ASTM D6574 D6574M-2013 red 2459 Standard Test Method for Determining the (In-Plane) Hydraulic Transmissivity of a Geosynthetic by Radial Flow《通过径向流测定土工合成物 (平面) 透水率的标准试验方法》.pdf
《ASTM D6574 D6574M-2013 red 2459 Standard Test Method for Determining the (In-Plane) Hydraulic Transmissivity of a Geosynthetic by Radial Flow《通过径向流测定土工合成物 (平面) 透水率的标准试验方法》.pdf》由会员分享,可在线阅读,更多相关《ASTM D6574 D6574M-2013 red 2459 Standard Test Method for Determining the (In-Plane) Hydraulic Transmissivity of a Geosynthetic by Radial Flow《通过径向流测定土工合成物 (平面) 透水率的标准试验方法》.pdf(6页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D6574 00 (Reapproved 2011)D6574/D6574M 13Standard Test Method forDetermining the (In-Plane) Hydraulic Transmissivity of aGeosynthetic by Radial Flow1This standard is issued under the fixed designation D6574;D6574/D6574M; the number immediately following the designation indicatesthe year
2、 of original adoption or, in the 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.1. Scope1.1 This test method covers the procedure for determining t
3、he in-plane transmissivity of geosynthetics under varying normalcompressive stresses using a radial flow apparatus. The test is intended to be an index test used primarily for geotextiles, althoughother products composed of geotextiles and geotextile-type materials may be suitable for testing with t
4、his test method.1.2 This test method is based on the assumption that the transmissivity of the geosynthetic is independent of orientation of theflow and is therefore limited to geosynthetics that have similar transmissivity in all directions and should not be used for materialswith oriented flow beh
5、avior.1.3 This test method has been developed specifically for geosynthetics that have transmissivity values on the order of or lessthan 2 104 m2/s. Consider using Test Method D4716 for geosynthetics with transmissivity values higher than 2 104 m2/s.1.4 The values stated in either SI units or inch-p
6、ound units are to be regarded separately as standard. The values given inparentheses are for information only. stated in each system may not be exact equivalents; therefore, each system shall be usedindependently of the other. Combining values from the two systems may result in non-conformance with
7、the standard.1.5 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 establish appropriate safety and health practices and determine the applicability of regulatorylimitations prior to use.2. R
8、eferenced Documents2.1 ASTM Standards:2D4354 Practice for Sampling of Geosynthetics and Rolled Erosion Control Products(RECPs) for TestingD4439 Terminology for GeosyntheticsD4491 Test Methods for Water Permeability of Geotextiles by PermittivityD4716 Test Method for Determining the (In-plane) Flow R
9、ate per Unit Width and Hydraulic Transmissivity of a GeosyntheticUsing a Constant HeadD5092 Practice for Design and Installation of Ground Water Monitoring Wells3. Terminology3.1 For definitions of terms relating to geosynthetics, refer to Terminology D4439.3.2 Definitions:3.2.1 geosynthetic, na pla
10、nar product manufactured from polymeric material used with soil, rock, earth, or other geotechnicalengineering related material as an integral part of a man-made project, structure, or system. D44393.2.2 geotextile, na permeable geosynthetic comprised solely of textiles. D44393.2.3 gravity flow, nfl
11、ow in a direction parallel to the plane of a geosynthetic driven predominantly by a difference in elevationbetween the inlet and outflow points of a specimen. D44391 This test method is under the jurisdiction of ASTM Committee D35 on Geosynthetics and is the direct responsibility of Subcommittee D35
12、.03 on Permeability andFiltration.Current edition approved June 1, 2011July 1, 2013. Published July 2011July 2013. Originally approved in 2000. Last previous edition approved in 20062011 asD6574 00(2006).(2011). DOI: 10.1520/D6574-00R11.10.1520/D6574_D6574M-13.2 For referencedASTM standards, visit t
13、heASTM website, www.astm.org, or contactASTM Customer Service at serviceastm.org. For Annual Book of ASTM Standardsvolume information, refer to the standards Document Summary page on the ASTM website.This document is not an ASTM standard and is intended only to provide the user of an ASTM standard a
14、n indication 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 t
15、o be considered the official document.Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959. United States13.2.3.1 DiscussionThe pressure at the outflow is considered to be atmospheric.3.2.4 head (static), nthe height above a standard datum of the surface
16、 of a column of water (or other liquid) that can besupported by a static pressure at a given point. The static head is the sum of the elevation head and the pressure head. D50923.2.5 hydraulic gradient, i, s (D), nthe loss of hydraulic head per unit distance of flow, dH/dL. D44393.2.5.1 DiscussionTh
17、e gradient is not constant from point to point in the direction of flow in the radial flow test. The gradient (mathematically) varieswith the inverse of the radial distance from the center.3.2.6 hydraulic transmissivity, (L2 T1), nfor a geosynthetic, the volumetric flow rate per unit width of specim
18、en per unitgradient in a direction parallel to the plane of the specimen. D44393.2.6.1 DiscussionTransmissivity is technically applicable only to saturated laminar flow hydraulic conditions.3.2.7 index test, na test procedure, which may contain a known bias but which may be used to establish an orde
19、r for a setof specimens with respect to the property of interest. D44393.2.8 in-plane flow, nfluid flow confined to a direction parallel to the plane of a geosynthetic. D44393.2.9 laminar flow, nflow in which the head loss is proportional to the first power of the velocity. D44393.2.10 normal stress
20、, (FL2), nthe component of applied stress that is perpendicular to the surface on which the force acts.D44393.2.11 turbulent flow, nthat type of flow in which any water particle may move in any direction with respect to any otherparticle and in which the head loss is approximately proportional to th
21、e second power of the velocity. D44393.3 Definitions of Terms Specific to This Standard:3.3.1 steady flow, nhydraulic flow conditions that do not vary with time at any given point.3.3.2 uniform flow, nhydraulic flow conditions where the cross-sectional area and the mean velocity in the direction of
22、floware constant from point to point.4. Summary of Test Method4.1 The transmissivity is determined using a device which transmits the flow of water radially outward from the center of atorus-shaped test specimen. The test method is performed with a constant head under a specific normal stress select
23、ed by the userand may be repeated using several gradients and under increasing normal stresses.4.2 The material property “hydraulic transmissivity” is technically applicable only to the regions of tests where the flow rateis constant with gradient, that is, the laminar region of the tests.4.3 In the
24、 constant head radial flow test, the flow regime is characterized as nonuniform steady flow since the cross-sectionalflow area and the hydraulic gradient vary from point to point along any radial flow line while remaining constant with time.5. Significance and Use5.1 This test method is an index tes
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