ASTM D5298-2016 Standard Test Method for Measurement of Soil Potential (Suction) Using Filter Paper《用滤纸测量土壤电位(吸力)的标准试验方法》.pdf
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1、Designation: D5298 10D5298 16Standard Test Method forMeasurement of Soil Potential (Suction) Using Filter Paper1This standard is issued under the fixed designation D5298; 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.1. Scope1.1 This test method covers laboratory filter papers as passive sensors to evaluate the soil matric (matrix) and total pot
3、ential(suction), a measure of the free energy of the pore-water or tension stress exerted on the pore-water by the soil matrix (1, 2).2 Theterm potential or suction is descriptive of the energy status of soil water.1.2 This test method controls the variables for measurement of the water content of f
4、ilter paper that is in direct contact with soilor in equilibrium with the partial pressure of water vapor in the air of an airtight container enclosing a soil specimen. The filterpaper is enclosed with a soil specimen in the airtight container until moisture equilibrium is established; that is, the
5、partial pressureof water vapor in the air is in equilibrium with the vapor pressure of pore-water in the soil specimen.1.3 This test method provides a procedure for calibrating different types of filter paper for use in evaluating soil matric and totalpotential.1.4 UnitsThe values stated in SI units
6、 are to be regarded as standard. The inch-pound units given in parentheses areapproximate.mathematical conversions, which are provided for information purposes only and are not considered standard.1.5 This standard does not purport to address all of the safety concerns, if any, associated with its u
7、se. It is the responsibilityof the user of this standard to establish appropriate safety and health practices and determine the applicability of regulatorylimitations prior to use.2. Referenced Documents2.1 ASTM Standards:3C114 Test Methods for Chemical Analysis of Hydraulic CementD653 Terminology R
8、elating to Soil, Rock, and Contained FluidsD1125 Test Methods for Electrical Conductivity and Resistivity of WaterD2216 Test Methods for Laboratory Determination of Water (Moisture) Content of Soil and Rock by MassD3740 Practice for Minimum Requirements for Agencies Engaged in Testing and/or Inspect
9、ion of Soil and Rock as Used inEngineering Design and ConstructionD4542 Test Methods for Pore Water Extraction and Determination of the Soluble Salt Content of Soils by RefractometerD4753 Guide for Evaluating, Selecting, and Specifying Balances and Standard Masses for Use in Soil, Rock, and Construc
10、tionMaterials TestingD6836 Test Methods for Determination of the Soil Water Characteristic Curve for Desorption Using Hanging Column, PressureExtractor, Chilled Mirror Hygrometer, or CentrifugeE1E230/E230M Specification for ASTM Liquid-in-Glass Thermometersand Temperature-Electromotive Force (emf) T
11、ables forStandardized ThermocouplesE337 Test Method for Measuring Humidity with a Psychrometer (the Measurement of Wet- and Dry-Bulb Temperatures)E832 Specification for Laboratory Filter PapersE1137/E1137M Specification for Industrial Platinum Resistance ThermometersE2251 Specification for Liquid-in
12、-Glass ASTM Thermometers with Low-Hazard Precision LiquidsE2877 Guide for Digital Contact Thermometers1 This test method is under the jurisdiction of ASTM Committee D18 on Soil and Rock and is the direct responsibility of Subcommittee D18.04 on Hydrologic Propertiesand Hydraulic Barriers.Current edi
13、tion approved July 1, 2010Nov. 15, 2016. Published August 2010December 2016. Originally approved in 1992. Discontinued December 2002 and reinstatedas D529803. Last previous edition approved in 20032010 as D529803.10. DOI: 10.1520/D5298-10.10.1520/D5298-16.2 The boldface numbers in parentheses refer
14、to a list of references at the end of this standard.3 For referencedASTM standards, visit theASTM website, www.astm.org, or contactASTM Customer Service at serviceastm.org. For Annual Book of ASTM Standardsvolume information, refer to the standards Document Summary page on the ASTM website.This docu
15、ment is not an ASTM standard and is intended only to provide the user of an ASTM standard an indication of what changes have been made to the previous version. Becauseit may not be technically possible to adequately depict all changes accurately, ASTM recommends that users consult prior editions as
16、appropriate. In all cases only the current versionof the standard as published by ASTM is to be considered the official document.Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959. United States13. Terminology3.1 Definitions:3.1.1 For common definition
17、s of technical terms in this standard, refer to Terminology D653.3.2 Definitions of Terms Specific to This Standard:3.2.1 atmospherea unit of pressure equal to 76 cm Mercury or 101 kPa at 0 C.0C.3.2.2 matric (matrix) suction,suction (potential), hm (kPa)the negative pressure (expressed as a positive
18、 value), relative toambient atmospheric pressure on the soil water, to which a solution identical in composition with the soil water must be subjectedin order to be in equilibrium through a porous permeable wall with the soil water; pressure equivalent to that measured by TestMethods in geohydrology
19、/hydrogeology, matric D6836. Matric suction is a function of the relative humidity due to the differencein air the difference between the pore gas pressure, ug, and water pressure acrossthe pore water pressure, uw the water surface; therelative humidity or, in soil; that is, y = ug water vapor uw pr
20、essure decreases as the radius of curvature of the, which yields apositive value in either pressure FL2 water surface decreases. The term “matric” is grammatically correct, while matrix iscommonly used in the civil engineering literature.or pressure head, L.3.2.2.1 DiscussionIn most cases the pore g
21、as is air at atmospheric pressure. Matric suction is also referred to as capillary suction, capillary pressure,and capillary potential. Water flows from a soil with low matric suction (a moist soil) to soil with a high suction (a dry soil). Theterm matrix should not replace matric because only matri
22、c refers to the two solid-liquid binding mechanism (adsorption andcapillarity) contributing to the negative pore-water pressure, uw.3.2.3 molality, moles/1000 gnumber of moles of solute per 1000 g of solvent.3.2.4 molemolecular weight of a substance in grams.3.2.5 osmotic (solute) suction, hs (kPa)t
23、he negative pressure to which a pool of pure water must be subjected in order to bein equilibrium through a semipermeable membrane with a pool containing a solution identical in composition with the soil water;decrease in relative humidity due to the presence of dissolved salts in pore-water.3.2.6 p
24、Fa unit of negative pressure expressed as the logarithm to the base ten of the height in centimeters that a column ofwater will rise by capillary action or negative gauge pressure (kPa) divided by the unit weight of water (kN/m3) times 1000. pF 3 + logarithm to the base ten of the negative pressure
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