ASTM D7928-2017 red 8750 Standard Test Method for Particle-Size Distribution (Gradation) of Fine-Grained Soils Using the Sedimentation (Hydrometer) Analysis《采用沉降(液体比重计)分析法测定细粒土壤粒径分.pdf
《ASTM D7928-2017 red 8750 Standard Test Method for Particle-Size Distribution (Gradation) of Fine-Grained Soils Using the Sedimentation (Hydrometer) Analysis《采用沉降(液体比重计)分析法测定细粒土壤粒径分.pdf》由会员分享,可在线阅读,更多相关《ASTM D7928-2017 red 8750 Standard Test Method for Particle-Size Distribution (Gradation) of Fine-Grained Soils Using the Sedimentation (Hydrometer) Analysis《采用沉降(液体比重计)分析法测定细粒土壤粒径分.pdf(28页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D7928 161D7928 17Standard Test Method forParticle-Size Distribution (Gradation) of Fine-Grained SoilsUsing the Sedimentation (Hydrometer) Analysis1This standard is issued under the fixed designation D7928; the number immediately following the designation indicates the year oforiginal ad
2、option or, 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 NOTEEditorially corrected A1.4.3.1, Fig. X1.5, and Fig. X1.6 in January 2017.1.
3、Scope1.1 This test method covers the quantitative determination of the distribution of particle sizes of the fine-grained portion of soils.The sedimentation or hydrometer method is used to determine the particle-size distribution (gradation) of the material that is finerthan the No. 200 (75-m) sieve
4、 and larger than about 0.2-m. The test is performed on material passing the No. 10 (2.0-mm) orfiner sieve and the results are presented as the mass percent finer versus the log of the particle diameter.1.2 This method can be used to evaluate the fine-grained fraction of a soil with a wide range of p
5、article sizes by combining thesedimentation results with a sieve analysis resulting in the complete gradation curve. The method can also be used when there areno coarse-grained particles or when the gradation of the coarse-grained material is not required or not needed.NOTE 1The significant digits r
6、ecorded in this test method preclude obtaining the grain size distribution of materials that do not contain a significantamount of fines. For example, clean sands will not yield detectable amounts of silt and clay sized particles, and therefore should not be tested with thismethod. The minimum amoun
7、t of fines in the sedimentation specimen is 15 g.1.3 When combining the results of the sedimentation and sieve tests, the procedure for obtaining the material for thesedimentation analysis and calculations for combining the results will be provided by the more general test method, such as TestMethod
8、s D6913 (Note 2).NOTE 2Subcommittee D18.03 is currently developing a new test method “Test Method for Particle-Size Analysis of Soils Combining the Sieve andSedimentation Techniques.”1.4 The terms “soil” and “material” are used interchangeably throughout the standard.1.5 The sedimentation analysis i
9、s based on the concept that larger particles will fall through a fluid faster than smaller particles.StokesLaw gives a governing equation used to determine the terminal velocity of a spherical particle falling through a stationaryliquid. The terminal velocity is proportional to the square of the par
10、ticle diameter. Therefore, particles are sorted by size in bothtime and position when settling in a container of liquid.1.5.1 Stokes Law has several assumptions which are: the particles are spherical and smooth; there is no interference betweenthe particles; there is no difference between the curren
11、t in the middle of the container and the sides; flow is laminar; and theparticles have the same density. These assumptions are applied to soil particles of various shapes and sizes.1.6 A hydrometer is used to measure the fluid density and determine the quantity of particles in suspension at a specif
12、ic timeand position. The density of the soil-water suspension depends upon the concentration and specific gravity of the soil particles andthe amount of dispersant added. Each hydrometer measurement at an elapsed time is used to calculate the percentage of particlesfiner than the diameter given by S
13、tokes Law. The series of readings provide the distribution of material mass as a function ofparticle size.1.7 This test method does not cover procurement of the sample or processing of the sample prior to obtaining the reducedsample in any detail. It is assumed that the sample is obtained using appr
14、opriate methods and is representative of site materialsor conditions. It is also assumed that the sample has been processed such that the reduced sample accurately reflects theparticle-size distribution (gradation) of this finer fraction of the material.1.8 Material ProcessingMaterial is tested in t
15、he moist or as-received state unless the material is received in an air-dried state.The moist preparation method shall be used to obtain a sedimentation test specimen from the reduced sample.Air-dried preparation1 This test method is under the jurisdiction of ASTM Committee D18 on Soil and Rock and
16、is the direct responsibility of Subcommittee D18.03 on Texture, Plasticityand Density Characteristics of Soils.Current edition approved May 1, 2016May 1, 2017. Published May 2016May 2017. Originally approved in 2016. Last previous edition approved in 2016 as D7928 161.DOI: 10.1520/D7928-16E0110.1520
17、/D7928-17This document is not an ASTM standard and is intended only to provide the user of an ASTM standard an indication of what changes have been made to the previous version. Becauseit may not be technically possible to adequately depict all changes accurately, ASTM recommends that users consult
18、prior editions as appropriate. In all cases only the current versionof the standard as published by ASTM is to be considered the official document.Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959. United States1is only allowed when the material is re
19、ceived in the air-dried state. The method to be used may be specified by the requestingauthority; however, the moist preparation method shall be used for referee testing.1.9 This test method is not applicable for the following soils:1.9.1 Soils containing fibrous peat.1.9.2 Soils containing less tha
20、n approximately 5 % of fine-grained material (Note 1).1.9.3 Soils containing extraneous matter, such as organic solvents, oil, asphalt, wood fragments, or similar items (Note 3).NOTE 3If extraneous matter, such as wood, can be easily removed by hand, it is permissible to do so. However, there may be
21、 cases where theextraneous matter is being evaluated as part of the material and it should not be removed from the material.1.9.4 Materials that contain cementitious components, such as cement, fly ash, lime, or other stabilization admixtures.1.10 This test method may not produce consistent test res
22、ults within and between laboratories for the following soils. To testthese soils, this test method must be adapted and these adaptations documented.1.10.1 Soils that flocculate during sedimentation. Such materials may need to be treated to reduce salinity or alter the pH of thesuspension.1.10.2 Fria
23、ble soils in which processing changes the gradation of the soil. Typical examples of these soils are some residualsoils, most weathered shales, and some weakly cemented soils.1.10.3 Soils that will not readily disperse, such as glauconitic clays or some dried plastic clays.1.11 Samples that are not
24、soils, but are made up of particles may be tested using this method. The applicable sections aboveshould be used in applying this standard.1.12 UnitsThe values stated in SI units are to be regarded as standard. Except the sieve designations, they are identified usingthe “alternative” system in accor
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