ASTM D3649-2006(2014) Standard Practice for High-Resolution Gamma-Ray Spectrometry of Water《水的高分辩率伽马射线光谱测定法的标准实施规程》.pdf
《ASTM D3649-2006(2014) Standard Practice for High-Resolution Gamma-Ray Spectrometry of Water《水的高分辩率伽马射线光谱测定法的标准实施规程》.pdf》由会员分享,可在线阅读,更多相关《ASTM D3649-2006(2014) Standard Practice for High-Resolution Gamma-Ray Spectrometry of Water《水的高分辩率伽马射线光谱测定法的标准实施规程》.pdf(8页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D3649 06 (Reapproved 2014) An American National StandardStandard Practice forHigh-Resolution Gamma-Ray Spectrometry of Water1This standard is issued under the fixed designation D3649; the number immediately following the designation indicates the year oforiginal adoption or, in the case
2、 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. Scope1.1 This practice covers the measurement of gamma-rayemitting radionuclides in water by means of
3、 gamma-rayspectrometry. It is applicable to nuclides emitting gamma-rayswith energies greater than 45 keV. For typical counting systemsand sample types, activity levels of about 40 Bq are easilymeasured and sensitivities as low as 0.4 Bq are found for manynuclides. Count rates in excess of 2000 coun
4、ts per secondshould be avoided because of electronic limitations. Highcount rate samples can be accommodated by dilution, byincreasing the sample to detector distance, or by using digitalsignal processors.1.2 This practice can be used for either quantitative orrelative determinations. In relative co
5、unting work, the resultsmay be expressed by comparison with an initial concentrationof a given nuclide which is taken as 100 %. For quantitativemeasurements, the results may be expressed in terms of knownnuclidic standards for the radionuclides known to be present.This practice can also be used just
6、 for the identification ofgamma-ray emitting radionuclides in a sample without quan-tifying them. General information on radioactivity and themeasurement of radiation has been published (1,2).2Informa-tion on specific application of gamma spectrometry is alsoavailable in the literature (3-5). See al
7、so the referenced ASTMStandards in 2.1 and the related material section at the end ofthis standard.1.3 This standard does not purport to address the safetyconcerns, if any, associated with its use. It is the responsibilityof the user of this standard to establish appropriate safety andhealth practic
8、es and determine the applicability of regulatorylimitation prior to use.2. Referenced Documents2.1 ASTM Standards:3D1066 Practice for Sampling SteamD1129 Terminology Relating to WaterD2777 Practice for Determination of Precision and Bias ofApplicable Test Methods of Committee D19 on WaterD3370 Pract
9、ices for Sampling Water from Closed ConduitsD3648 Practices for the Measurement of RadioactivityD4448 Guide for Sampling Ground-Water Monitoring WellsE181 Test Methods for Detector Calibration and Analysis ofRadionuclides3. Terminology3.1 DefinitionsFor definitions of terms used in thispractice, ref
10、er to Terminology D1129. For terms not defined inthis practice or in Terminology D1129, reference may be madeto other published glossaries.4. Summary of Practice4.1 Gamma ray spectra are measured with modular equip-ment consisting of a detector, high-voltage power supply,preamplifier, amplifier and
11、analog-to-digital converter (or digi-tal signal processor), multichannel analyzer, as well as acomputer with display.4.2 High-purity germanium (HPGe) detectors, p-type orn-type, are used for the analysis of complex gamma-ray spectrabecause of their excellent energy resolution. These germaniumsystems
12、, however, are characterized by high cost and requirecooling. Liquid nitrogen or electromechanical cooling, or both,can be used.4.3 In a germanium semiconductor detector, gamma-rayphotons produce electron-hole pairs. The charged pair is thencollected by an applied electric field. A very stable low n
13、oisepreamplifier is needed to amplify the pulses of electric charge1This practice is under the jurisdiction of ASTM Committee D19 on Water andis the direct responsibility of Subcommittee D19.04 on Methods of RadiochemicalAnalysis.Current edition approved June 1, 2014. Published July 2014. Originally
14、 approvedin 1978. Last previous edition approved in 2006 as D3649 06. DOI: 10.1520/D3649-06R14.2The boldface numbers in parentheses refer to a list of references at the end ofthis standard.3For referenced ASTM standards, visit the ASTM website, www.astm.org, orcontact ASTM Customer Service at servic
15、eastm.org. For Annual Book of ASTMStandards volume information, refer to the standards Document Summary page onthe ASTM website.Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959. United States1resulting from gamma photon interactions. The output from
16、thepreamplifier is directly proportional to the energy deposited bythe incident gamma-ray. These current pulses are fed into anamplifier of sufficient gain to produce voltage output pulses inthe amplitude range from 0 to 10 V.4.4 A multichannel pulse-height analyzer is used to deter-mine the amplitu
17、de of each pulse originating in the detector,and accumulates in a memory the number of pulses in eachamplitude band (or channel) in a given counting time. Com-puterized systems with stored programs and interface hardwarecan accomplish the same functions as hardwired multichannelanalyzers. The primar
18、y advantages of the computerized systeminclude the capability of programming the multi-channel ana-lyzer functions and the ability to immediately perform datareduction calculations using the spectral data stored in thecomputer memory or mass storage device. Fora0to2-MeVspectrum, 4000 or more channel
19、s are typically needed in orderto fully utilize a germanium detectors excellent energy reso-lution.4.5 The distribution of the amplitudes (pulse heights) of thepulses can be separated into two principal components. One ofthese components has a nearly Gaussian distribution and is theresult of total a
20、bsorption of the gamma-ray energy in thedetector. This peak is normally referred to as the full-energypeak or photopeak. The other component is a continuous onelower in energy than that of the photopeak. This continuouscurve is referred to as the Compton continuum and is due tointeractions wherein t
21、he gamma photons deposit only part oftheir energy in the detector. These two portions of the curve areshown in Fig. 1. Other peaks, such as escape peaks, backscat-tered gamma rays or X rays from shields, are often superim-posed on the Compton continuum. Escape peaks will bepresent when gamma-rays wi
22、th energies greater than 1.02 MeVare emitted from the sample. The positron formed in pairproduction is usually annihilated in the detector and one orboth of the 511keV annihilation quanta may escape from thedetector without interaction. This condition will cause single ordouble escape peaks at energ
23、ies of 0.511 or 1.022 MeV lessthan the photopeak energy. In the plot of pulse height versuscount rate, the size and location of the photopeak on the pulseheight axis is proportional to the number and energy of theincident photons, and is the basis for the quantitative andqualitative application of t
24、he spectrometer. The Comptoncontinuum serves no useful purpose in photopeak analysis andmust be subtracted when peaks are analyzed.4.6 If the analysis is being directed and monitored by anonline computer program, the analysis period may be termi-nated by prerequisites incorporated in the program. If
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