ASTM D5856-1995(2007) 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性材料液压导电率的标准试.pdf
《ASTM D5856-1995(2007) 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性材料液压导电率的标准试.pdf》由会员分享,可在线阅读,更多相关《ASTM D5856-1995(2007) 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性材料液压导电率的标准试.pdf(8页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D 5856 95 (Reapproved 2007)Standard Test Method forMeasurement of Hydraulic Conductivity of Porous MaterialUsing a Rigid-Wall, Compaction-Mold Permeameter1This standard is issued under the fixed designation D 5856; the number immediately following the designation indicates the year ofor
2、iginal adoption or, in the case of revision, the year of last revision. A number 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 test method covers laboratory measurement of thehydraul
3、ic conductivity (also referred to as coeffcient of per-meability) 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 lessthan or equal to 1 3 105m/s. The hydraulic con
4、ductivity ofcompacted materials that have hydraulic conductivities greaterthan 1 3 105m/s may be determined by Test Method D 2434.1.3 The values stated in SI units are to be regarded as thestandard, unless other units are specifically given. By traditionin U.S. practice, hydraulic conductivity is re
5、ported in centime-tres per second, although the common SI units for hydraulicconductivity are metres per second.1.4 This standard does not purport to address all of thesafety concerns, if any, associated with its use. It is theresponsibility of the user of this standard to establish appro-priate saf
6、ety and health practices and determine the applica-bility of regulatory limitations prior to use.2. Referenced Documents2.1 ASTM Standards:2D 653 Terminology Relating to Soil, Rock, and ContainedFluidsD 698 Test Methods for Laboratory Compaction Character-istics of Soil Using Standard Effort (12,400
7、 ft-lbf/ft3(600kN-m/m3)D 854 Test Methods for Specific Gravity of Soil Solids byWater PycnometerD 1557 Test Methods for Laboratory Compaction Charac-teristics of Soil Using Modified Effort (56,000 ft-lbf/ft3(2,700 kN-m/m3)D 2216 Test Methods for Laboratory Determination of Wa-ter (Moisture) Content
8、of Soil and Rock by MassD 2434 Test Method for Permeability of Granular Soils(Constant Head)D 4753 Guide for Evaluating, Selecting, and SpecifyingBalances and Standard Masses for Use in Soil, Rock, andConstruction Materials TestingD 5084 Test Methods for Measurement of Hydraulic Con-ductivity of Sat
9、urated Porous Materials Using a FlexibleWall PermeameterE 145 Specification for Gravity-Convection and Forced-Ventilation Ovens3. Terminology3.1 Definitions of Terms Specific to This Standard:3.1.1 fluxquantity of flow per unit area per unit time.3.1.2 hydraulic conductivity, kthe rate of discharge
10、ofwater under laminar flow conditions through a unit cross-sectional area of a porous medium under a unit hydraulicgradient and standard temperature conditions (20C).3.1.2.1 DiscussionThe term coeffcient of permeability isoften used instead of hydraulic conductivity, but hydraulicconductivity is use
11、d exclusively in this test method. A morecomplete discussion of the terminology associated with Dar-cys law is given in the literature3.3.1.3 pore volume of flowthe cumulative quantity ofoutflow from a test specimen divided by the volume of porespace in the specimen.3.1.4 For definitions of other te
12、rms used in this test methodsee Terminology D 653.4. Significance and Use4.1 This test method applies to one-dimensional, laminarflow of water within laboratory-compacted, porous materialssuch as soil.4.2 The hydraulic conductivity of porous materials gener-ally decreases with an increasing amount o
13、f air in the pores ofthe material. This test method applies to porous materialscontaining little or no air. The test method is designed tominimize the amount of air in the test specimen. However, this1This test method is under the jurisdiction ofASTM Committee D18 on Soil andRock and is the direct r
14、esponsibility of Subcommittee D18.04 on HydrologicProperties and Hydraulic Barriers.Current edition approved May 1, 2007. Published July 2007. Originally approvedin 1995. Last previous edition approved in 2002 as D 585695(2002)e1.2For referenced ASTM standards, visit the ASTM website, www.astm.org,
15、orcontact ASTM Customer Service at serviceastm.org. For Annual Book of ASTMStandards volume information, refer to the standards Document Summary page onthe ASTM website.3Olson, R. E., and Daniel, D. E., “Measurement of the Hydraulic Conductivityof Fine-Grained Soils,” Symposium on Permeability and G
16、roundwater ContaminantTransport, ASTM STP 746, ASTM, 1981, pp. 1864.1Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959, United States.test method does not ensure complete saturation of the testspecimen with water. In cases where it is essential to sat
17、uratethe test specimen fully with water, the compacted specimenmay be tested using Test Method D 5084.4.3 This test method applies to permeation of porous mate-rials with water. Permeation with other liquids, such aschemical wastes, can be accomplished using procedures simi-lar to those described in
18、 this test method. However, this testmethod is only intended to be used when water is the permeantliquid.4.4 It is assumed that Darcys law is valid and that thehydraulic conductivity is essentially unaffected by hydraulicgradient. The validity of Darcys law may be evaluated bymeasuring the hydraulic
19、 conductivity of the specimen at threehydraulic gradients; if all measured values are similar (within25 %), then Darcys law may be taken as valid. However, whenthe hydraulic gradient acting on a test specimen is changed, thestate of stress will also change, and, if the specimen or porefluid is compr
20、essible, the volume of the test specimen or porefluid will change. Thus, some change in hydraulic conductivitymay occur when the hydraulic gradient is altered, even in caseswhere Darcys law is valid.4.5 One potential problem with this method of testing is thepossibility that water will flow along th
21、e interface between thetest specimen and the compaction/permeameter ring. Theproblem tends to be of minimal significance for materials thatswell when exposed to water (for example, compacted, clayeysoils) but can be a very serious problem for materials thatmight tend to shrink and pull away from the
22、 walls of thepermeameter. Test Method D 5084 is recommended for anymaterial that tends to shrink when exposed to the permeantliquid.4.6 The correlation between results obtained with this testmethod and the hydraulic conductivities of in-place, com-pacted materials has not been fully investigated. Ex
23、periencehas sometimes shown that flow patterns in small, laboratory-prepared test specimens do not necessarily follow the samepatterns on large field scales and that hydraulic conductivitiesmeasured on small test specimens are not necessarily the sameas larger-scale values. Therefore, the results sh
24、ould be appliedto field situations with caution and by qualified personnel.5. Apparatus5.1 Hydraulic SystemConstant head (Test Method A),falling head (Test Methods B, C, and D), or constant rate offlow (Test Method E) systems may be used provided they meetthe criteria outlined as follows:5.1.1 Const
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