ASTM D4920-1998(2003) Standard Terminology Relating to Moisture in Textiles《有关纺织品水分的名词术语》.pdf
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1、Designation: D4920 98 (Reapproved 2003)Standard Terminology Relating toMoisture in Textiles1This standard is issued under the fixed designation D4920; the number immediately following the designation indicates the year oforiginal adoption or, in the case of revision, the year of last revision. A num
2、ber 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 terminology is a compilation of definitions oftechnical terms related to moisture in textiles. Terms that aregenerally understood or
3、 adequately defined in other readilyavailable sources are not included.1.2 For other ASTM defined conditioning terms, refer toTerminology E 41. For other terms associated with textiles,refer to Terminology D 123, Relating to Textiles.2. Referenced Documents2.1 ASTM Standards:D 123 Terminology Relati
4、ng to Textiles2E 41 Terminology Relating to Conditioning33. Terminology3.1 Definitions:absolute humidity, nthe mass of water vapor present in aunit volume of air.DISCUSSIONCommon units of measure for absolute humidity aregrams per cubic metre or grains per cubic foot. The amount of watervapor is als
5、o reported in terms of mass per unit mass of dry air, forexample, grams per kilogram, or grains per pound, of dry air. This valuediffers from values calculated on a volume basis and should not bereferred to as absolute humidity. It is designated as humidity ratio,specific humidity, or moisture pick-
6、up.absorption, na process in which one material (the absor-bent) takes in or absorbs another (the absorbate); as theabsorption of moisture by fibers. (See also adsorption, andmoisture equilibrium for testing. Compare desorption andresorption.) D 4772adsorption, na process in which the surface of a s
7、olid takeson or adsorbs in an extremely thin layer molecules of gases,of dissolved substances, or of liquids with which it is incontact. (See also absorption and moisture equilibrium fortesting. Compare desorption and resorption.)atmosphere for testing, nair at ambient conditions ofrelative humidity
8、 and temperature in which tests or experi-ments are conducted. (See also standard atmosphere fortesting.)DISCUSSIONIn the hierarchy of terms, atmosphere is the genericterm where the air is ambient with conditions “controlled” by localweather and therefore variable. Atmosphere for testing is a delimi
9、tedterm in which the use of the atmosphere is restricted for a certainpurpose. In a standard atmosphere for testing, the conditions arespecified (standardized) and controlled for routine testing and fortesting reproducibility. On this basis, there is no real reason for notreferring to the specified
10、atmospheres that have been traditionally usedfor testing glass textiles or tire cords, etc., as standard atmospheresfor testing those mercial allowance (CA), nan arbitrary value, equal tothe commercial moisture regain, plus a specified allowancefor finish, used with the mass of scoured, oven-dried y
11、arn, tocompute (1) yarn linear density, (2) the commercial or legalmass of a shipment or delivery of any specific textilematerial (see also commercial moisture regain), or (3) themass of a specific component in the analysis of fiber blends.D 1907, D 2494, D 3887commercial mass, nbilled mass as deter
12、mined by a gener-ally accepted method or as agreed upon between the pur-chaser and seller. D 2494commercial moisture content, nin wool, the moisturecalculated as a percentage of the mass of the wool, top, noils,yarn, fabric, etc., in the “as-is” condition; that is, containingwhatever moisture, oil,
13、grease, or other extraneous matterthat may be present. D2118commercial moisture regain (CMR), na formally adopted,arbitrary value, to be used with the oven-dried mass oftextile fibers, when calculating the commercial mass of ashipment or delivery.DISCUSSIONThe assigned commercial moisture regain val
14、ue isusually higher than the experimental moisture regain value for the samematerial.condition, vto bring a material to moisture equilibrium witha specified atmosphere.desorption, na process in which a sorbed material isreleased from another material, as the desorption of moisturefrom fibers; the re
15、verse of absorption, adsorption, or both.1This terminology is under the jurisdiction of ASTM Committee D13 on Textilesand is the direct responsibility of Subcommittee D13.51 on Chemical Conditioningand Performance.Current edition approved Oct. 10, 1996. Published February 1997. Originallypublished a
16、s D 4920 89. Last previous edition D 4920 96b.2Annual Book of ASTM Standards, Vol 07.01.3Annual Book of ASTM Standards, Vol 14.02.1Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959, United States.dew point, nthe temperature below which condensation of
17、water vapor begins to take place when the atmosphere iscooled.DISCUSSIONAs air is cooled, the amount of water vapor which it canhold decreases. If air is cooled sufficiently, the saturation water-vaporpressure becomes equal to the actual water-vapor pressure and anyfurther cooling beyond this point
18、will normally result in the conden-sation of moisture.humidity, nthe condition of the atmosphere in respect towater vapor. (Compare absolute humidity and relativehumidity.)hygrometer, nany instrument for measuring the humidity ofthe atmosphere.moisture, nas used with textiles, water absorbed, adsorb
19、ed,or resorbed by a material. (See also water.)moisture as-is, ndeprecated term. See moisture content.moisture as-received, ndeprecated term. See moisturecontent.moisture content, nthat part of the total mass of a materialthat is absorbed or adsorbed water, compared to the totalmass. (Compare moistu
20、re pick-up and moisture regain.)DISCUSSIONMoisture is usually expressed as a percentage and iscalculated using the equation:C 5 100 A 2 D!/Awhere:C = moisture content, %,A = mass of material before drying, andD = mass of the dried material.There is a relationship between moisture content and mois-tu
21、re pick-up since both may be calculated from the same data.The difference is in the bases used for calculating the percent-ages, original versus dried material mass. The relationshipbetween moisture content and moisture pick-up is shown bythe equations:C 5 100 P/100 1 P!P 5 100 C/100 2 C!where:C = m
22、oisture content, %, andP = moisture pick-up, %.moisture content, nat moisture-equilibrium, the moisturecontent of a material in equilibrium with air of known, orspecified, temperature and relative humidity.DISCUSSIONA frequently prescribed condition for determiningmoisture content at moisture-equili
23、brium is use of a standard atmo-sphere, for example, 21 6 1C (70 6 2F) and 65 6 2 % relativehumidity, for textiles, both in establishing the equilibrium and as airsupply for the drying oven.moisture content (dry-basis), ndeprecated term. See mois-ture pick-up.moisture (dry-basis), ndeprecated term.
24、See moisturepick-up.moisture equilibrium, nthe condition reached by a materialwhen it no longer takes up moisture from, or gives upmoisture to, the surrounding atmosphere. (Comparemoisture-free.)DISCUSSIONThe establishment of equilibrium between a materialand the surrounding atmosphere is dependent
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