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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 finer than the No. 200 (75-μm)...
1.1 This test method covers the quantitative determination of the distribution of particle sizes of the fine-grained portion of soils. The sedimentation by hydrometer method is used to determine the particle-size distribution (gradation) of the material that is finer than the No. 200 (75-µm)...
1.1 This test method covers the quantitative determination of the distribution of particle sizes of the fine-grained portion of soils. The sedimentation by hydrometer method is used to determine the particle-size distribution (gradation) of the material that is finer than the No. 200 (75-µm)...
1.1 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 finer than the No. 200 (75-µm)...
1.1 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 finer than the No. 200 (75-µm)...
1.1 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 finer than the No. 200 (75-µm)...
1.1 This test method covers the quantitative determination of the distribution of particle sizes in soils. The distribution of particle sizes larger than 75 μm (retained on the No. 200 sieve) is determined by sieving, while the distribution of particle sizes smaller than 75 μm is determined by a...
1.1 Two test methods are provided to give a qualitative indication of the natural dispersive characteristics of clayey soils: Method A and Method B. 1.1.1 Method A-Procedure for Natural Soil Crumbs described in 10.1. 1.1.2 Method B-Procedure for Remolded Soil Crumbs described in 10.2. 1.2 The crumb...
Two test methods are provided to give a qualitative indication of the natural dispersive characteristics of clayey soils: Method A and Method B. Method A-Procedure for Natural Soil Crumbs described in 10.1. Method B-Procedure for Remolded Soil Crumbs described in 10.2. The crumb test, while a good,...
1.1 Two test methods are provided to give a qualitative indication of the natural dispersive characteristics of clayey soils: Method A and Method B. 1.1.1 Method A-Procedure for Natural Soil Crumbs described in 10.1. 1.1.2 Method B-Procedure for Remolded Soil Crumbs described in 10.2. 1.2 The crumb...
1.1 These test methods provide a qualitative indication of the natural dispersive characteristics of clayey soils. 1.2 These test methods are not applicable for soils with less than 12 % fraction finer than 0.005 mm and with a plasticity index less than or equal to 8. 1.3 The crumb test method has...
1.1 These test methods provide a qualitative indication of the natural dispersive characteristics of clayey soils. 1.2 These test methods are not applicable for soils with less than 12 % fraction finer than 0.005 mm and with a plasticity index less than or equal to 8. 1.3 The crumb test method has...
1.1 Two test methods are provided to give a qualitative indication of the natural dispersive characteristics of clayey soils:. Method A and Method B. 1.1.1 Method A-Procedure for Natural Soil Crumbs described in 10.2. 1.1.2 Method B-Procedure for Remolded Soil Crumbs described in 10.3. 1.2 The...
1.1 Two test methods are provided to give a qualitative indication of the natural dispersive characteristics of clayey soils: Method A and Method B. 1.1.1 Method A-Procedure for Natural Soil Crumbs described in 10.2. 1.1.2 Method B-Procedure for Remolded Soil Crumbs described in 10.3. 1.2 The crumb...
1.1 Two test methods are provided to give a qualitative indication of the natural dispersive characteristics of clayey soils: Method A and Method B. 1.1.1 Method A-Procedure for Natural Soil Crumbs described in 10.2. 1.1.2 Method B-Procedure for Remolded Soil Crumbs described in 10.3. 1.2 The crumb...
5.1 The crumb test method provides a simple, quick method for field or laboratory identification of a dispersive clay soil. The internal erosion failures of a number of homogeneous earth dams, erosion along channel or canal banks, and rainfall erosion of earthen structures have been attributed to...
1.1 These test methods cover the determination of the specific gravity of water and brine free of separable oil, as follows: Sections Test Method A-Pycnometer 7 to 11, 21 Test Method B-Balance 12 to 16, 21 Test Method C-Erlenmeyer Flask 17 to 21 Test Method D-Hydrometer 22 to 27 1.2 Test...
This part of ISO 17892 specifies a method of determining the particle size distribution of soils. This part of ISO 17892 is applicable to the laboratory determination of the particle size distribution of a soil test specimen by sieving, or sedimentation, or a combination of both within the scope of...
ISO 17892-4.2016 specifies a method of determining the particle size distribution of soils. ISO 17892-4.2016 is applicable to the laboratory determination of the particle size distribution of a soil test specimen by sieving, or sedimentation, or a combination of both within the scope of...
This part of ISO 17892 specifies a method of determining the particle size distribution of soils. This part of ISO 17892 is applicable to the laboratory determination of the particle size distribution of a soil test specimen by sieving, or sedimentation, or a combination of both within the scope of...
