ASTM D5614-1994(2003) Standard Test Method for Open Channel Flow Measurement of Water with Broad-Crested Weirs《用宽口堰测量明渠水流量的标准试验方法》.pdf
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1、Designation: D 5614 94 (Reapproved 2003)Standard Test Method forOpen Channel Flow Measurement of Water with Broad-Crested Weirs1This standard is issued under the fixed designation D 5614; the number immediately following the designation indicates the year oforiginal adoption or, in the case of revis
2、ion, 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. Scope1.1 This test method covers measurement of the volumetricflow rate of water in open channels with two ty
3、pes ofhorizontal broad-crested weirs: those having a square (sharp)upstream corner and those having a well-rounded upstreamcorner.1.2 The values stated in inch-pound units are to be regardedas the standard. The values given in parentheses are forinformation only.1.3 This standard does not purport to
4、 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 and health practices and determine the applica-bility of regulatory limitations prior to use.2. Referenced Documents2.1 ASTM Standards:D 1129 Ter
5、minology Relating to Water2D 2777 Practice for Determination of Precision and Bias ofApplicable Methods of Committee D19 on Water2D 3858 Practice for Open-Channel Flow Measurement ofWater by Velocity-Area Method22.2 ISO Standards:ISO 555-1973 Liquid Flow Measurement in OpenChannelsDilution Methods f
6、or Measurement of SteadyFlowConstant Rate Injection Method3ISO 3846-1989 Liquid Flow Measurement in Open Chan-nels by Weirs and FlumesRectangular Broad-CrestedWeirs3ISO 4373-1979 Measurement of Liquid Flow in OpenChannelsWater Level Measuring Devices3ISO 4374-1990 Liquid Flow Measurement in Open Cha
7、n-nels by Weirs and FlumesRound-Nose Horizontal CrestWeirs33. Terminology3.1 DefinitionsFor definitions of terms used in this testmethod, refer to Terminology D 1129.3.2 Definitions of Terms Specific to This Standard:3.2.1 boundary layer displacement thicknessthe boundarylayer is a layer of fluid fl
8、ow adjacent to a solid surface (in thiscase, the weir crest and sidewalls) in which, due to viscousfriction, the velocity increases from zero at the stationarysurface to an essentially frictionless-flow value at the edge ofthe layer. The displacement thickness is a distance normal tothe solid surfac
9、e that the flow streamlines can be considered tohave been displaced by virtue of the boundary-layer informa-tion.3.2.2 crestthe horizontal plane surface of the weir.3.2.3 critical flowopen channel flow in which the energy,expressed in terms of depth plus velocity head, is a minimumfor a given flow r
10、ate and channel. The Froude number is unityat critical flow.3.2.4 Froude numbera dimensionless number expressingthe ratio of inertial to gravity forces in free surface flow. It isequal to the average velocity divided by the square root of theproduct of the average depth and the acceleration due togr
11、avity.3.2.5 headin this test method, the depth of water above aspecified elevation. The measuring head is the depth of flowabove the weir crest measured at an appropriate locationupstream of the weir; the downstream head is referencedsimilarly to the crest elevation and measured downstream ofthe wei
12、r. The head plus the corresponding velocity head isoften termed the total head or total energy head.3.2.6 hydraulic jumpan abrupt transition from supercriti-cal flow to subcritical or tranquil flow, accompanied byconsiderable turbulence or gravity waves, or both.3.2.7 nappethe curved sheet or jet of
13、 water overfalling thedownstream end of the weir.3.2.8 primary devicethe device (in this case, the weir) thatcreates a hydrodynamic condition that can be sensed by thesecondary instrument.1This test method is under the jurisdiction of ASTM Committee D19 on Waterand is the direct responsibility of Su
14、bcommittee D19.07 on Sediments, Geomor-phology, and Open-Channel Flow.Current edition approved June 10, 2003. Published August 2003. Originallyapproved in 1994. Last previous edition approved in 1998 as D 5614 94 (1998).2Annual Book of ASTM Standards, Vol 11.01.3Available from American National Stan
15、dards Institute (ANSI), 25 W. 43rd St.,4th Floor, New York, NY 100361Copyright ASTM International, 100 Barr Harbor Drive, PO Box C700, West Conshohocken, PA 19428-2959, United States.3.2.9 Reynolds numbera dimensionless number express-ing the ratio of inertial to viscous forces in a flow. The pertin
16、entReynolds number on the weir crest is equal to the (critical)velocity multiplied by the crest length and divided by thekinematic viscosity of the water.3.2.10 secondary instrumentin this case, a device thatmeasures the depth of flow (referenced to the crest elevation)at an appropriate location ups
17、tream of the weir. The secondaryinstrument may also convert this measured head to an indicatedflow rate or could totalize flow rate.3.2.11 stilling wella small free-surface reservoir con-nected through a restricted passage to the head-measurementlocation upstream of the weir so that a head measureme
18、nt canbe made under quiescent conditions.3.2.12 subcritical flowopen channel flow that is deeperand at lower velocity than critical flow for the same flow rate;sometimes called tranquil flow.AFroude number less than oneexists.3.2.13 submergencea condition in which the water levelon the downstream si
19、de of the weir is high enough to affect theflow over the weir and hence alter the head-discharge relation.It is usually expressed as a ratio or percentage of downstreamto upstream head or downstream to upstream total head.3.2.14 supercritical flowopen channel flow that is shal-lower and at higher ve
20、locity than critical flow for the same flowrate. A Froude number greater than one exists.3.2.15 tailwaterthe water elevation immediately down-stream of the weir.3.2.16 tranquil flowsee subcritical flow.3.2.17 velocity headthe square of the average velocitydivided by twice the acceleration due to gra
21、vity.4. Summary of Test Method4.1 In broad-crested weirs, the length of the horizontal crestin the direction of flow is large enough relative to the upstreamhead for essentially rectilinear critical flow to occur at somepoint along the crest. This ideally permits the flow rate to beobtained from a s
22、ingle measurement of the upstream head; acorrective coefficient must be applied in practice. This coeffi-cient has been evaluated experimentally for square-edge weirsand can be determined analytically for rounded weirs.5. Significance and Use5.1 Broad-crested weirs can be used for accurate measure-m
23、ents of a wide range of flow rates, but their structuralsimplicity and sturdiness make them particularly useful formeasuring large flows under field conditions.5.2 Because they require vertical sidewalls, broad-crestedweirs are particularly adaptable to rectangular artificial chan-nels or to natural
24、 and artificial channels that can readily belined with vertical sidewalls in the immediate vicinity of theweir.6. Interferences6.1 Broad-crested weirs are not suitable for use in sediment-laden streams that are carrying heavy bed loads. However,floating debris is readily passed, particularly by the
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