ASTM D5093-2015 Standard Test Method for Field Measurement of Infiltration Rate Using Double-Ring Infiltrometer with Sealed-Inner Ring《使用有密封内环的双环渗透计现场测量渗透率的标准试验方法》.pdf
《ASTM D5093-2015 Standard Test Method for Field Measurement of Infiltration Rate Using Double-Ring Infiltrometer with Sealed-Inner Ring《使用有密封内环的双环渗透计现场测量渗透率的标准试验方法》.pdf》由会员分享,可在线阅读,更多相关《ASTM D5093-2015 Standard Test Method for Field Measurement of Infiltration Rate Using Double-Ring Infiltrometer with Sealed-Inner Ring《使用有密封内环的双环渗透计现场测量渗透率的标准试验方法》.pdf(9页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D5093 02 (Reapproved 2008)D5093 15Standard Test Method forField Measurement of Infiltration Rate Using Double-RingInfiltrometer with Sealed-Inner Ring1This standard is issued under the fixed designation D5093; the number immediately following the designation indicates the year oforigina
2、l adoption or, in the case of revision, the year of last revision. A number in parentheses indicates the year of last reapproval. Asuperscript epsilon () indicates an editorial change since the last revision or reapproval.1. Scope1.1 This test method describes a procedure for measuring the infiltrat
3、ion rate of water through in-place soils using a double-ringinfiltrometer with a sealed inner ring.1.2 This test method is useful for soils with infiltration rates in the range of 1 1075 m/scm/s to 1 10108 m/s.cm/s. Wheninfiltration rates 1 1075 m/scm/s are to be measured Test Method D3385 shall be
4、used.1.3 All observed and calculated values shall conform to the guide for significant digits and rounding established in PracticeD6026.1.3.1 The method used to specify how data are collected, calculated, or recorded in this standard is not directly related to theaccuracy to which the data can be ap
5、plied in design or other uses, or both. How one applies the results obtained using this standardis beyond its scope.1.4 This test method provides a direct measurement of infiltration rate, not hydraulic conductivity. Although the units ofinfiltration rate and hydraulic conductivity are similar, ther
6、e is a distinct difference between these two quantities. They cannot bedirectly related unless the hydraulic boundary conditions, such as hydraulic gradient and the extent of lateral flow of water areknown or can be reliably estimated.1.5 This test method can be used for natural soil deposits, recom
7、pacted soil layers, and amended soils such as soil bentonite andsoil lime mixtures.1.6 UnitsThe values stated in SI units are to be regarded as standard. The values given in parentheses are for informationonly.mathematical conversions to inch-pound units, which are provided for information only and
8、are not considered standard.1.7 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 pr
9、ior to use.2. Referenced Documents2.1 ASTM Standards:2D653 Terminology Relating to Soil, Rock, and Contained FluidsD3385 Test Method for Infiltration Rate of Soils in Field Using Double-Ring InfiltrometerD3740 Practice for Minimum Requirements for Agencies Engaged in Testing and/or Inspection of Soi
10、l and Rock as Used inEngineering Design and ConstructionD6026 Practice for Using Significant Digits in Geotechnical Data3. Terminology3.1 Definitions:3.1.1 For common definitions of technical terms in this standard, refer to Terminology D653.3.2 Definitions:Definitions of Terms Specific to This Stan
11、dard:1 This test method is under the jurisdiction of ASTM Committee D18 on Soil and Rock and is the direct responsibility of Subcommittee D18.04 on Hydrologic Propertiesand Hydraulic Barriers.Current edition approved Sept. 1, 2008June 1, 2015. Published September 2008July 2015. Originally approved i
12、n 1990. Last previous edition approved in 20022008 asD5093 02.D5093 02(2008). DOI: 10.1520/D5093-02R08.10.1520/D5093-15.2 For referencedASTM standards, visit theASTM website, www.astm.org, or contactASTM Customer Service at serviceastm.org. For Annual Book of ASTM Standardsvolume information, refer
13、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 an indication of what changes have been made to the previous version. Becauseit may not be technically possible to adequately depict all chang
14、es accurately, ASTM recommends that users consult prior editions as appropriate. In all cases only the current versionof the standard as published by ASTM is to be considered the official document.Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959. Uni
15、ted States13.2.1 infiltrationdownward entry of liquid into a porous body.3.2.2 infiltration rate, Iquantity of liquid entering a porous material (m3) per unit area (m2) per unit time (s), expressed in unitsof m/s.3.2.3 infiltrometera device used to pond liquid on a porous body and to allow for the m
16、easurement of the rate at which liquidenters the porous body.3.1.4 For definitions of other terms used in this test method, see Terminology D653.4. Summary of Test Method4.1 The infiltration rate of water through soil is measured using a double-ring infiltrometer with a sealed or covered inner ring(
17、Fig. 1). The infiltrometer consists of an open outer and a sealed inner ring. The rings are embedded and sealed in trenchesexcavated in the soil. Both rings are filled with water such that the inner ring is submerged.4.2 The rate of flow is measured by connecting a flexible bag filled with a known w
18、eight of water to a port on the inner ring.As water infiltrates into the ground from the inner ring, an equal amount of water flows into the inner ring from the flexible bag.After a known interval of time, the flexible bag is removed and weighed. The weight loss, converted to a volume, is equal to t
19、heamount of water that has infiltrated into the ground. An infiltration rate is then determined from this volume of water, the area ofthe inner ring, and the interval of time. This process is repeated and a plot of infiltration rate versus time is constructed. The testis continued until the infiltra
20、tion rate becomes steady or until it becomes equal to or less than a specified value.5. Significance and Use5.1 This test method provides a means to measure low infiltration rates associated with fine-grained, clayey soils, and are in therange of 1 1075 m/scm/s to 1 10 98 m/s.cm/s.5.2 This test meth
21、od is particularly useful for measuring liquid flow through soil moisture barriers such as compacted clay lineror covers used at waste disposal facilities, for canal and reservoir liners, for seepage blankets, and for amended soil liners suchas those used for retention ponds or storage tanks.5.3 The
22、 purpose of the sealed inner ring is to: (1) provide a means to measure the actual amount of flow rather than a drop inwater elevation which is the flow measurement procedure used in Test Method D3385 and (2) to eliminate evaporation losses.5.4 The purpose of the outer ring is to promote one-dimensi
23、onal, vertical flow beneath the inner ring. The use of large diameterrings and large depths of embedments helps to ensure that flow is essentially one-dimensional.5.5 This test method provides a means to measure infiltration rate over a relatively large area of soil. Tests on large volumesof soil ca
24、n be more representative than tests on small volumes of soil.5.6 The data obtained from this test method are most useful when the soil layer being tested has a uniform distribution of porespace, and when the density and degree of saturation and the hydraulic conductivity of the material underlying t
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