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Brady S. McElroy, P.E. USDA-NRCS Lamar, Colorado
Water Measurement Brady S. McElroy, P.E. USDA-NRCS Lamar, Colorado
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Objectives Why is water measurement important to IWM?
Explain some of the mathematics of water measurement Discuss some of the common measuring devices encountered in NRCS work Discuss other opportunities for measurement Work some example problems
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Why is water measurement important?
Difficult to effectively manage irrigation without measurement Positive aspects Maximize use of available water supply Reduced cost due to leached nutrients Reduced environmental impact from over-irrigation
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Why is water measurement important?
Some measurement may have a negative connotation Regulatory (mandated by state, etc.) Billing
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KANSAS
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Why is water measurement important?
Water is one of the most precious resources in the West Increased competition among water users
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“Whiskey is for drinking. Water is for fighting over.”
Mark Twain
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References Primary reference for NRCS is Chapter 9 of Part 623 (Irrigation) of the National Engineering Handbook States that NRCS’ reference shall be the Bureau of Reclamation’s Water Measurement Manual, 3rd edition, published in 1997 Available online at
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References Other useful references Other NRCS documents
Irrigator’s Guides Extension publications Hydraulic texts King’s Handbook of Hydraulics
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Definitions Volume: length3 Flow Rate (Q): volume/time Velocity: length/time Area: length2
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Definitions Head- measurement of the energy in a fluid. Units are typically length. Total head at a given point is the sum of three components Elevation head, which is equal to the elevation of the point above a datum Pressure head, which is the height of a column of static water that can be supported by the static pressure at the point Velocity head, which is the height to which the kinetic energy of the liquid is capable of lifting the liquid
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Definitions Pressure- measurement of the force acting on a surface. Units are force/length2 Often convenient to express in terms of feet of fluid (pressure head) h=p/γ (multiply psi x 2.31 for feet of H20)
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Units Typically in U.S. Customary units for irrigation work.
Units vary depending on type of measurement Q vs. volume Open channel vs. pipe flow
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Units Flow rate units expressed in volume/time Open channel flow
Cubic feet per second (cfs) second-feet Pipe flow Gallons per minute (gpm)
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Handy Conversion Factor
Units Handy Conversion Factor 1 cfs = gpm or 1 cfs ≈ 450 gpm
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Units May also vary regionally Shares
Some canals refer to a head of water as a delivery unit Not the same as energy measurement Miner’s inches 38.4 miner’s inches = 1 cfs (Colorado) 40 miner's inches = 1 cfs (California, et al.) 50 miner’s inches = 1 cfs (New Mexico, et al.)
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A share is not a share is not a share
Units A share is not a share is not a share Canal Allocation/share (cfs) Bessemer Colorado Rocky Ford Highline Oxford Otero Holbrook Catlin Rocky Ford Fort Lyon Amity cfs at 0.6 hr/share Lamar
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Units Volume units are often expressed in units of area x depth or depth Acre-foot = volume of water that would cover 1 acre to a depth of 1 foot 12 acre-inches 43,560 cubic feet 325,851 gallons
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Handy Conversion Factor
Units Handy Conversion Factor 1 cfs for 24 hours ≈ 2 acre-feet or 1 cfs ≈ 1 ac-in/hr
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Water Measurement Mathematics
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Water Measurement Mathematics
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Water Measurement Mathematics
Continuity Equation Q=vA Irrigator’s Equation Qt=Ad
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Continuity Equation Q=vA Q = flow rate v = velocity A = area Qin Qout
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Continuity Equation Q=vA v=Q/A A=Q/v
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Continuity Equation Given: d=12 inches v=2.5 ft/s Find: Q in cfs
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Continuity Equation Solution: Q = vA A = 0.785 ft2
v=2.5 ft/s 12 in. Solution: Q = vA A = ft2 Q = 2.5 ft/s x ft2 = 1.96 ft3/s
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Irrigator’s Equation Qt = Ad Q = flow rate t = time A = area D = depth
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d = Qt/A Q = Ad/t t = Ad/Q A = Qt/d
Irrigator’s Equation d = Qt/A Q = Ad/t t = Ad/Q A = Qt/d
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Irrigator’s Equation Given: d = 3 inches A = 50 acres Q = 2 cfs Find: Time required to apply d
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Irrigator’s Equation Solution: t = dA/Q 1 cfs ≈ 1 ac-in/hr
t = 75 hours
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Irrigator’s Equation Given: t = 36 hours A = 20 acres Q = 2 cfs Find: Depth of applied water, d
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Irrigator’s Equation Solution: d = Qt/A 1 cfs ≈ 1 ac-in/hr
d = 3.6 inches
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Water Measurement Devices
Most water measurement devices either sense or measure velocity, or measure either pressure or head. Tables, charts, or equations are then used to calculate the corresponding discharge
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Water Measurement Devices
Devices that sample or sense velocity Current meters Propeller meters Vane deflection meters Float and stopwatch
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Water Measurement Devices
