ASTM C1255-1993(2005) Standard Test Method for Analysis of Uranium and Thorium in Soils by Energy Dispersive X-Ray Fluorescence Spectroscopy《用能量色散X射线荧光光谱法分析土壤中铀和钍的标准试验方法》.pdf
《ASTM C1255-1993(2005) Standard Test Method for Analysis of Uranium and Thorium in Soils by Energy Dispersive X-Ray Fluorescence Spectroscopy《用能量色散X射线荧光光谱法分析土壤中铀和钍的标准试验方法》.pdf》由会员分享,可在线阅读,更多相关《ASTM C1255-1993(2005) Standard Test Method for Analysis of Uranium and Thorium in Soils by Energy Dispersive X-Ray Fluorescence Spectroscopy《用能量色散X射线荧光光谱法分析土壤中铀和钍的标准试验方法》.pdf(7页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: C 1255 93 (Reapproved 2005)Standard Test Method forAnalysis of Uranium and Thorium in Soils by EnergyDispersive X-Ray Fluorescence Spectroscopy1This standard is issued under the fixed designation C 1255; the number immediately following the designation indicates the year oforiginal adop
2、tion 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 the energy dispersive X-rayfluorescence (EDXRF)
3、 spectrochemical analysis of trace levelsof uranium and thorium in soils.Any sample matrix that differsfrom the general ground soil composition used for calibration(that is, fertilizer or a sample of mostly rock) would have to becalibrated separately to determine the effect of the differentmatrix co
4、mposition.1.2 The analysis is performed after an initial drying andgrinding of the sample, and the results are reported on a drybasis. The sample preparation technique used incorporates intothe sample any rocks and organic material present in the soil.This test method of sample preparation differs f
5、rom othertechniques that involve tumbling and sieving the sample.1.3 Linear calibration is performed over a concentrationrange from 20 to 1000 g per gram for uranium and thorium.1.4 The values stated in SI units are to be regarded as thestandard. The inch-pound units in parentheses are for informa-t
6、ion only.1.5 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.2. Ref
7、erenced Documents2.1 ASTM Standards:2C 982 Guide for Selecting Components for Energy Disper-sive X-Ray Fluorescence (XRF) SystemsC 998 Practice for Sampling Surface Soil for RadionuclidesD 420 Guide for Investigating and Sampling Soil and RockD 1452 Practice for Soil Investigation and Sampling byAug
8、er 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 Drilling for Site Inves-tigationD 3550 Practice for Ring-Lined Barrel Sampling of SoilsD 4697 Guide for Maintaining Test Methods in
9、 the UsersLaboratoryE 135 Terminology Relating to Analytical Chemistry forMetals, Ores, and Related MaterialsE 305 Practice for Establishing and Controlling Spectro-chemical Analytical CurvesE 456 Terminology Relating to Quality and StatisticsE 876 Practice for Use of Statistics in the Evaluation of
10、Spectrometric DataE 882 Guide for Accountability and Quality Control in theChemical Analysis Laboratory2.2 Other Document:NBS Radiation Safety Handbook Number 111 for X-RayDiffraction and Fluorescence Analysis Equipment33. Terminology3.1 Definitions:3.1.1 For definitions of terms relating to analyti
11、cal atomicspectroscopy, refer to Terminology E 135.3.1.2 For definitions of terms relating to statistics refer toTerminology E 456.3.2 Definitions of Terms Specific to This Standard:3.2.1 escape peaka peak generated by an X-ray havingenergy greater than 1.84 keV (the energy of the k-alphaabsorption
12、edge for silicon) that enters the detector and causesthe silicon detector crystal to fluoresce. If the silicon X-rayescapes the detector, carrying with it the energy of the siliconk-alpha X-ray, 2.79 E-16 Joules J (1.74 keV), the energymeasured for the detected X-ray will be less than the actualX-ra
13、y energy by exactly 2.79 E-16 J (1.74 keV). Therefore, ascounts accumulate for any major X-ray peak, an escape peakcan be expected to appear at an energy of 2.79 E-16 J (1.741This test method is under the jurisdiction of ASTM Committee C26 on NuclearFuel Cycle and is the direct responsibility of Sub
14、committee C26.05 on Methods ofTests.Current edition approved June 1, 2005. Published December 2005. Originallyapproved in 1993. Last previous edition approved in 1999 as C 125593(1999).2For referenced ASTM standards, visit the ASTM website, www.astm.org, orcontact ASTM Customer Service at serviceast
15、m.org. For Annual Book of ASTMStandards volume information, refer to the standards Document Summary page onthe ASTM website.3Available from the U.S. Department of Commerce, National Institute ofStandards and Technology, Gaithersburg, MD 20899.1Copyright ASTM International, 100 Barr Harbor Drive, PO
16、Box C700, West Conshohocken, PA 19428-2959, United States.keV) below the major peak. Escape peaks can be calculatedand removed from the spectrum by most insrumentationsoftware.3.2.2 flux monitor (FM) valuethe detected X-ray intensitywithin a specified spectral range from a metallic standardgiving a
17、high number of counts. The same excitation condi-tions as the sample analysis are used (except for the change inthe current to achieve maximum efficiency of the data acqui-sition system). With all conditions remaining constant, the FMvalue is proportional to the X-ray energy flux being emittedfrom t
18、he X-ray tube or radioisotope source.3.2.3 flux monitor ratio (FMR)the ratio of the initial FMvalue (FMi) prior to calibration and sample analysis to currentFM value (FMc) at the time of sample analysis. This ratio isused to correct the measured element intensity for changes inthe X-ray energy flux.
19、4. Summary of Test Method4.1 A representative sample of soil is obtained by firsttaking a sizeable amount (100 g) and drying it, then runningit through a crusher and placing it on a shaker/tumbler tohomogenize it. A portion is then ground in a ball mill andpressed into a sample pellet. An energy dis
20、persive X-rayfluorescence spectrometer is used to expose the sample to amonochromatic X-ray source capable of exciting the uraniumand thorium L-alpha series lines. The X-rays emitted by thesample are detected via a solid state detector Si(Li) andcounted in discrete energy channels on a multi-channel
21、 ana-lyzer (MCA) to form an energy spectrum. The spectrum is thenprocessed to obtain the peak intensities for uranium andthorium for calibration and quantitation.5. Significance and Use5.1 This test method was developed and the instrumentcalibrated using ground soils from the site of a nuclearmateri
22、als plant. This test method can be used to measure theextent of contamination from uranium and thorium in groundsoils. Since the detection limit of this technique (nominally 20g per gram) approaches typical background levels for thesecontaminants, the method can be used as a quick characteriza-tion
23、of an on-site area to indicated points of contamination.Then after cleanup, EDXRF may be used to verify theelimination of contamination or other analysis methods (suchas colorimetry, fluoremetry, phosphorescence, etc.) can be usedif it is necessary to test for cleanup down to a requiredbackground le
24、vel. This test method can also be used for thesegregation of soil lots by established contamination levelsduring on-site construction and excavation.6. Interferences6.1 The following elements typically are found in an X-rayspectrum from soil in the spectral region of uranium andthorium: zinc (Zn), t
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