ASTM D6031-1996(2004) Standard Test Method for Logging In Situ Moisture Content and Density of Soil and Rock by the Nuclear Method in Horizontal Slanted and Vertical Access Tubes《在.pdf
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1、Designation: D 6031 96 (Reapproved 2004)Standard 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 D 6031; the number immediately following the designa
2、tion indicates the year oforiginal adoption or, in the case of revision, the year of 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 collecti
3、on 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 andthe density in mass per unit volume of soil and rock at positionsor in intervals along the length of an
4、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 SI units are regarded as thestandard. The inch-pound units given in parentheses may beapproximate and are provided for informati
5、on only.1.4 This standard does not purport 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 sp
6、ecifichazards, see Section 6.2. Referenced Documents2.1 ASTM Standards:2D 1452 Practice for Soil Investigation and Sampling byAuger BoringsD 1586 Test Method for Penetration Test and Split/BarrelSampling of SoilsD 1587 Practice for Thin-Walled Tube Sampling of SoilsD2113 Practice for Diamond Core Dr
7、illing for Site Inves-tigationD 2216 Test Method for Laboratory Determination of Water(Moisture) Content of Soil and RockD 2922 Test Methods for Density of Soil and Soil-Aggregate in Place by Nuclear Methods (Shallow Depth)D 2937 Test Method for Density of Soil in Place by theDrive-Cylinder MethodD
8、3017 Test Method for Water Content of Soil and Rock inPlace by Nuclear Methods (Shallow Depth)D 4428/D 4428M Test Methods of Crosshole Seismic Test-ingD 4564 Test Method for Density of Soil in Place by theSleeve MethodD 5195 Test Method for Density of Soil and Rock In-Placeat Depths Below the Surfac
9、e by Nuclear MethodsD 5220 Test Method for Water Content of Soil and RockIn-Place by the Neutron Depth Probe Method3. Significance and Use3.1 This test method is useful as a repeatable, nondestruc-tive technique to monitor in-place density and moisture of soiland rock along lengthy sections of horiz
10、ontal, 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 soil androck.3.2 This test method is used in vadose zone monitoring, forperformance assessment of engineered barri
11、ers at waste facili-ties, and for research related to monitoring the movement ofliquids (water solutions and hydrocarbons) through soil androck. The nondestructive nature of the test allows repetitivemeasurements at a site and statistical analysis of results.3.3 The fundamental assumptions inherent
12、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 material under test will affect
13、 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, in forms other than water,
14、 as defined by TestMethod D 2216, will cause measurements in excess of the truemoisture content. Some elements such as boron, chlorine, and1This test method is under the jurisdiction ofASTM Committee D18 on Soil andRock and is the direct responsibility of Subcommittee D18.21 on Ground Water andVados
15、e Zone Investigations.Current edition approved Nov. 1, 2004. Published December 2004. Originallyapproved in 1996. Last previous edition approved in 1996 as D 603196.2For referenced ASTM standards, visit the ASTM website, www.astm.org, orcontact ASTM Customer Service at serviceastm.org. For Annual Bo
16、ok of ASTMStandards volume information, 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.minute quantities of cadmium, if present in the material undertest, will cause me
17、asurements lower than the true moisturecontent. Some 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 sens
18、itive to thematerial closest to the access tube. The density and moisturemeasurements are necessarily an average of the total sampleinvolved.4.4 The sample volume for a moisture measurement isapproximately 0.11 m3(3.8 ft3) at a moisture content of 200kg/m3(12.5 lbf/ft3). The actual sample volume for
19、 moisture isindeterminate and varies with the apparatus and 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 0.028 m3(0.8 ft3). The actual sample volume f
20、ordensity is indeterminate and varies with the apparatus and 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 a
21、nd density to be less than the calibrated values.4.7 Condensed 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 sys
22、tem shall consist of:5.1.1 Fast Neutron SourceA sealed mixture of a radioac-tive material such as americium or radium and a target materialsuch as beryllium, or other fast neutron sources such ascalifornium that do not require a target.5.1.2 Slow Neutron DetectorAny type of slow neutrondetector, suc
23、h as boron trifluoride or helium-3 proportionalcounters.5.1.3 High-Energy Gamma-Radiation Source A sealedsource of radioactive material, such as cesium-137, cobalt-60,or radium-226.5.1.4 Gamma DetectorAny type of gamma detector, suchas a Geiger-Mueller tube.5.1.5 Suitable Readout Device:5.1.6 Cylind
24、rical ProbeThe apparatus shall be equippedwith a cylindrical probe, containing the neutron and gammasources and the detectors, connected by a cable or cables ofsufficient design and length, that are capable of raising andlowering the probe in vertical applications and pulling it inhorizontal applica
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