Devices that measure head or pressure Open channel devices commonly use h Pipeline devices may use p Flumes Orifices Venturi meters Weirs Velocity is computed from h, so weirs are classifed as head measuring devices
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Open Channel Devices Weirs Flumes Submerged Orifices Other devices
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Weirs A weir is an overflow structure installed perpendicular to open channel flow Has a unique depth of water at an upstream measuring point for each discharge If the water springs clear of downstream face, acts as sharp-crested weir A long, raised channel control crest is a broad-crested weir
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Weirs Usually named for the shape of the overflow opening
Rectangular Triangular Cipolletti Lowest elevation on overflow is zero reference elevation for measuring h
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Weirs Rectangular weirs can be either contracted or suppressed
Suppressed weirs use side of flow channel for weir ends No side contraction occurs Often used in divide boxes Canal overshot gates can act as weirs
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Weirs
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Weirs Cipolletti Weir
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Weir Box Turnout with Cipolletti Weir
Weirs Weir Box Turnout with Cipolletti Weir
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90 degree triangular and suppressed rectangular
Weirs Compound Weir 90 degree triangular and suppressed rectangular
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Weirs Advantages Simple to construct Fairly good at passing trash
1 head measurement Disadvantages High head loss Susceptible to sedimentation problems Sensitive to approach and exit conditions
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Weirs Conditions needed for sharp-crested weirs
Upstream face should be plumb, smooth, normal to axis of channel Entire crest should be level for rectangular and Cipolletti. Bisector of V-notch angles should be plumb for triangular. Plate should be thin enough to act as a sharp-crested weir Chamfer downstream edge if necessary Upstream edge must be straight and sharp Thickness should be uniform for entire length
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Weirs Maximum downstream elevation should be at least 0.2 ft below crest Head measurement should be greater than 0.2 ft for optimal elevation Head is measured upstream 4 X maximum head on crest Approach must be kept free of sediment deposits
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Weirs Given: Standard Contracted Rectangular Weir L = 2 feet h = 0.40 feet Find: Q, in cfs Solution: Refer to Table A7-2 in BoR Water Measurement Manual, 3rd edition
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Weirs
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Weirs Inspection of Existing Structures Approach flow Turbulence
Rough water surface at staff gage Velocity head Exit flow conditions Worn equipment Poor installation Crest must be correctly installed
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Poor approach condition
Weirs Poor approach condition
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Sediment in approach pool
Weirs Sediment in approach pool
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Flumes Flumes are shaped open channel flow sections.
Force flow to accelerate Converging sidewalls Raised bottom Combination Force flow to pass through critical depth Unique relationship between water surface profile and discharge
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Flumes Two basic classes of flumes Long throated flumes
Parallel flow lines in control section Accurately rate with fluid flow analysis Short throated flumes Curvilinear flow in control section Calibrated with more precise measurement devices
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Short Throated Flumes Parshall Flume is most well-known example
of short throated flumes Developed by Ralph Parshall at Colorado Agricultural College (now Colorado State University) ASAE Historic Landmark
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Parshall Flumes Since the beginning of irrigated agriculture, it has been important to measure flows of irrigation water. Accuracy of early water measurement methods often suffered because of trash or sediment in the water, or unusual flow conditions. Ralph L. Parshall saw this problem when he began working for the USDA in 1915, as an irrigation research engineer. In 1922 he invented the flume now known by his name. When this flume is placed in a channel, flow is uniquely related to the water depth. By 1953 Parshall had developed the depth-flow relationships for flumes with throat widths from 3 inches to 50 feet. The Parshall flume has had a major influence on the equitable distribution and proper management of irrigation water. Thousands of flumes have been used to measure irrigation water, as well as industrial and municipal liquid flows throughout the world. This plaque marks the site of the original Colorado Agricultural College Hydraulics Laboratory, where Parshall carried out his historic experiments. DEDICATED BY THE AMERICAN SOCIETY OF AGRICULTURAL ENGINEERS 1985
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Parshall Flumes
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Parshall Flumes Designated by throat width
Measure 0.01 cfs with 1 inch flume Measure 3000 cfs with 50 foot flume Dimensions are standardized for each flume Not geometrically proportionate A 12 ft flume is not simply 3x a 4 ft flume Relate Ha (or Ha and Hb ) to discharge with rating equation, or consult appropriate chart
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Parshall Flumes Flow occurs under two conditions Free flow
Downstream water surface does not reduce discharge Requires only 1 head reading (Ha)
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Parshall Flumes Submerged flow
Downstream flow is high enough to reduce discharge 2 head readings required 50% submergence (Hb/Ha) on 1-3 inch flumes 80% submergence (Hb/Ha) ≥8 feet flumes After 90% submergence, flume is no longer effective Ha Hb
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Parshall Flumes Advantages
