ASTM D5567-1994(2006) Standard Test Method for Hydraulic Conductivity Ratio (HCR) Testing of Soil Geotextile Systems《土壤土工合成织物系统液力传导比(CHR)标准试验方法》.pdf
《ASTM D5567-1994(2006) Standard Test Method for Hydraulic Conductivity Ratio (HCR) Testing of Soil Geotextile Systems《土壤土工合成织物系统液力传导比(CHR)标准试验方法》.pdf》由会员分享,可在线阅读,更多相关《ASTM D5567-1994(2006) Standard Test Method for Hydraulic Conductivity Ratio (HCR) Testing of Soil Geotextile Systems《土壤土工合成织物系统液力传导比(CHR)标准试验方法》.pdf(9页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D 5567 94 (Reapproved 2006)Standard Test Method forHydraulic Conductivity Ratio (HCR) Testing of Soil/Geotextile Systems1This standard is issued under the fixed designation D 5567; the number immediately following the designation indicates the year oforiginal adoption or, in the case of
2、 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 thehydraulic conductivity of water-saturated
3、 porous materialswith a flexible-wall permeameter.1.2 This test method may be used with undisturbed orcompacted soil specimens that have a hydraulic conductivityless than or equal to 5 3 102cm/s.1.3 The filtration behavior of soils with hydraulic conduc-tivities greater than 5 3 102cm/s may be deter
4、mined by thegradient ratio test (Test Method D 5101).1.4 The values stated in SI units are to be regarded as thestandard, although other units are provided for information andclarification purposes.1.5 This standard does not purport to address all of thesafety concerns, if any, associated with its u
5、se. 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:2D 422 Test Method for Particle-Size Analysis of SoilsD 653 Terminology Rel
6、ating to Soil, Rock, and ContainedFluidsD 698 Test Methods for Laboratory Compaction Character-istics of Soil Using Standard Effort (12,400 ft-lbf/ft3(600kN-m/m3)D 854 Test Methods for Specific Gravity of Soil Solids byWater PycnometerD 1587 Practice for Thin-Walled Tube Sampling of Soilsfor Geotech
7、nical PurposesD 2216 Test Methods for Laboratory Determination of Wa-ter (Moisture) Content of Soil and Rock by MassD 2487 Practice for Classification of Soils for EngineeringPurposes (Unified Soil Classification System)D 2488 Practice for Description and Identification of Soils(Visual-Manual Proced
8、ure)D 4220 Practices for Preserving and Transporting SoilSamplesD 4318 Test Methods for Liquid Limit, Plastic Limit, andPlasticity Index of SoilsD 4354 Practice for Sampling of Geosynthetics for TestingD 4439 Terminology for GeosyntheticsD 4491 Test Methods for Water Permeability of Geotextilesby Pe
9、rmittivityD 4647 Test Method for Identification and Classification ofDispersive Clay Soils by the Pinhole TestD 4751 Test Method for Determining Apparent OpeningSize of a GeotextileD 5084 Test Methods for Measurement of Hydraulic Con-ductivity of Saturated Porous Materials Using a FlexibleWall Perme
10、ameterD 5101 Test Method for Measuring the Soil-GeotextileSystem Clogging Potential by the Gradient Ratio3. Terminology3.1 Definitions:3.1.1 filter, na layer or combination of layers of previousmaterials designed and installed in such a manner as to providedrainage, yet prevent the movement of soil
11、particles due toflowing water (Terminology D 653).3.1.1.1 DiscussionA geotextile filter is the term used for alayer or combination of layers of pervious geosynthetic mate-rial(s) that are used in the capacity of a filter as defined above.3.1.2 geotextile, nany permeable textile material usedwith fou
12、ndation, soil, rock, earth, or any other geotechnicalengineering related material, as an integral part of a man-madeproduct, structure, or system (Terminology D 4439).3.1.3 hydraulic conductivity (k), nthe rate of discharge ofwater under laminar flow conditions through a unit cross-sectional area of
13、 a porous medium under a unit hydraulicgradient and standard temperature conditions (20C) (TestMethod D 5084).1This test method is under the jurisdiction of ASTM Committee D35 onGeosynthetics and is the direct responsibility of Subcommittee D35.03 on Perme-ability and Filtration.Current edition appr
14、oved June 15, 2006. Published February 2007. Originallyapproved in 1994. Last previous edition approved in 2001 as D 556794(2001).2For referenced ASTM standards, visit the ASTM website, www.astm.org, orcontact ASTM Customer Service at serviceastm.org. For Annual Book of ASTMStandards volume informat
15、ion, refer to the standards Document Summary page onthe ASTM website.1Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959, United States.3.1.3.1 DiscussionThe term coeffcient of permeability isoften used instead of hydraulic conductivity, but hydraulicc
16、onductivity is used exclusively in this test method.Acompletediscussion of the terminology associated with Darcys law isgiven in the literature.33.1.4 permeation, nthe transmission of a fluid through aporous medium (NEW).3.1.5 pore volumes of flow (Vpq), nthe cumulative volumeof flow through a test
17、specimen divided by the volume of voidswithin the specimen (modified from Test Method D 5084).3.2 Definitions of Terms Specific to This Standard:3.2.1 hydraulic conductivity ratio (HCR), n the ratio ofthe hydraulic conductivity of the soil/geotextile system, ksg,atany time during the test, to the in
18、itial hydraulic conductivity,ksgo, measured at the beginning of the test (NEW).4. Summary of Test Method4.1 This test method presents a procedure for performingpermeability tests of soil/geotextile systems. The techniquerequires placement of the soil and geotextile in a flexible-wallpermeameter.4.2
19、The soil/geotextile specimen is saturated using de-airedwater and back pressure techniques. The specimen is consoli-dated at the effective stress anticipated in the proposed appli-cation. The sample is then permeated with water. The hydraulicconductivity of the soil/geotextile specimen is measured a
20、ndplotted as a function of elapsed time and volume of waterpassing through the sample. The hydraulic conductivity mayeither increase or decrease during the test, depending on thebehavior of the geotextile filter. The test is terminated when astabilized hydraulic conductivity is obtained, or when the
21、hydraulic conductivity decreases below the minimum valueallowed by the drainage design.5. Significance and Use5.1 This test method is to be used for measuring thehydraulic conductivity of water-saturated soil/geotextile sys-tems.5.2 This test method is to be used as a design performancetest, or as a
22、 comparative tool for evaluating the filtrationbehavior of soils with geotextiles. This test method is notintended for routine (index-style) testing, since the results willdepend on the specific soil and hydraulic conditions that areevaluated. It is not appropriate to use the test results for jobspe
23、cifications or manufacturers certifications.5.3 This test method applies to the permeation of porousmaterials with water. Permeation with other liquids, such aschemical wastes, can be accomplished using procedures simi-lar to those described in this test method. However, this testmethod is intended
24、to be used only when water is the permeantliquid.5.4 The mathematical concepts (primarily Darcys law)used in this test method were originally developed for one-dimensional, laminar flow of water within porous materials,which is often the case with soil and geotextiles. When flowconditions are lamina
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