ASTM D2980-17 Standard Test Method for Saturated Density, Moisture-Holding Capacity, and Porosity of Saturated Peat Materials.pdf
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1、Designation: D2980 17Standard Test Method forSaturated Density, Moisture-Holding Capacity, and Porosityof Saturated Peat Materials1This standard is issued under the fixed designation D2980; the number immediately following the designation indicates the year oforiginal adoption or, in the case of rev
2、ision, 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. Scope*1.1 This test method was designed to evaluate the aeration,water penetration, and water retention prop
3、erties of peat underfield conditions of water saturation by measurement of thesaturated density, the moisture holding capacity, and theporosity.1.2 UnitsThe values stated in SI units are being regardedas standard. The values given in parentheses are mathematicalconversions to inch-pound units, which
4、 are provided forinformation only and are not considered standard.1.3 All observed and calculated values shall conform to theguidelines for significant digits and rounding established inPractice D6026.1.3.1 The procedures used to specify how data are collected/recorded or calculated in this standard
5、 are regarded as theindustry standard. In addition, they are representative of thesignificant digits that generally should be retained. The proce-dures used do not consider material variation, purpose forobtaining the data, special purpose studies, or any consider-ations for the users objectives; an
6、d it is common practice toincrease or reduce significant digits of reported data to becommensurate with these considerations. It is beyond the scopeof this standard to consider significant digits used in analysismethods for engineering design1.4 This standard does not purport to address all of thesa
7、fety 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. Referenced Documents2.1 ASTM Standards:2D653 Terminology Relating to S
8、oil, Rock, and ContainedFluidsD2974 Test Methods for Moisture, Ash, and Organic Matterof Peat and Other Organic SoilsD3740 Practice for Minimum Requirements for AgenciesEngaged in Testing and/or Inspection of Soil and Rock asUsed in Engineering Design and ConstructionD4753 Guide for Evaluating, Sele
9、cting, and Specifying Bal-ances and Standard Masses for Use in Soil, Rock, andConstruction Materials TestingD6026 Practice for Using Significant Digits in GeotechnicalDataE11 Specification for Woven Wire Test Sieve Cloth and TestSieves3. Terminology3.1 Definitions:3.1.1 For common definitions of com
10、mon terms in thisstandard, refer to Terminology D653.4. Summary of Test Method4.1 The test method sets up standardized conditions formeasuring the volume and mass of saturated peat. From thesedata, saturated volume, mass, moisture-holding capacity (on amass and volume basis), dry peat volumes, and p
11、orosity can bedetermined.5. Significance and Use5.1 This test method measures the air-filled spaces (poros-ity) and the moisture-holding capacity of peat on both a massand a volume basis under conditions of saturation. If largespaces are present, water and air can penetrate easily. If spacesare smal
12、ler, the water holding capacity is increased. Waterholding capacity is larger in humified peat materials (smallinter-particulate spaces) (sapric soil), whereas water and air-penetration is larger in unhumified peat (larger inter-particulatespaces) (fibric soil). The spaces can also be an indication
13、of theoxygen available to the plant roots.As such, the interplay of theproperties of moisture holding capacity and porosity dictate thebest use of the harvested organic soil material as well as thebest management practices for organic soils. The moisture1This test method is under the jurisdiction of
14、ASTM Committee D18 on Soil andRock and is the direct responsibility of Subcommittee D18.22 on Media for PlantGrowth.Current edition approved Feb. 1, 2017. Published February 2017. Originallyapproved in 1971. Last previous edition approved in 2010 as D2980 04(2010).DOI: 10.1520/D2980-17.2For referenc
15、ed 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 the standards Document Summary page onthe ASTM website.*A Summary of Changes section appears at the end of this standardCopyright
16、 ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959. United StatesThis international standard was developed in accordance with internationally recognized principles on standardization established in the Decision on Principles for theDevelopment of International
17、Standards, Guides and Recommendations issued by the World Trade Organization Technical Barriers to Trade (TBT) Committee.1retention relationships of these soils are critical to decisionsinvolving irrigation, drainage, and bearing capacity of thesesoil.NOTE 1The quality of the result produced by this
18、 standard isdependent on the competence of the personnel performing it, and thesuitability of the equipment and facilities used. Agencies that meet thecriteria of Practice D3740 are generally considered capable of competentand objective testing/sampling/inspection/etc. Users of this standard arecaut
19、ioned that compliance with Practice D3740 does not in itself assurereliable results. Reliable results depend on many factors; Practice D3740provides a means of evaluating some of those factors.5.2 Water retention values are particularly important in themanagement of organic soils. There is much conf
20、usion in theliterature about the moisture retention values being expressedin various bases; as a percent by volume; as a percent of ovendry mass; or as the percent of the wet mass. In somemanagement decisions, it is necessary to express the watercontents of organic soils on a volume basis because of
21、 theirvaried bulk densities, but because of the volume reductionoccurring on drying, the water contents must also be expressedon a wet volume basis as collected in the field. Whereas, inother management decisions, moisture retention values are bestexpressed on a dry mass basis. For example, the diff
22、erence inmass between the wet and oven dry sample is the moistureheld. These values are best expressed on a dry mass basis.Water holding capacities show a marked difference due to thedegree of decomposition in an organic soil. The mass of waterin fibric soil may be as much as 20 times the mass of th
23、e solidparticles, whereas that held in a sapric soil contains less thantwice the mass. If the water holding capacity is expressed on avolume basis these differences are much less apparent.6. Apparatus6.1 Dispensing Apparatus:6.1.1 Two dispensing burets, 250-cm3capacity in 1-cm3subdivisions, 62-cm3to
24、lerance, pinch-cock type;6.1.2 A one-hole No. 6 rubber stopper;6.1.3 Straight polyethylene drying tube with serrated rubbertubing fittings, 150 mm long, 19 mm (34 in.) in outsidediameter, 16 mm (58 in.) in inside diameter;6.2 A 4-mesh sieve conforming to Specification E11;6.3 Balance or Scale, a bal
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