ASTM D5093-2002 Standard Test Method for Field Measurement of Infiltration Rate Using a Double-Ring Infiltrometer with a 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 Standard Test Method for Field Measurement of Infiltration Rate Using a Double-Ring Infiltrometer with a 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 Standard Test Method for Field Measurement of Infiltration Rate Using a Double-Ring Infiltrometer with a 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 02Standard Test Method forField Measurement of Infiltration Rate Using a Double-RingInfiltrometer with a Sealed-Inner Ring1This standard is issued under the fixed designation D 5093; the number immediately following the designation indicates the year oforiginal adoption or, in th
2、e 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. Scope *1.1 This test method describes a procedure for measuringthe infiltration rate of water
3、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 observed and cal
4、culated 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 otheruses,
5、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 difference betwee
6、n 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 amended soi
7、ls 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 theresponsibility of the
8、 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:D 653 Terminology Relating to Soil, Rock, and ContainedFluids2D 3385 Test Method for Infiltration Rate of Soi
9、ls in FieldUsing Double Ring Infiltrometers2D 3740 Practice for Minimum Requirements for AgenciesEngaged in the Testing and/or Inspection of Soil and RockUsed in Engineering Design and Construction2D 6026 Practice for Using Significant Digits in Geotechni-cal Data33. Terminology3.1 Definitions:3.1.1
10、 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 of the
11、 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 infil
12、trometer 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 to a p
13、ort on the innerring. 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 and weighed. The weight loss, converted to a volume,is equal to the amount of water that
14、has infiltrated into theground. An infiltration rate is then determined from thisvolume of water, the area of the inner ring, and the interval of1This test method is under the jurisdiction of ASTM Committee D18 on Soil andRock and is the direct responsibility of Subcommittee D18.04 on HydrologicProp
15、erties of Soil and Rocks.Current edition approved July 10, 2002. Published September 2002. Originallypublished as D509390. Last previous edition D509390(1997).2Annual Book of ASTM Standards, Vol 04.08.3Annual Book of ASTM Standards, Vol 04.09.1*A Summary of Changes section appears at the end of this
16、 standard.Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959, United States.time. This process is repeated and a plot of infiltration rateversus time is constructed. The test is continued until theinfiltration rate becomes steady or until it becomes eq
17、ual 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 range of 1 3 107m/s to 1 3 109m/s.5.2 This test method is particularly useful for measuringliquid flow through
18、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 used for retention ponds or storage tanks.5.3 The purpose of the sealed inner ring is to: (1) provide ameans t
19、o 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 purpose of the outer ring is to promote one-dimensional, vertical flow beneath the inner ring. The use oflarge dia
20、meter 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 area of soil. Tests on largevolumes of soil can be more representative than tests on smallvolumes of soil.5.6
21、 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 hydraulic conductivity of the material underlying the soillayer are known.5.7 Changes in water temperature can introd
22、uce 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 watercontained within the inner ring.5.8 The problem of temperature changes can be minimizedby insulating the rings
23、, 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 bag from the inner ring whenthe water in the inner ring is at the same temperature.5.9 If the soil being test
24、ed 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 are recommended for stud-ies of the influence of level of stress on the hydraulic propertiesof the soil.NOTE 1T
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