ASTM D3385-2018 Standard Test Method for Infiltration Rate of Soils in Field Using Double-Ring Infiltrometer《用双环渗透仪现场测定土壤渗透率的标准试验方法》.pdf
《ASTM D3385-2018 Standard Test Method for Infiltration Rate of Soils in Field Using Double-Ring Infiltrometer《用双环渗透仪现场测定土壤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 D3385-2018 Standard Test Method for Infiltration Rate of Soils in Field Using Double-Ring Infiltrometer《用双环渗透仪现场测定土壤渗透率的标准试验方法》.pdf(8页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D3385 18Standard Test Method forInfiltration Rate of Soils in Field Using Double-RingInfiltrometer1This standard is issued under the fixed designation D3385; the number immediately following the designation indicates the year oforiginal adoption or, in the case of revision, the year of
2、last revision. A number in parentheses indicates the year of last reapproval. Asuperscript epsilon () indicates an editorial change since the last revision or reapproval.This standard has been approved for use by agencies of the U.S. Department of Defense.1. Scope*1.1 This test method describes a pr
3、ocedure for field mea-surement of the rate of infiltration of liquid (typically water)into soils using double-ring infiltrometer.1.2 The infiltrometer is installed by driving into the soil.Theinfiltrometer also may be installed in a trench excavated in dryor stiff soils.1.3 Soils should be regarded
4、as natural occurring soils orprocessed materials or mixtures of natural soils and processedmaterials, or other porous materials, and which are basicallyinsoluble and are in accordance with requirements of 1.6.1.4 This test method is particularly applicable to relativelyuniform fine-grained soils, wi
5、th an absence of very plastic (fat)clays and gravel-size particles and with moderate to lowresistance to ring penetration.1.5 This test method may be conducted at the groundsurface or at given depths in pits, and on bare soil or withvegetation in place, depending on the conditions for whichinfiltrat
6、ion rates are desired. However, this test method cannotbe conducted where the test surface is below the groundwatertable or perched water table.1.6 This test method is difficult to use or the resultant datamay be unreliable, or both, in very pervious or impervious soils(soils with a hydraulic conduc
7、tivity greater than about 102cm/s or less than about 1 105cm/s) or in dry or stiff soils ifthese fracture when the rings are installed. For soils withhydraulic conductivity less than 1 105cm/s refer to TestMethod D5093.1.7 This test method cannot be used directly to determinethe hydraulic conductivi
8、ty (coefficient of permeability) of thesoil (see 5.2).1.8 UnitsThe values stated in SI units are to be regardedas the standard. The inch-pound units given in parentheses aremathematical conversions, which are provided for informationpurposes only and are not considered standard.1.9 This standard doe
9、s 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, health, and environmental practices and deter-mine the applicability of regulatory limitations prior to use.1.10 This internatio
10、nal standard was developed in accor-dance with internationally recognized principles on standard-ization established in the Decision on Principles for theDevelopment of International Standards, Guides and Recom-mendations issued by the World Trade Organization TechnicalBarriers to Trade (TBT) Commit
11、tee.2. Referenced Documents2.1 ASTM Standards:2D653 Terminology Relating to Soil, Rock, and ContainedFluidsD1452 Practice for Soil Exploration and Sampling byAugerBoringsD2216 Test Methods for Laboratory Determination of Water(Moisture) Content of Soil and Rock by MassD2488 Practice for Description
12、and Identification of Soils(Visual-Manual Procedures)D3740 Practice for Minimum Requirements for AgenciesEngaged in Testing and/or Inspection of Soil and Rock asUsed in Engineering Design and ConstructionD5093 Test Method for Field Measurement of InfiltrationRate Using Double-Ring Infiltrometer with
13、 Sealed-InnerRing3. Terminology3.1 DefinitionsFor common definitions of technical termsin this standard, refer to Terminology D653.1This test method is under the jurisdiction ofASTM Committee D18 on Soil andRock and is the direct responsibility of Subcommittee D18.04 on HydrologicProperties and Hydr
14、aulic Barriers.Current edition approved March 1, 2018. Published April 2018. Originallyapproved in 1975. Last previous edition approved in 2009 as D3385 09. DOI:10.1520/D3385-18.2For referenced ASTM standards, visit the ASTM website, www.astm.org, orcontact ASTM Customer Service at serviceastm.org.
15、For Annual Book of ASTMStandards volume information, refer to the standards Document Summary page onthe ASTM website.*A Summary of Changes section appears at the end of this standardCopyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959. United StatesThis
16、international standard was developed in accordance with internationally recognized principles on standardization established in the Decision on Principles for theDevelopment of International Standards, Guides and Recommendations issued by the World Trade Organization Technical Barriers to Trade (TBT
17、) Committee.13.2 Definitions of Terms Specific to This Standard:3.2.1 incremental infiltration velocitythe quantity of flowper unit area over an increment of time. It has the same unitsas the infiltration rate.3.2.2 infiltrationthe downward entry of liquid into thesoil.3.2.3 infiltration ratethe rat
18、e, based on measured incre-mental infiltration velocities, at which liquid can enter the soilunder specified conditions. During infiltration, this rate maydecrease with time until reaching a quasi-steady value.3.2.4 infiltrometera device for measuring the rate of entryof liquid into a porous body, f
19、or example, water into soil.4. Summary of Test Method4.1 The double-ring infiltrometer method consists of install-ing two open cylinders, one inside the other, into the ground,partially filling the rings with water or other liquid, and thenmaintaining the liquid at a constant level. The volume of li
20、quidadded to the inner ring, to maintain the liquid level constant isthe measure of the volume of liquid that infiltrates the soil. Thevolume infiltrated during timed intervals is converted to anincremental infiltration velocity by dividing by the area of theinner ring, usually expressed in centimet
21、er per hour (or inchper hour) and plotted versus elapsed time. The maximumsteady-state or average incremental infiltration velocity, de-pending on the purpose/application of the test is equivalent tothe infiltration rate.5. Significance and Use5.1 This test method is useful for field measurement of
22、theinfiltration rate of soils. Infiltration rates have application tosuch studies as liquid waste disposal, evaluation of potentialseptic-tank disposal fields, leaching and drainage efficiencies,irrigation requirements, water spreading and recharge, andcanal or reservoir leakage, among other applica
23、tions.5.2 Although the units of infiltration rate and hydraulicconductivity of soils are similar, there is a distinct differencebetween these two quantities. They cannot be directly relatedunless the hydraulic boundary conditions are known, such ashydraulic gradient and the extent of lateral flow of
24、 water, or canbe reliably estimated.5.3 The purpose of the outer ring is to promote one-dimensional, vertical flow beneath the inner ring.5.4 Many factors affect the infiltration rate, for example thesoil structure, soil layering, condition of the soil surface,degree of saturation of the soil, chemi
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