Guide for Evaluating, Selecting, and SpecifyingBalances and Standard Masses for Use
17、in Soil, Rock, andConstruction Materials TestingD 6026 Practice for Using Significant Digits in Geotechni-cal DataE 2251 Specification for Liquid-in-Glass ASTM Thermom-eters with Low-Hazard Precision Liquids2.2 Other Reference:Soil Science Society of America Glossary of Soil ScienceTerms33. Terminol
18、ogy3.1 Refer to Terminology D 653 for standard definitions ofterms.4. Significance and Use4.1 Dry density, as defined as “density of soil or rock” inTerminology D 653 and “bulk density” by soil scientists, canbe used to convert the water fraction of soil from a mass basisto a volume basis and vise-v
19、ersa. When particle density, that is,specific gravity (Test Methods D 854) is also known, drydensity can be used to calculate porosity and void ratio (seeAppendix X1). Dry density measurements are also useful fordetermining degree of soil compaction. Since moisture contentis variable, moist soil den
20、sity provides little useful informationexcept to estimate the weight of soil per unit volume, forexample, pounds per cubic yard, at the time of sampling. Sincesoil volume shrinks with drying of swelling soils, bulk densitywill vary with moisture content. Hence, the water content ofthe soil should be
21、 determined at the time of sampling.4.2 Densities (unit weights) of remolded/reconstitutedspecimens are commonly used to evaluate the degree ofcompaction of earthen fills, embankments, etc. Dry densityvalues are usually used in conjunction with compaction curvevalues (Test Methods D 698 and D 1557).
22、4.3 Density (unit weight) is one of the key components indetermining the mass composition/phase relations of soil, seeAppendix X1.NOTE 1The quality of the result produced by this standard isdependent on the competence of the personnel performing it and thesuitability of the equipment and facilities
23、used. Agencies that meet thecriteria of Practice D 3740 are generally considered capable of competentand objective testing/sampling/inspection/etc. Users of this standard arecautioned that compliance with Practice D 3740 does not in itself assurereliable results. Reliable results depend on several f
24、actors; PracticeD 3740 provides a means of evaluating some of these factors.5. Apparatus5.1 For Method A the following apparatus are required:5.1.1 BalanceAll balances must meet the requirements ofSpecification D 4753 and this section. A Class GP1 balance of0.01 g readability is required for specime
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