ASTM D5614-1994(2014) 4504 Standard Test Method for Open Channel Flow Measurement of Water with Broad-Crested Weirs《采用宽口堰测量明渠水流流量的标准试验方法》.pdf
《ASTM D5614-1994(2014) 4504 Standard Test Method for Open Channel Flow Measurement of Water with Broad-Crested Weirs《采用宽口堰测量明渠水流流量的标准试验方法》.pdf》由会员分享,可在线阅读,更多相关《ASTM D5614-1994(2014) 4504 Standard Test Method for Open Channel Flow Measurement of Water with Broad-Crested Weirs《采用宽口堰测量明渠水流流量的标准试验方法》.pdf(8页珍藏版)》请在麦多课文档分享上搜索。
1、Designation: D5614 94 (Reapproved 2014)Standard Test Method forOpen Channel Flow Measurement of Water with Broad-Crested Weirs1This standard is issued under the fixed designation D5614; the number immediately following the designation indicates the year oforiginal adoption or, in the case of revisio
2、n, 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 covers measurement of the volumetricflow rate of water in open channels with two types
3、 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 standard. The values given in parentheses are mathematicalconversions to SI units that are provided for inform
4、ation onlyand are not considered standard.1.3 This standard does 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 and health practices and determine the applica-bility of regulator
5、y limitations prior to use.2. Referenced Documents2.1 ASTM Standards:2D1129 Terminology Relating to WaterD2777 Practice for Determination of Precision and Bias ofApplicable Test Methods of Committee D19 on WaterD3858 Test Method for Open-Channel Flow Measurementof Water by Velocity-Area Method2.2 IS
6、O Standards:3ISO 555-1973 Liquid Flow Measurement in OpenChannelsDilution Methods for Measurement of SteadyFlowConstant Rate Injection MethodISO 3846-1989 Liquid Flow Measurement in Open Chan-nels by Weirs and FlumesRectangular Broad-CrestedWeirsISO 4373-1979 Measurement of Liquid Flow in OpenChanne
7、lsWater Level Measuring DevicesISO 4374-1990 Liquid Flow Measurement in Open Chan-nels by Weirs and FlumesRound-Nose Horizontal CrestWeirs3. Terminology3.1 DefinitionsFor definitions of terms used in this testmethod, refer to Terminology D1129.3.2 Definitions of Terms Specific to This Standard:3.2.1
8、 boundary layer displacement thickness the bound-ary layer is a layer of fluid flow adjacent to a solid surface (inthis case, 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 edg
9、e ofthe layer. The displacement thickness is a distance normal tothe solid surface 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 ener
10、gy,expressed in terms of depth plus velocity head, is a minimumfor a given flow rate 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
11、 the square root of theproduct of the average depth and the acceleration due togravity.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 he
12、ad is referencedsimilarly to the crest elevation and measured downstream ofthe weir. 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 byconsi
13、derable turbulence or gravity waves, or both.3.2.7 nappethe curved sheet or jet of water overfalling thedownstream end of the weir.1This test method is under the jurisdiction of ASTM Committee D19 on Waterand is the direct responsibility of Subcommittee D19.07 on Sediments,Geomorphology, and Open-Ch
14、annel Flow.Current edition approved Jan. 1, 2014. Published March 2014. Originallyapproved in 1994. Last previous edition approved in 2008 as D5614 94 (2008).DOI: 10.1520/D5614-94R14.2For referenced ASTM standards, visit the ASTM website, www.astm.org, orcontact ASTM Customer Service at serviceastm.
15、org. For Annual Book of ASTMStandards volume information, refer to the standards Document Summary page onthe ASTM website.3Available from American National Standards Institute (ANSI), 25 W. 43rd St.,4th Floor, New York, NY 10036, http:/www.ansi.org.Copyright ASTM International, 100 Barr Harbor Drive
16、, PO Box C700, West Conshohocken, PA 19428-2959. United States13.2.8 primary devicethe device (in this case, the weir) thatcreates a hydrodynamic condition that can be sensed by thesecondary instrument.3.2.9 Reynolds numbera dimensionless number express-ing the ratio of inertial to viscous forces in
17、 a flow.The pertinentReynolds 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 instrument in this case, a device thatmeasures the depth of flow (referenced to the crest elevation)at an appro
18、priate location upstream 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 th
19、at a head measurement 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 levelo
20、n the downstream side 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-low
21、er and at higher velocity 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 acce
22、leration due to gravity.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
23、beobtained from a single 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
24、 accurate measure-ments 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
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