ASTM C1402-2004 Standard Guide for High-Resolution Gamma-Ray Spectrometry of Soil Samples《土壤样品的高分辨率γ射线光谱测定法的标准指南》.pdf
《ASTM C1402-2004 Standard Guide for High-Resolution Gamma-Ray Spectrometry of Soil Samples《土壤样品的高分辨率γ射线光谱测定法的标准指南》.pdf》由会员分享,可在线阅读,更多相关《ASTM C1402-2004 Standard Guide for High-Resolution Gamma-Ray Spectrometry of Soil Samples《土壤样品的高分辨率γ射线光谱测定法的标准指南》.pdf(9页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: C 1402 04Standard Guide forHigh-Resolution Gamma-Ray Spectrometry of Soil Samples1This standard is issued under the fixed designation C 1402; the number immediately following the designation indicates the year oforiginal adoption or, in the case of revision, the year of last revision. A
2、 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 guide covers the identification and quantitativedetermination of gamma-ray emitting radionuclides in soilsamples by means of gam
3、ma-ray spectrometry. It is applicableto nuclides emitting gamma rays with an approximate energyrange of 20 to 2000 keV. For typical gamma-ray spectrometrysystems and sample types, activity levels of about 5 Bq (135pCi) are measured easily for most nuclides, and activity levelsas low as 0.1 Bq (2.7 p
4、Ci) can be measured for many nuclides.It is not applicable to radionuclides that emit no gamma rayssuch as the pure beta-emitting radionuclides hydrogen-3,carbon-14, strontium-90, and becquerel quantities of mosttransuranics. This guide does not address the in situ measure-ment techniques, where soi
5、l is analyzed in place withoutsampling. Guidance for in situ techniques can be found in Ref(1) and (2).2This guide also does not discuss methods fordetermining lower limits of detection. Such discussions can befound in Refs (3), (4), (5), and (6).1.2 This guide can be used for either quantitative or
6、 relativedeterminations. For quantitative assay, the results are expressedin terms of absolute activities or activity concentrations of theradionuclides found to be present. This guide may also be usedfor qualitative identification of the gamma-ray emitting radio-nuclides in soil without attempting
7、to quantify their activities.It can also be used to only determine their level of activitiesrelative to each other but not in an absolute sense. Generalinformation on radioactivity and its measurement may befound in Refs (7), (8), (9), (10), and (11) and Standard TestMethods E 181. Information on sp
8、ecific applications ofgamma-ray spectrometry is also available in Refs (12) or (13).Practice D 3649 may be a valuable source of information.1.3 This standard may involve hazardous material, opera-tions, and equipment. This standard does not purport toaddress all of the safety concerns, if any, assoc
9、iated with itsuse. It is the responsibility of the user of this standard toestablish appropriate safety and health practices and deter-mine the applicability of regulatory limitations prior to use.2. Referenced Documents2.1 ASTM Standards:3C 998 Practice for Sampling Surface Soil for RadionuclidesC
10、999 Practice for Soil Sample Preparation for the Deter-mination of RadionuclidesC 1009 Guide for Establishing a Quality Assurance Pro-gram for Analytical Chemistry Laboratories Within theNuclear IndustryD 3649 Practice for High-Resolution Gamma-Ray Spec-trometry of WaterE 181 Test Methods for Detect
11、or Calibration and Analysisof RadionuclidesIEEE/ASTM-SI-10 Standard for Use of the InternationalSystem of Units (SI) the Modern Metric System2.2 ANSI Standards:4N13.30 Performance Criteria for RadiobioassayN42.14 Calibration and Use of Germanium Spectrometersfor the Measurement of Gamma-Ray Emission
12、 Rates ofRadionuclidesN42.23 Measurement Quality Assurance for RadioassayLaboratoriesANSI/IEEE-645 Test Procedures for High Purity Germa-nium Detectors for Ionizing Radiation3. Summary of Guide3.1 High-resolution germanium detectors and multichannelanalyzers are used to ensure the identification of
13、the gamma-ray emitting radionuclides that are present and to provide thebest possible accuracy for quantitative activity determinations.3.2 For qualitative radionuclide identifications, the systemmust be energy calibrated. For quantitative determinations, thesystem must also be shape and efficiency
14、calibrated. Thestandard sample/detector geometries must be established aspart of the efficiency calibration procedure.3.3 The soil samples typically need to be pretreated (forexample, dried), weighed, and placed in a standard container.For quantitative measurements, the dimensions of the container1T
15、his guide is under the jurisdiction of ASTM Committee C26 on Nuclear FuelCycle and is the direct responsibility of Subcommittee C26.05 on Methods of Test.Current edition approved June 1, 2004. Published July 2004. Originally approvedin 1998. Last previous edition approved in 1998 as C 1402 98.2The b
16、oldface numbers in parentheses refer to the list of references at the endof this standard.3For 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 Sum
17、mary page onthe ASTM website.4Available from American National Standards Institute, West 42nd St. 13thFloor, New York, NY 10036.1Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959, United States.holding the sample and its placement in front of the dete
18、ctormust match one of the efficiency-calibrated geometries. Ifmultiple geometries can be selected, the geometry chosenshould reflect the detection limit and count rate limitations ofthe system. Qualitative measurements may be performed innon-calibrated geometries.3.4 The identification of the radion
19、uclides present is basedon matching the energies of the observed gamma rays in thespectrum to computer-based libraries of literature referencessee Refs (14), (15), (16), (17),or(18). The quantitativedeterminations are based on comparisons of observed countrates to previously obtained counting effici
20、ency versus energycalibration data, and published branching ratios for the radio-nuclides identified.4. Significance and Use4.1 Gamma-ray spectrometry of soil samples is used toidentify and quantify certain gamma-ray emitting radionu-clides. Use of a germanium semiconductor detector is neces-sary fo
21、r high-resolution gamma-ray measurements.4.2 Much of the data acquisition and analysis can beautomated with the use of commercially available systems thatinclude both hardware and software. For a general descriptionof the typical hardware in more detail than discussed in Section6, see Ref (19).4.3 B
22、oth qualitative and quantitative analyses may be per-formed using the same measurement data.4.4 The procedures described in this guide may be used fora wide variety of activity levels, from natural backgroundlevels and fallout-type problems, to determining the effective-ness of cleanup efforts after
23、 a spill or an industrial accident, totracing contamination at older production sites, where wasteswere purposely disposed of in soil. In some cases, thecombination of radionuclide identities and concentration ratioscan be used to determine the source of the radioactivematerials.4.5 Collecting sampl
24、es and bringing them to a data acqui-sition system for analysis may be used as the primary methodto detect deposition of radionuclides in soil. For obtaining arepresentative set of samples that cover a particular area, seePractice C 998. Soil can also be measured by taking the dataacquisition system
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