ASTM G167-2005(2010) Standard Test Method for Calibration of a Pyranometer Using a Pyrheliometer《用直接日射强度表校正日射强度计标准试验方法》.pdf

《ASTM G167-2005(2010) Standard Test Method for Calibration of a Pyranometer Using a Pyrheliometer《用直接日射强度表校正日射强度计标准试验方法》.pdf》由会员分享，可在线阅读，更多相关《ASTM G167-2005(2010) Standard Test Method for Calibration of a Pyranometer Using a Pyrheliometer《用直接日射强度表校正日射强度计标准试验方法》.pdf（21页珍藏版）》请在麦多课文档分享上搜索。

1、Designation: G167 05 (Reapproved 2010)Standard Test Method forCalibration of a Pyranometer Using a Pyrheliometer1This standard is issued under the fixed designation G167; the number immediately following the designation indicates the year oforiginal adoption or, in the case of revision, the year of

2、last revision. A number in parentheses indicates the year of last reapproval. Asuperscript epsilon () indicates an editorial change since the last revision or reapproval.INTRODUCTIONAccurate and precise measurements of total global (hemispherical) solar irradiance are required inthe assessment of ir

3、radiance and radiant exposure in the testing of exposed materials, determinationof the energy available to solar collection devices, and assessment of global and hemispherical solarradiation for meteorological purposes.This test method requires calibrations traceable to the World Radiometric Referen

4、ce (WRR), whichrepresents the SI units of irradiance. The WRR is determined by a group of selected absolutepyrheliometers maintained by the World Meteorological Organization (WMO) in Davos, Switzerland.Realization of the WRR in the United States, and other countries, is accomplished by theintercompa

5、rison of absolute pyrheliometers with the World Radiometric Group (WRG) through aseries of intercomparisons that include the International Pyrheliometric Conferences held every fiveyears in Davos. The intercomparison of absolute pyrheliometers is covered by procedures adopted byWMO and is not covere

6、d by this test method.It should be emphasized that “calibration of a pyranometer” essentially means the transfer of theWRR scale from a pyrheliometer to a pyranometer under specific experimental procedures.1. Scope1.1 This test method covers an integration of previous TestMethod E913 dealing with th

7、e calibration of pyranometerswith axis vertical and previous Test Method E941 on calibra-tion of pyranometers with axis tilted. This amalgamation of thetwo methods essentially harmonizes the methodology with ISO9846.1.2 This test method is applicable to all pyranometersregardless of the radiation re

8、ceptor employed, and is applicableto pyranometers in horizontal as well as tilted positions.1.3 This test method is mandatory for the calibration of allsecondary standard pyranometers as defined by the WorldMeteorological Organization (WMO) and ISO 9060, and forany pyranometer used as a reference py

9、ranometer in thetransfer of calibration using Test Method E842.1.4 Two types of calibrations are covered: Type I calibra-tions employ a self-calibrating, absolute pyrheliometer, andType II calibrations employ a secondary reference pyrheliom-eter as the reference standard (secondary reference pyrheli

10、om-eters are defined by WMO and ISO 9060).1.5 Calibrations of reference pyranometers may be per-formed by a method that makes use of either an altazimuth orequatorial tracking mount in which the axis of the radiometersradiation receptor is aligned with the sun during the shadingdisk test.1.6 The det

11、ermination of the dependence of the calibrationfactor (calibration function) on variable parameters is calledcharacterization. The characterization of pyranometers is notspecifically covered by this method.1.7 This test method is applicable only to calibration pro-cedures using the sun as the light

12、source.1.8 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. Refer

13、enced Documents2.1 ASTM Standards:2E772 Terminology Relating to Solar Energy ConversionE824 Test Method for Transfer of Calibration From Refer-ence to Field Radiometers1This test method is under the jurisdiction of ASTM Committee G03 onWeathering and Durability and is the direct responsibility of Su

14、bcommittee G03.09on Radiometry.Current edition approved Dec. 1, 2010. Published December 2010. Originallyapproved in 2000. Last previous edition approved in 2005 as G167 05. DOI:10.1520/G0167-05R10.2For referenced ASTM standards, visit the ASTM website, www.astm.org, orcontact ASTM Customer Service

15、at serviceastm.org. For Annual Book 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.2.2 WMO Document:World Meteorological Organizati

16、on (WMO), “Measure-ment of Radiation” Guide to Meteorological Instrumentsand Methods of Observation, fifth ed., WMO-No. 8,Geneva32.3 ISO Standards:ISO 9060:1990 Solar EnergySpecification and Classifica-tion of Instruments for Measuring Hemispherical Solarand Direct Solar Radiation3ISO 9846:1993 Sola

17、r EnergyCalibration of a Pyranom-eter Using a Pyrheliometer33. Terminology3.1 Definitions:3.1.1 See Terminology E772.3.2 Definitions of Terms Specific to This Standard:3.2.1 altazimuth mount, na tracking mount capable ofrotation about orthogonal altitude and azimuth axes; trackingmay be manual or by

