ASTM D5093-2002(2008) 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 D5093-2002(2008) 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 D5093-2002(2008) 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(7页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D 5093 02 (Reapproved 2008)Standard Test Method forField Measurement of Infiltration Rate Using Double-RingInfiltrometer with Sealed-Inner Ring1This standard is issued under the fixed designation D 5093; the number immediately following the designation indicates the year oforiginal adop
2、tion 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 measuringthe infiltration rat
3、e of water through in-place soils using adouble-ring infiltrometer with a sealed inner ring.1.2 This test method is useful for soils with infiltration ratesin the range of 1 3 107m/s to 1 3 1010m/s. When infiltra-tion rates $1 3 107m/s are to be measured Test MethodD 3385 shall be used.1.3 All obser
4、ved and calculated values shall conform to theguide for significant digits and rounding established in PracticeD 6026.1.3.1 The method used to specify how data are collected,calculated, or recorded in this standard is not directly related tothe accuracy to which the data can be applied in design or
5、otheruses, or both. How one applies the results obtained using thisstandard is beyond its scope.1.4 This test method provides a direct measurement ofinfiltration rate, not hydraulic conductivity. Although the unitsof infiltration rate and hydraulic conductivity are similar, thereis a distinct differ
6、ence between these two quantities. Theycannot be directly related unless the hydraulic boundaryconditions, such as hydraulic gradient and the extent of lateralflow of water are known or can be reliably estimated.1.5 This test method can be used for natural soil deposits,recompacted soil layers, and
7、amended soils such as soilbentonite and soil lime mixtures.1.6 The values stated in SI units are to be regarded asstandard. The values in parentheses are for information only.1.7 This standard does not purport to address all of thesafety concerns, if any, associated with its use. It is theresponsibi
8、lity 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 ASTM Standards:2D 653 Terminology Relating to Soil, Rock, and ContainedFluidsD 3385 Test Method for Infiltration
9、Rate of Soils in FieldUsing Double-Ring InfiltrometerD 3740 Practice for Minimum Requirements for AgenciesEngaged in Testing and/or Inspection of Soil and Rock asUsed in Engineering Design and ConstructionD 6026 Practice for Using Significant Digits in Geotechni-cal Data3. Terminology3.1 Definitions
10、:3.1.1 infiltrationdownward entry of liquid into a porousbody.3.1.2 infiltration rate, Iquantity of liquid entering a po-rous material (m3) per unit area (m2) per unit time (s),expressed in units of m/s.3.1.3 infiltrometera device used to pond liquid on aporous body and to allow for the measurement
11、of the rate atwhich liquid enters the porous body.3.1.4 For definitions of other terms used in this test method,see Terminology D 653.4. Summary of Test Method4.1 The infiltration rate of water through soil is measuredusing a double-ring infiltrometer with a sealed or covered innerring (Fig. 1). The
12、 infiltrometer consists of an open outer and asealed inner ring. The rings are embedded and sealed intrenches excavated in the soil. Both rings are filled with watersuch that the inner ring is submerged.4.2 The rate of flow is measured by connecting a flexiblebag filled with a known weight of water
13、to a port on the inner1This test method is under the jurisdiction ofASTM Committee D18 on Soil andRock and is the direct responsibility of Subcommittee D18.04 on HydrologicProperties and Hydraulic Barriers.Current edition approved Sept. 1, 2008. Published September 2008. Originallyapproved in 1990.
14、Last previous edition approved in 2002 as D 5093 02.2For referenced ASTM standards, visit the ASTM website, www.astm.org, orcontact ASTM Customer Service at serviceastm.org. For Annual Book of ASTMStandards volume information, refer to the standards Document Summary page onthe ASTM website.1Copyrigh
15、t ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959, United States.ring.As water infiltrates into the ground from the inner ring, anequal amount of water flows into the inner ring from theflexible bag. After a known interval of time, the flexible bag isremoved
16、and weighed. The weight loss, converted to a volume,is equal to the amount of water that has infiltrated into theground. An infiltration rate is then determined from thisvolume of water, the area of the inner ring, and the interval oftime. This process is repeated and a plot of infiltration ratevers
17、us time is constructed. The test is continued until theinfiltration rate becomes steady or until it becomes equal to orless than a specified value.5. Significance and Use5.1 This test method provides a means to measure lowinfiltration rates associated with fine-grained, clayey soils, andare in the r
18、ange of 1 3 107m/s to 1 3 109m/s.5.2 This test method is particularly useful for measuringliquid flow through soil moisture barriers such as compactedclay liner or covers used at waste disposal facilities, for canaland reservoir liners, for seepage blankets, and for amended soilliners such as those
19、used for retention ponds or storage tanks.5.3 The purpose of the sealed inner ring is to: (1) provide ameans to measure the actual amount of flow rather than a dropin water elevation which is the flow measurement procedureused in Test Method D 3385 and (2) to eliminate evaporationlosses.5.4 The purp
20、ose of the outer ring is to promote one-dimensional, vertical flow beneath the inner ring. The use oflarge diameter rings and large depths of embedments helps toensure that flow is essentially one-dimensional.5.5 This test method provides a means to measure infiltra-tion rate over a relatively large
21、 area of soil. Tests on largevolumes of soil can be more representative than tests on smallvolumes of soil.5.6 The data obtained from this test method are most usefulwhen the soil layer being tested has a uniform distribution ofpore space, and when the density and degree of saturation andthe hydraul
22、ic conductivity of the material underlying the soillayer are known.5.7 Changes in water temperature can introduce significanterror in the volume change measurements. Temperaturechanges will cause water to flow in or out of the inner ring dueto expansion or contraction of the inner ring and the water
23、contained within the inner ring.5.8 The problem of temperature changes can be minimizedby insulating the rings, by allowing enough flow to occur sothat the amount of flow resulting from a temperature change isnot significant compared to that due to infiltration, or byconnecting and disconnecting the
24、 bag from the inner ring whenthe water in the inner ring is at the same temperature.5.9 If the soil being tested will later be subjected toincreased overburden stress, then the infiltration rate can beexpected to decrease as the overburden stress increases. Labo-ratory hydraulic conductivity tests a
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