ASTM G183-2005(2010) Standard Practice for Field Use of Pyranometers Pyrheliometers and UV Radiometers《日辐射强度计 直接日照强度计和紫外线辐射计现场使用的标准操作规程》.pdf
《ASTM G183-2005(2010) Standard Practice for Field Use of Pyranometers Pyrheliometers and UV Radiometers《日辐射强度计 直接日照强度计和紫外线辐射计现场使用的标准操作规程》.pdf》由会员分享,可在线阅读,更多相关《ASTM G183-2005(2010) Standard Practice for Field Use of Pyranometers Pyrheliometers and UV Radiometers《日辐射强度计 直接日照强度计和紫外线辐射计现场使用的标准操作规程》.pdf(9页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: G183 05 (Reapproved 2010)Standard Practice forField Use of Pyranometers, Pyrheliometers and UVRadiometers1This standard is issued under the fixed designation G183; the number immediately following the designation indicates the year oforiginal adoption or, in the case of revision, the ye
2、ar 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 describes deployment conditions, mainte-nance requirements, verification procedures and calibratio
3、nfrequencies for use of pyranometers, pyrheliometers and UVradiometers in outdoor testing environments. This practice alsodiscusses the conditions that dictate the level of accuracyrequired for instruments of different classes.1.2 While both pyranometers and UV radiometers may beemployed indoors to
4、measure light radiation sources, themeasurement of ultraviolet and light radiation in acceleratedweathering enclosures using manufactured light sources gen-erally requires specialized radiometric instruments. Use ofradiometric instrumentation to measure laboratory lightsources is covered in ISO 9370
5、.NOTE 1An ASTM standard that is similar to ISO 9370 is underdevelopment and deals with the instrumental determination of irradianceand radiant exposure in weathering tests.1.3 The characterization of radiometers is outside the scopeof the activities required of users of radiometers, as contem-plated
6、 by this standard.2. Referenced Documents2.1 ASTM Standards:2E772 Terminology Relating to Solar Energy ConversionG7 Practice for Atmospheric Environmental Exposure Test-ing of Nonmetallic MaterialsG24 Practice for Conducting Exposures to Daylight FilteredThrough GlassG90 Practice for Performing Acce
7、lerated Outdoor Weather-ing of Nonmetallic Materials Using Concentrated NaturalSunlightG113 Terminology Relating to Natural andArtificial Weath-ering Tests of Nonmetallic Materials2.2 ISO Standards:ISO 877 PlasticsMethods of Exposure to Direct Weath-ering, Indirect Weathering Using Glass-Filtered Da
8、ylightand Indirect Weathering by Daylight Using Fresnel Mir-rors3ISO 9060 Solar EnergySpecification and Classification ofInstruments for Measuring Hemispherical Solar and Di-rect Solar Radiation3ISO 9370 PlasticsInstrumental Determination of RadiantExposure in Weathering TestsGeneral Guidance3ISO TR
9、 9901 Solar EnergyField PyranometersRecommended Practice for Use32.3 Other Reference:World Meteorological Organization (WMO), 1983 “Mea-surement of Radiation,” Guide to Meteorological Instru-ments and Methods of Observation, fifth ed., WMO-No. 8,Geneva3. Terminology3.1 DefinitionsThe definitions giv
10、en in TerminologiesE772 and G113 are applicable to this practice.4. Radiometer Selection4.1 Criteria for the Selection of Radiometers:4.1.1 There are several criteria that need to be consideredfor selection of the radiometer that will be used:4.1.1.1 Function specific criteria, such as whether a pyr
11、a-nometer, pyrheliometer or UV radiometer is required,4.1.1.2 Task specific criteria, such as the accuracy require-ments for the selected incident angle and temperature ranges,and maximum response time,4.1.1.3 Operational criteria, such as dimensions, weight,stability and maintenance, and4.1.1.4 Eco
12、nomic criteria, such as when networks have to beequipped, or whether the instrument is being acquired forinternal reference purposes, or for research purposes, etc.4.2 Selection Related to Radiometer Type:4.2.1 Pyranometers, which measure global solar irradiancein the 300 to 2500 nm wavelength regio
13、n, are required to assessthe hemispherical solar irradiance on surfaces of test specimens1This practice is under the jurisdiction of ASTM Committee G03 on Weatheringand Durability and is the direct responsibility of Subcommittee G03.09 onRadiometry.Current edition approved Dec. 1, 2010. Published De
14、cember 2010. Originallyapproved in 2005. Last previous edition approved in 2005 as G183 05. DOI:10.1520/G0183-05R10.2For 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
15、the standards Document Summary page onthe ASTM website.3Available from American National Standards Institute (ANSI), 25 W. 43rd St.,4th Floor, New York, NY 10036, http:/www.ansi.org.1Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959, United States.mou
16、nted on weathering test racks that are used by the outdoorweathering exposure community. Typically, pyranometers arerequired to measure the exposure levels specified in theapplicable ASTM and/or ISO outdoor weathering standardssuch as those described in Practices G7, G24, G90, andISO 877.4.2.2 Pyrhe
17、liometers, which measure direct (or, beam) solarirradiance in the 300 to 2500 nm wavelength region, arerequired to assess the solar irradiance reflected onto the targetboard by the mirrors of Fresnel Reflecting Concentrators usedin outdoor accelerated tests specified by ASTM and ISOStandards describ
18、ed in Practice G90 and ISO 877.4.2.3 Ultraviolet radiometers are either broad band or nar-row band instruments covering defined wavelength regions ofthe solar ultraviolet spectrum.4.2.3.1 Broad-band UV radiometers usually are designed tomeasure either UV-A, UV-B or some component of both UV-Aand UV-
19、B radiation.NOTE 2Certain UV radiometers that are designated as total ultravioletradiometers are advertised to measure over the total wavelength rangefrom the so called UV cutoff at approximately 300 nm to 385 or 400 nm,but in fact measure mostly UV-A radiation by virtue of their very lowresponsivit
20、y to wavelengths below 315 nm.4.2.3.2 Narrow-band UV radiometers are essentially con-structed using interference filters that isolate narrow bands ofradiation having FWHM values of 20 nm, or less; their centerwavelengths (CW) may reside anywhere in the UV spectrumfrom 280 to 400 nm wavelengthdependi
21、ng on the applicationfor which they are intended.NOTE 3While the World Meteorological Organization (WMO) andthe International Standards Organization (ISO) have established require-ments for Secondary Standard and First-, Second- and Third-classpyranometers and pyrheliometers, specifications and requ
22、ired operationalcharacteristics of different classes of ultraviolet radiometers have not beenaddressed by either organization.NOTE 4First-class instruments are not necessary for all applications.4.3 Selection Related to Measuring Specifications:4.3.1 As a first step, all possible ranges of measuring
23、parameters such as temperature, irradiance levels, angles ofincidence, tilt angles, and station latitude, must be compiled.4.3.2 Next, documentation must be compiled of availableinformation about the technical characteristics, and the techni-cal and physical specifications of the relevant radiometer
24、sgiven by:4.3.2.1 The WMO and ISO classification of pyranometersgiven in the WMO Guide, and in ISO 9060 and ISO 9370(which together define the specifications to be met by differentcategories of pyranometers and pyrheliometers),4.3.2.2 The data specification sheets obtained from themanufacturer, and4
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