18、 a follow-the-sun servomechanism.3.2.2 calibration of a radiometer, vdetermination of theresponsivity (or the calibration factor, the reciprocal of theresponsivity) of a radiometer under well-defined measurementconditions.3.2.3 direct solar radiation, nthat component of solarradiation within a speci

19、fied solid angle (usually 5.0 or 5.7)subtended at the observer by the suns solar disk, including aportion of the circumsolar radiation.3.2.4 diffuse solar radiation, nthat component of solarradiation scattered by the air molecules, aerosol particles, cloudand other particles in the hemisphere define

20、d by the sky dome.3.2.5 equatorial mount, nsee Terminology E772.3.2.6 field of view angle of a pyrheliometer, nfull angle ofthe cone which is defined by the center of the receiver surface(see ISO 9060, 5.1) and the border of the limiting aperture, ifthe latter are circular and concentric to the rece

21、iver surface; ifnot, effective angles may be calculated (1, 2).43.2.7 global solar radiation, ncombined direct and dif-fuse solar radiation falling on a horizontal surface; solarradiation incident on a horizontal surface from the hemispheri-cal sky dome, or from 2p Steradian (Sr).3.2.8 hemispherical

22、 radiation, ncombined direct and dif-fuse solar radiation incident from a virtual hemisphere, or from2p Sr, on any inclined surface.3.2.8.1 DiscussionThe case of a horizontal surface isdenoted global solar radiation (3.2.7).3.2.9 pyranometer, nsee Terminology E772.3.2.10 pyranometer, field, na pyran

23、ometer meeting WMOSecond Class or better (that is, First Class) appropriate to fielduse and typically exposed continuously.3.2.11 pyranometer, reference, na pyranometer (see alsoISO 9060), used as a reference to calibrate other pyranometers,which is well-maintained and carefully selected to possessr

24、elatively high stability and has been calibrated using apyrheliometer.3.2.12 pyrheliometer, nsee Terminology E772 and ISO9060.3.2.13 pyrheliometer, absolute (self-calibrating), na solarradiometer with a limited field of view configuration. The fieldof view should be approximately 5.0 and have a slop

25、e angle offrom 0.75 to 0.8, with a blackened conical cavity receiver forabsorption of the incident radiation. The measured electricalpower to a heater wound around the cavity receiver constitutesthe method of self-calibration from first principles and trace-ability to absolute SI units. The self-cal

26、ibration principlerelates to the sensing of the temperature rise of the receivingcavity by an associated thermopile when first the sun isincident upon the receiver and subsequently when the samethermopile signal is induced by applying precisely measuredpower to the heater with the pyrheliometer shut

27、tered from thesun.3.2.14 shading-disk device, na device which allowsmovement of a disk in such a way that the receiver of thepyranometer to which it is affixed, or associated, is shadedfrom the sun. The cone formed between the origin of thereceiver and the disk subtends an angle that closely matches

28、 thefield of view of the pyrheliometer against which it is compared.Alternatively, and increasingly preferred, a sphere rather than adisk eliminates the need to continuously ensure the properalignment of the disk normal to the sun. See Appendix X1.3.2.15 slope angle, nthe angle defined by the differ

29、ence inradii of the view limiting aperture (radius = R) and the receiverradius (= r) in a pyrheliometer. The slope angle, s,isthearctangent of R minus r divided by the distance between thelimiting aperture and the receiver surface, denoted by L:s =Tan-1(R r)/L. See Ref (1).3.2.16 thermal offset, na

30、non-zero signal generated by aradiometer when blocked from all sources of radiation. Be-lieved to be the result of infrared (thermal) radiation exchangesbetween elements of the radiometer and the environment.3.3 Acronyms:3.3.1 ACRAbsolute Cavity Radiometer3.3.2 ANSIAmerican National Standards Instit

31、ute3.3.3 ARMAtmospheric RadiationMeasurement Program3.3.4 DOEDepartment of Energy3.3.5 GUM(ISO) Guide to Uncertainty in Measurements3.3.6 IPCInternational Pyrheliometer comparison3.3.7 ISOInternational Standards Organization3.3.8 NCSLNational Council of Standards Laboratories3.3.9 NISTNational Insti

32、tute of Standards and Technol-ogy3.3.10 NRELNational Renewable Energy Laboratory3.3.11 PMODPhysical Meteorological Observatory Da-vos3.3.12 SACSingapore Accreditation Council3.3.13 SINGLASSingapore Laboratory Accreditation Ser-vice3.3.14 UKASUnited Kingdom Accrediation Service3.3.15 WRCWorld Radiati

