ASTM D6574-2000(2006) Standard Test Method for Determining the (In-Plane) Hydraulic Transmissivity of a Geosynthetic by Radial Flow《径向流动法测定土工合成物(平面)液压透射率的试验方法》.pdf
《ASTM D6574-2000(2006) Standard Test Method for Determining the (In-Plane) Hydraulic Transmissivity of a Geosynthetic by Radial Flow《径向流动法测定土工合成物(平面)液压透射率的试验方法》.pdf》由会员分享,可在线阅读,更多相关《ASTM D6574-2000(2006) Standard Test Method for Determining the (In-Plane) Hydraulic Transmissivity of a Geosynthetic by Radial Flow《径向流动法测定土工合成物(平面)液压透射率的试验方法》.pdf(5页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D 6574 00 (Reapproved 2006)Standard Test Method forDetermining the (In-Plane) Hydraulic Transmissivity of aGeosynthetic by Radial Flow1This standard is issued under the fixed designation D 6574; the number immediately following the designation indicates the year oforiginal adoption or,
2、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 the procedure for determiningthe in-plane transmissivity
3、 of geosynthetics under varyingnormal compressive stresses using a radial flow apparatus. Thetest is intended to be an index test used primarily for geotex-tiles, although other products composed of geotextiles andgeotextile-type materials may be suitable for testing with thistest method.1.2 This te
4、st 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 materials with oriented flow behavior.1.3 This test method ha
5、s been developed specifically forgeosynthetics that have transmissivity values on the order of orless than 2 3 104m2/s. Consider using Test Method D 4716for geosynthetics with transmissivity values higher than 2 3104m2/s.1.4 The values stated in SI units are to be regarded as thestandard. The values
6、 given in parentheses are for informationonly.1.5 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 safety and health practices and determine the applica-bility of regul
7、atory limitations prior to use.2. Referenced Documents2.1 ASTM Standards:2D 4354 Practice for Sampling of Geosynthetics for TestingD 4439 Terminology for GeosyntheticsD 4491 Test Methods for Water Permeability of Geotextilesby PermittivityD 4716 Test Method for Determining the (In-plane) FlowRate pe
8、r Unit Width and Hydraulic Transmissivity of aGeosynthetic Using a Constant HeadD 5092 Practice for Design and Installation of GroundWater Monitoring Wells3. Terminology3.1 For definitions of terms relating to geosynthetics, referto Terminology D 4439.3.2 Definitions:3.2.1 geosynthetic, na planar pr
9、oduct manufactured frompolymeric material used with soil, rock, earth, or other geo-technical engineering related material as an integral part of aman-made project, structure, or system. D 44393.2.2 geotextile, na permeable geosynthetic comprisedsolely of textiles. D 44393.2.3 gravity flow, nflow in
10、 a direction parallel to theplane of a geosynthetic driven predominantly by a difference inelevation between the inlet and outflow points of a specimen.D 44393.2.3.1 DiscussionThe pressure at the outflow is consid-ered to be atmospheric.3.2.4 head (static), nthe height above a standard datum ofthe s
11、urface of a column of water (or other liquid) that can besupported by a static pressure at a given point. The static headis the sum of the elevation head and the pressure head.D 50923.2.5 hydraulic gradient, i, s (D), nthe loss of hydraulichead per unit distance of flow, dH/dL. D 44393.2.5.1 Discuss
12、ionThe 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, u (L2T1), nfor a geosyn-thetic, the volumetric flow rate per unit width of s
13、pecimen perunit gradient in a direction parallel to the plane of thespecimen. D 44393.2.6.1 DiscussionTransmissivity is technically appli-cable only to saturated laminar flow hydraulic conditions.1This test method is under the jurisdiction of ASTM Committee D35 onGeosynthetics and is the direct resp
14、onsibility of Subcommittee D35.03 on Perme-ability and Filtration.Current edition approved June 1, 2006. Published June 2006. Originallyapproved in 2000. Last previous edition approved in 2000 as D 6574 00.2For referenced ASTM standards, visit the ASTM website, www.astm.org, orcontact ASTM Customer
15、Service at serviceastm.org. For Annual Book of ASTMStandards volume information, 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.3.2.7 index test, na test procedure, whi
16、ch may contain aknown bias but which may be used to establish an order for aset of specimens with respect to the property of interest.D 44393.2.8 in-plane flow, nfluid flow confined to a directionparallel to the plane of a geosynthetic. D 44393.2.9 laminar flow, nflow in which the head loss ispropor
17、tional to the first power of the velocity. D 44393.2.10 normal stress, (FL2), nthe component of appliedstress that is perpendicular to the surface on which the forceacts. D 44393.2.11 turbulent flow, nthat type of flow in which anywater particle may move in any direction with respect to anyother par
18、ticle and in which the head loss is approximatelyproportional to the second power of the velocity. D 44393.3 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
19、thecross-sectional area and the mean velocity in the direction offlow are 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 per
20、formedwith a constant head under a specific normal stress selected bythe 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 wi
21、th gradient, that is, the laminar region of thetests.4.3 In the constant 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 tim
22、e.5. Significance and Use5.1 This test method is an index test to estimate 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 geosynth
23、etics, but caution is advisedsince information about between-laboratory 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 purc
24、haser and the suppliershould first confirm that the tests have been conducted usingcomparable test parameters including specimen conditioning,normal stress, hydraulic system gradient, etc. Comparativetests then should be conducted to determine if there is astatistical bias between their laboratories
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