ASTM D5856-2015 red 6829 Standard Test Method for Measurement of Hydraulic Conductivity of Porous Material Using a Rigid-Wall Compaction-Mold Permeameter《使用刚性壁压缩模式磁导率计测量多孔材料液压导电率的标.pdf
《ASTM D5856-2015 red 6829 Standard Test Method for Measurement of Hydraulic Conductivity of Porous Material Using a Rigid-Wall Compaction-Mold Permeameter《使用刚性壁压缩模式磁导率计测量多孔材料液压导电率的标.pdf》由会员分享,可在线阅读,更多相关《ASTM D5856-2015 red 6829 Standard Test Method for Measurement of Hydraulic Conductivity of Porous Material Using a Rigid-Wall Compaction-Mold Permeameter《使用刚性壁压缩模式磁导率计测量多孔材料液压导电率的标.pdf(13页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D5856 95 (Reapproved 2007)D5856 15Standard Test Method forMeasurement of Hydraulic Conductivity of Porous MaterialUsing a Rigid-Wall, Compaction-Mold Permeameter1This standard is issued under the fixed designation D5856; the number immediately following the designation indicates the yea
2、r oforiginal adoption or, in the case of revision, 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. Scope1.1 This test method covers laboratory measurement of the h
3、ydraulic conductivity (also referred to as coeffcient of permeability)of laboratory-compacted materials with a rigid-wall, compaction-mold permeameter.1.2 This test method may be used with laboratory-compacted specimens that have a hydraulic conductivity less than or equalto 1 105 m/s. The hydraulic
4、 conductivity of compacted materials that have hydraulic conductivities greater than 1 105 m/smay be determined by Test Method D2434.1.3 UnitsThe values stated in SI units are to be regarded as the standard, unless other units are specifically given. By traditionin U.S. practice, hydraulic conductiv
5、ity is reported in centimetres per second, cm/s, although the common SI units for hydraulicconductivity are metres per second.m/s.1.4 This standard does not purport to address all of the safety concerns, if any, associated with its use. It is the responsibilityof the user of this standard to establi
6、sh appropriate safety and health practices and determine the applicability of regulatorylimitations prior to use.2. Referenced Documents2.1 ASTM Standards:2D653 Terminology Relating to Soil, Rock, and Contained FluidsD698 Test Methods for Laboratory Compaction Characteristics of Soil Using Standard
7、Effort (12 400 ft-lbf/ft3 (600 kN-m/m3)D854 Test Methods for Specific Gravity of Soil Solids by Water PycnometerD1557 Test Methods for Laboratory Compaction Characteristics of Soil Using Modified Effort (56,000 ft-lbf/ft3 (2,700kN-m/m3)D2216 Test Methods for Laboratory Determination of Water (Moistu
8、re) Content of Soil and Rock by MassD2434 Test Method for Permeability of Granular Soils (Constant Head) (Withdrawn 2015)3D3740 Practice for Minimum Requirements for Agencies Engaged in Testing and/or Inspection of Soil and Rock as Used inEngineering Design and ConstructionD4753 Guide for Evaluating
9、, Selecting, and Specifying Balances and Standard Masses for Use in Soil, Rock, and ConstructionMaterials TestingD5084 Test Methods for Measurement of Hydraulic Conductivity of Saturated Porous Materials Using a Flexible WallPermeameterE145 Specification for Gravity-Convection and Forced-Ventilation
10、 Ovens3. Terminology3.1 Definitions of Terms Specific to This Standard:Definitions:3.1.1 fluxquantity of flow per unit area per unit time.3.1.1 hydraulic conductivity, kthe rate of discharge of water under laminar flow conditions through a unit cross-sectional areaof a porous medium under a unit hyd
11、raulic gradient and standard temperature conditions (20C).1 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 edition approved May 1, 2007June 1, 2015. Publi
12、shed July 2007July 2015. Originally approved in 1995. Last previous edition approved in 20022007 asD585695(2002)D585695(2007).e1. DOI: 10.1520/D5856-95R07.10.1520/D5856-15.2 For referencedASTM standards, visit theASTM website, www.astm.org, or contactASTM Customer Service at serviceastm.org. For Ann
13、ual Book of ASTM Standardsvolume information, refer to the standards Document Summary page on the ASTM website.3 The last approved version of this historical standard is referenced on www.astm.org.This document is not an ASTM standard and is intended only to provide the user of an ASTM standard an i
14、ndication 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 appropriate. In all cases only the current versionof the standard as published by ASTM is to b
15、e considered the official document.Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959. United States13.1.1.1 DiscussionThe term coeffcient of permeability is often used instead of hydraulic conductivity ,conductivity, but hydraulic conductivity is used
16、exclusively in this test method. A more complete discussion of the terminology associated with Darcys law is given in theliterature4.3.1.3 pore volume of flowthe cumulative quantity of outflow from a test specimen divided by the volume of pore space in thespecimen.3.1.2 For common definitions of oth
17、ertechnical terms used in this test method seestandard, refer to Terminology D653.3.2 Definitions of Terms Specific to This Standard:3.2.1 fluxquantity of flow per unit area per unit time.3.2.2 pore volume of flowthe cumulative quantity of outflow from a test specimen divided by the volume of pore s
18、pace in thespecimen.4. Significance and Use4.1 This test method applies to one-dimensional, laminar flow of water within laboratory-compacted, porous materials such assoil.4.2 The hydraulic conductivity of porous materials generally decreases with an increasing amount of air in the pores of themater
19、ial. This test method applies to porous materials containing little or no air. The test method is designed to minimize theamount of air in the test specimen. However, this test method does not ensure complete saturation of the test specimen with water.In cases where it is essential to saturate the t
20、est specimen fully with water, the compacted specimen may be tested using TestMethod D5084.4.3 This test method applies to permeation of porous materials with water. Permeation with other liquids, such as chemicalwastes, can be accomplished using procedures similar to those described in this test me
21、thod. However, this test method is onlyintended to be used when water is the permeant liquid.4.4 It is assumed that Darcys law is valid and that the hydraulic conductivity is essentially unaffected by hydraulic gradient.The validity of DarcysDarcys law may be evaluated by measuring the hydraulic con
22、ductivity of the specimen at three hydraulicgradients; if all measured values are similar (within 25 %), then DarcysDarcys law may be taken as valid. However, when thehydraulic gradient acting on a test specimen is changed, the state of stress will also change, and, if the specimen or pore fluid isc
23、ompressible, the volume of the test specimen or pore fluid will change. Thus, some change in hydraulic conductivity may occurwhen the hydraulic gradient is altered, even in cases where DarcysDarcys law is valid.4.5 One potential problem with this method of testing is the possibility that water will
24、flow along the interface between the testspecimen and the compaction/permeameter ring. The problem tends to be of minimal significance for materials that swell whenexposed to water (for example, compacted, clayey soils) but can be a very serious problem for materials that might tend to shrinkand pul
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