33、on Center3.3.16 WRRWorld Radiometric Reference3.3.17 WMOWorld Meteorological Organization3Available from American National Standards Institute (ANSI), 25 W. 43rd St.,4th Floor, New York, NY 10036, http:/www.ansi.org.4The boldface numbers in parentheses refer to the list of references at the end ofth

34、is standard.G167 05 (2010)24. Significance and Use4.1 The pyranometer is a radiometer designed to measurethe sum of directly solar radiation and sky radiation in suchproportions as solar altitude, atmospheric conditions and cloudcover may produce. When tilted to the equator, by an angle b,pyranomete

35、rs measure only hemispherical radiation falling inthe plane of the radiation receptor.4.2 This test method represents the only practical means forcalibration of a reference pyranometer. While the sun-trackers,the shading disk, the number of instantaneous readings, and theelectronic display equipment

36、 used will vary from laboratory tolaboratory, the method provides for the minimum acceptableconditions, procedures and techniques required.4.3 While, in theory, the choice of tilt angle (b) is unlimited,in practice, satisfactory precision is achieved over a range oftilt angles close to the zenith an

37、gles used in the field.4.4 The at-tilt calibration as performed in the tilted positionrelates to a specific tilted position and in this position requiresno tilt correction. However, a tilt correction may be required torelate the calibration to other orientations, including axisvertical.NOTE 1WMO Fis

38、t Class pyranometers, or better, generally exhibit tilterrors of less than 1 % to tilts of 50 from the horizontal.4.5 Traceability of calibrations to the World RadiometricReference (WRR) is achieved through comparison to a refer-ence absolute pyrheliometer that is itself traceable to the WRRthrough

39、one of the following:4.5.1 One of the International Pyrheliometric Comparisons(IPC) held in Davos, Switzerland since 1980 (IPC IV). SeeRefs (3-7).4.5.2 Any like intercomparison held in the United States,Canada or Mexico and sanctioned by the World MeteorologicalOrganization as a Regional Intercompar

40、ison of Absolute Cav-ity Pyrheliometers.4.5.3 Intercomparison with any absolute cavity pyrheliom-eter that has participated in either and IPC or a WMO-sanctioned intercomparison within the past five years andwhich was found to be within 60.4 % of the mean of allabsolute pyrheliometers participating

41、therein.4.6 The calibration method employed in this test methodassumes that the accuracy of the values obtained are indepen-dent of time of year, with the constraints imposed and by thetest instruments temperature compensation circuit (neglectingcosine errors).5. Selection of Shade Method5.1 Alterna

42、ting Shade Method:5.1.1 The alternating shade method is required for a primarycalibration of the reference pyranometer used in the Continu-ous, Component-Summation Shade Method described in 5.2.5.1.2 The pyranometer under test is compared with apyrheliometer measuring direct solar irradiance (or, op

43、tionally,a continuously shaded control pyranometer; see AppendixX3-Appendix X5). The voltage values from the pyranometerthat correspond to direct solar irradiance are derived from thedifference between the response of the pyranometer to hemi-spherical (unshaded) solar irradiance and the diffuse (sha

44、ded)solar irradiance. These response values (for example, voltages)are induced periodically by means of a movable sun shadedisk. For the calculation of the responsivity, the differencebetween the unshaded and shaded irradiance signals is dividedby the direct solar irradiance (measured by the pyrheli

45、ometer)component that is normal to the receiver plane of the pyra-nometer.5.1.3 For meteorological purposes, the solid angle fromwhich the scattered radiative fluxes that represent diffuseradiation are measured shall be the total sky hemisphere,excluding a small solid angle around the suns disk.5.1.

46、4 In addition to the basic method, modifications of thismethod that are considered to improve the accuracy of thecalibration factors, but which require more operational expe-rience, are presented in Appendix X3-Appendix X5.5.2 Continuous Sun-and-Shade Method (Component Sum-mation):5.2.1 The pyranome

47、ter is compared with two referenceradiometers, one of which is a pyrheliometer and the other awell-calibrated reference pyranometer equipped with a track-ing shade disk or sphere to measure diffuse solar radiation. Thereference pyranometer shall be either calibrated using thealternating sun-and shad

48、e method described in 5.1, or shall becompared against such a pyranometer in accordance with TestMethod E824.5.2.2 Global solar irradiance (or hemispherical solar irradi-ance for inclined pyranometers) is determined by the sum ofthe direct solar irradiance measured with a pyrheliometermultiplied by

49、the cosine of the incidence angle of the beam tothe local horizontal (or inclined plane parallel to the radiometersensor), plus the diffuse solar irradiance measured with ashaded reference pyranometer mounted in the same configu-ration (tilted or horizontal) as the unit under test.5.2.3 The smallest uncertainty realized in the calibration ofpyranometers will occur when the pyrheliometer is a self-calibrating absolute cavity pyrheliometer and when the refer-ence pyranometer has itself been calibrated over a range of airmass (zenith ang