ASTM D6031 D6031M-1996(2010)e1 1875 Standard Test Method for Logging In Situ Moisture Content and Density of Soil and Rock by the Nuclear Method in Horizontal Slanted and Vertical .pdf
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1、Designation: D6031/D6031M 96 (Reapproved 2010)1Standard Test Method forLogging In Situ Moisture Content and Density of Soil andRock by the Nuclear Method in Horizontal, Slanted, andVertical Access Tubes1This standard is issued under the fixed designation D6031/D6031M; the number immediately followin
2、g the designation indicates theyear of original adoption or, in the case of revision, the year of last revision. A number in parentheses indicates the year of lastreapproval. A superscript epsilon () indicates an editorial change since the last revision or reapproval.1NOTEThe units statement in 1.3
3、and the designation were revised editorially in August 2010.1. Scope1.1 This test method covers collection and comparison oflogs of thermalized-neutron counts and back-scattered gammacounts along horizontal or vertical air-filled access tubes.1.2 The in situ water content in mass per unit volume and
4、the density in mass per unit volume of soil and rock at positionsor in intervals along the length of an access tube are calculatedby comparing the thermal neutron count rate and gamma countrates respectively to previously established calibration data.1.3 The values stated in either inch-pound units
5、or SI unitspresented in brackets are to be regarded separately asstandard. The values stated in each system may not be exactequivalents; therefore, each system shall be used independentlyof the other. Combining values from the two systems mayresult in non-conformance with the standard.1.3.1 The grav
6、itational system of inch-pound units is usedwhen dealing with inch-pound units. In this system, the pound(lbf) represents a unit of force (weight), while the unit for massis slugs. The rationalized slug unit is not given, unless dynamic(F = ma) calculations are involved.1.4 This standard does not pu
7、rport 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. For specifichazards, see Section 6.2. Refer
8、enced Documents2.1 ASTM Standards:2D1452 Practice for Soil Exploration and Sampling byAugerBoringsD1586 Test Method for Penetration Test (SPT) and Split-Barrel Sampling of SoilsD1587 Practice for Thin-Walled Tube Sampling of Soils forGeotechnical PurposesD2113 Practice for Rock Core Drilling and Sam
9、pling ofRock for Site InvestigationD2216 Test Methods for Laboratory Determination of Wa-ter (Moisture) Content of Soil and Rock by MassD2922 Test Methods for Density of Soil and Soil-Aggregatein Place by Nuclear Methods (Shallow Depth)3D2937 Test Method for Density of Soil in Place by theDrive-Cyli
10、nder MethodD3017 Test Method for Water Content of Soil and Rock inPlace by Nuclear Methods (Shallow Depth)D3550 Practice for Thick Wall, Ring-Lined, Split Barrel,Drive Sampling of SoilsD4428/D4428M Test Methods for Crosshole Seismic Test-ingD4564 Test Method for Density and Unit Weight of Soil inPla
11、ce by the Sleeve MethodD5195 Test Method for Density of Soil and Rock In-Placeat Depths Below Surface by Nuclear MethodsD5220 Test Method for Water Mass per Unit Volume of Soiland Rock In-Place by the Neutron Depth Probe Method3. Significance and Use3.1 This test method is useful as a repeatable, no
12、ndestruc-tive technique to monitor in-place density and moisture of soiland rock along lengthy sections of horizontal, slanted, andvertical access holes or tubes. With proper calibration inaccordance with Annex A1, this test method can be used toquantify changes in density and moisture content of so
13、il androck.3.2 This test method is used in vadose zone monitoring, forperformance assessment of engineered barriers at waste facili-ties, and for research related to monitoring the movement ofliquids (water solutions and hydrocarbons) through soil and1This test method is under the jurisdiction ofAST
14、M Committee D18 on Soil andRock and is the direct responsibility of Subcommittee D18.21 on Ground Water andVadose Zone Investigations.Current edition approved Aug. 1, 2010. Published September 2010. Originallyapproved in 1996. Last previous edition approved in 2004 as D603196(2004).DOI: 10.1520/D603
15、1_D6031M-96R10E01.2For referenced ASTM standards, visit the ASTM website, www.astm.org, orcontact ASTM Customer Service at serviceastm.org. For Annual Book of ASTMStandards volume information, refer to the standards Document Summary page onthe ASTM website.3Withdrawn. The last approved version of th
16、is historical standard is referencedon www.astm.org.1Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959, United States.rock. The nondestructive nature of the test allows repetitivemeasurements at a site and statistical analysis of results.3.3 The funda
17、mental assumptions inherent in this testmethod are that the dry bulk density of the test material isconstant and that the response to fast neutrons and gammarayenergy associated with soil and liquid chemistry is constant.4. Interferences4.1 The sample heterogeneity and chemical composition ofthe mat
18、erial under test will affect the measurement of bothmoisture and density. The apparatus should be calibrated to thematerial under test at a similar density of dry soil or rock andin the similar type and orientation of access tube, or adjust-ments must be made in accordance with Annex A2.4.2 Hydrogen
19、, in forms other than water, as defined by TestMethod D2216, will cause measurements in excess of the truemoisture content. Some elements such as boron, chlorine, andminute quantities of cadmium, if present in the material undertest, will cause measurements lower than the true moisturecontent. Some
20、elements with atomic numbers greater than 20such as iron or other heavy metals may cause measurementshigher than the true density value.4.3 The measurement of moisture and density using this testmethod exhibits spatial bias in that it is more sensitive to thematerial closest to the access tube. The
21、density and moisturemeasurements are necessarily an average of the total sampleinvolved.4.4 The sample volume for a moisture measurement isapproximately 3.8 ft30.11 m3 at a moisture content of 12.5lbf/ft3200 kg/m3. The actual sample volume for moisture isindeterminate and varies with the apparatus a
22、nd the moisturecontent of the material. In general the greater the moisturecontent of the material, the smaller the measurement volume.4.5 Adensity measurement has a sample volume of approxi-mately 0.8 ft30.028 m3. The actual sample volume fordensity is indeterminate and varies with the apparatus an
23、d thedensity of the material. In general, the greater the density of thematerial, the smaller the measurement volume.4.6 Air gaps between the probe and the access tube or voidsaround the access tube will cause the indicated moisturecontent and density to be less than the calibrated values.4.7 Conden
24、sed moisture inside the access tube may causethe indicated moisture content to be greater than the truemoisture content of material outside the access tube.5. Apparatus5.1 While exact details of construction of the apparatus mayvary, the system shall consist of:5.1.1 Fast Neutron SourceA sealed mixt
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