ASTM D6574 D6574M-2013e1 9351 Standard Test Method for Determining the &40 In-Plane&41 Hydraulic Transmissivity of a Geosynthetic by Radial Flow《采用径向流动测定土工织物40在平面流41中液压输水作用的标准试验方法》.pdf
《ASTM D6574 D6574M-2013e1 9351 Standard Test Method for Determining the &40 In-Plane&41 Hydraulic Transmissivity of a Geosynthetic by Radial Flow《采用径向流动测定土工织物40在平面流41中液压输水作用的标准试验方法》.pdf》由会员分享,可在线阅读,更多相关《ASTM D6574 D6574M-2013e1 9351 Standard Test Method for Determining the &40 In-Plane&41 Hydraulic Transmissivity of a Geosynthetic by Radial Flow《采用径向流动测定土工织物40在平面流41中液压输水作用的标准试验方法》.pdf(5页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D6574/D6574M 131Standard Test Method forDetermining the (In-Plane) Hydraulic Transmissivity of aGeosynthetic by Radial Flow1This standard is issued under the fixed designation D6574/D6574M; the number immediately following the designation indicates theyear of original adoption or, in th
2、e case of revision, the year of last revision. A number in parentheses indicates the year of lastreapproval. A superscript epsilon () indicates an editorial change since the last revision or reapproval.1NOTETable 1 was editorially inserted in Section 11.3 in March 2014.1. Scope1.1 This test method c
3、overs the procedure for determiningthe in-plane transmissivity of geosynthetics under varyingnormal compressive stresses using a radial flow apparatus. Thetest is intended to be an index test used primarily forgeotextiles, although other products composed of geotextilesand geotextile-type materials
4、may be suitable for testing withthis test method.1.2 This test method is based on the assumption that thetransmissivity of the geosynthetic is independent of orientationof the flow and is therefore limited to geosynthetics that havesimilar transmissivity in all directions and should not be usedfor m
5、aterials with oriented flow behavior.1.3 This test method has been developed specifically forgeosynthetics that have transmissivity values on the order of orless than2104m2/s. Consider using Test Method D4716 forgeosynthetics with transmissivity values higher than 2 104m2/s.1.4 The values stated in
6、either SI units or inch-pound unitsare to be regarded separately as standard. The values stated ineach system may not be exact equivalents; therefore, eachsystem shall be used independently of the other. Combiningvalues from the two systems may result in non-conformancewith the standard.1.5 This sta
7、ndard 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 safety and health practices and determine the applica-bility of regulatory limitations prior to use.2. Referenced Documents2.1
8、ASTM Standards:2D4354 Practice for Sampling of Geosynthetics and RolledErosion Control Products(RECPs) for TestingD4439 Terminology for GeosyntheticsD4716 Test Method for Determining the (In-plane) FlowRate per Unit Width and Hydraulic Transmissivity of aGeosynthetic Using a Constant HeadD5092 Pract
9、ice for Design and Installation of GroundwaterMonitoring Wells3. Terminology3.1 For definitions of terms relating to geosynthetics, referto Terminology D4439.3.2 Definitions:3.2.1 geosynthetic, na planar product manufactured frompolymeric material used with soil, rock, earth, or other geo-technical
10、engineering related material as an integral part of aman-made project, structure, or system. D44393.2.2 geotextile, na permeable geosynthetic comprisedsolely of textiles. D44393.2.3 gravity flow, nflow in a direction parallel to theplane of a geosynthetic driven predominantly by a difference ineleva
11、tion between the inlet and outflow points of a specimen.D44393.2.3.1 DiscussionThe pressure at the outflow is consid-ered to be atmospheric.3.2.4 head (static), nthe height above a standard datum ofthe surface of a column of water (or other liquid) that can besupported by a static pressure at a give
12、n point. The static headis the sum of the elevation head and the pressure head. D50921This 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 approved July 1, 2013. Publis
13、hed July 2013. Originally approvedin 2000. Last previous edition approved in 2011 as D6574 00(2011). DOI:10.1520/D6574_D6574M-13E01.2For referenced ASTM standards, visit the ASTM website, www.astm.org, orcontact ASTM Customer Service at serviceastm.org. For Annual Book of ASTMStandards volume inform
14、ation, refer to the standards Document Summary page onthe ASTM website.Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959. United States13.2.5 hydraulic gradient, i, s (D), nthe loss of hydraulichead per unit distance of flow, dH/dL. D44393.2.5.1 Discu
15、ssionThe gradient is not constant from pointto point in the direction of flow in the radial flow test. Thegradient (mathematically) varies with the inverse of the radialdistance from the center.3.2.6 hydraulic transmissivity, (L2T1), nfor ageosynthetic, the volumetric flow rate per unit width ofspec
16、imen per unit gradient in a direction parallel to the plane ofthe specimen. D44393.2.6.1 DiscussionTransmissivity is technically appli-cable only to saturated laminar flow hydraulic conditions.3.2.7 index test, na test procedure, which may contain aknown bias but which may be used to establish an or
17、der for aset of specimens with respect to the property of interest. D44393.2.8 in-plane flow, nfluid flow confined to a directionparallel to the plane of a geosynthetic. D44393.2.9 laminar flow, nflow in which the head loss isproportional to the first power of the velocity. D44393.2.10 normal stress
18、, (FL2), nthe component of appliedstress that is perpendicular to the surface on which the forceacts. D44393.2.11 turbulent flow, nthat type of flow in which anywater particle may move in any direction with respect to anyother particle and in which the head loss is approximatelyproportional to the s
19、econd power of the velocity. D44393.3 Definitions of Terms Specific to This Standard:3.3.1 steady flow, nhydraulic flow conditions that do notvary with time at any given point.3.3.2 uniform flow, nhydraulic flow conditions where thecross-sectional area and the mean velocity in the direction offlow a
20、re constant from point to point.4. Summary of Test Method4.1 The transmissivity is determined using a device whichtransmits the flow of water radially outward from the center ofa torus-shaped test specimen. The test method is performedwith a constant head under a specific normal stress selected byth
21、e user and may be repeated using several gradients and underincreasing normal stresses.4.2 The material property “hydraulic transmissivity” is tech-nically applicable only to the regions of tests where the flowrate is constant with gradient, that is, the laminar region of thetests.4.3 In the constan
22、t head radial flow test, the flow regime ischaracterized as nonuniform steady flow since the cross-sectional flow area and the hydraulic gradient vary from pointto point along any radial flow line while remaining constantwith time.5. Significance and Use5.1 This test method is an index test to estim
23、ate andcompare the in-plane hydraulic transmissivity of one or severalcandidate geosynthetics under specific gradient and stressconditions.5.2 This test method may be used for acceptance testing ofcommercial shipments of geosynthetics, but caution is advisedsince information about between-laboratory
24、 precision is in-complete. Comparative tests as directed in 5.2.1 are advisable.5.2.1 In case of a dispute arising from differences inreported test results when using this procedure for acceptanceof commercial shipments, the purchaser and the suppliershould first confirm that the tests have been con
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