Relatively low head loss (1/4 of sharp crested weir) Handle some trash and sediment Well accepted May be mandated Many sizes are commercially available
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Parshall Flumes Disadvantages Complicated geometry for construction
Tight construction tolerances Aren’t amenable to fluid flow analysis BoR does not recommend for new construction
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Parshall Flumes
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Parshall Flumes Given: 1 foot throat Parshall Flume Free flow Ha = 0.40 feet Find: Q, in cfs Solution: Refer to Table A8-12 in BoR Water Measurement Manual, 3rd edition
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Parshall Flumes
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Parshall Flumes Given: 1 foot Parshall Flume Ha = 1 ft Hb = 0.8 ft Find: Q, in cfs
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Parshall Flumes Solution: Determine if submergence exceeds 70% (Hb/Ha) 0.8/1.0=0.8>0.7 Therefore, must correct for submergence
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Parshall Flumes Solution: From table A8-12, Q=3.95 cfs Find correction factor Use Figure 8-16
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Parshall Flumes
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Parshall Flumes Correction=0.35 ft3/s Actual Q =(free flow Q) – (correction) =3.95 ft3/s – 0.35 ft3/s =3.6 ft3/s
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Broad-crested Weirs Also called ramp flumes, Replogle flumes
Long throated flume where only the bottom is raised. No side contractions Also called ramp flumes, Replogle flumes
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Broad-crested Weirs
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Long throated flume (broad-crested weir) under construction)
Broad-crested Weirs Long throated flume (broad-crested weir) under construction)
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Long throated flume (broad-crested weir) Q = 1200 cfs
Broad-crested Weirs Long throated flume (broad-crested weir) Q = 1200 cfs
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Broad-crested Weirs Advantages
Easily constructed, especially in existing concrete lined channels WinFlume software available to quickly design and rate structures Less expensive construction Low head loss Handle trash and sediment well
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Broad-crested Weirs Disadvantages
Some state laws or compacts may preclude use Not readily accepted by some water users Not what they’re used to using
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Other Flumes Several other types of flumes are used H-flumes
Cutthroat flumes Palmer-Bowles
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Other Flumes
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Flumes Inspection of Existing Structures Approach flow Turbulence
Flumes are in-line structures Should have smooth flow across width and depth of cross section Length of straight approach varies depending on control width, channel width, and velocity Turbulence Level both along and perpendicular to flow Excessive submergence Exit flow conditions
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Submerged Orifices A well defined sharp-edged opening in a wall or bulkhead through which flow occurs When size and shape of the orifice and the heads acting on it are known, flow measurement is possible Orifices are typically circular or rectangular in shape Can be used to regulate and measure water in a turnout structure Radial gates can act as submerged orifices
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Submerged Orifices
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Submerged Orifices Advantages Less head required than for weirs
Used where space limitations prevent weir or flume Disadvantages Sediment and debris accumulation will prevent accurate measuring Typically not used if conditions permit flumes which handle trash better
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Current Meters Velocity measuring devices Sample velocity at one point
Point sample isn’t representative of average velocity in flow are Develop relationship between observed and average velocity, or Take multiple velocity readings Use continuity equation (Q=vA) to compute discharge
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Current Meters Types of current meters Anemometer Propeller
Electromagnetic Doppler Optical strobe Anemometer and propeller are most common for irrigation work
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Anemometer type current meter
Current Meters Anemometer type current meter
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Other Open Channel Methods
Slope-Area Method Slope of water surface and average cross-sectional area used with Manning’s equation Difficult to estimate “n” Can only approximate Q
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Float Method Similar in concept to current meters
Velocity is estimated by timing how long a floating object takes to travel a pre-determined distance Observed velocity is adjusted by some factor to estimate average velocity Determine cross-sectional flow area Use continuity equation to estimate Q Provides only a rough estimate
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Float Method
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Pressurized Conduit Devices
Pipeline devices are usually classified by their basic operation Calibrated velocity sensing meters Differential head meters Positive volume displacement summing meters (municipal water) Measured proportional or calibrated bypass meters Acoustic meters
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Differential Head Meters
Include venturi, nozzle, and orifice meters When properly installed, accuracy ±1% Some irrigation operating conditions probably limit accuracy to ±3-5% No moving parts Uses principle of accelerating flow through a constriction Resulting pressure difference is related to discharge using tables or curves, or a suitable coefficient and the proper equation
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Venturi Meter Common differential head meter Minimal head loss
Full pipe flow required Also used to inject chemicals into an irrigation system Pressure reduction is used to pull chemicals into the system Examples of venturi meters constructed of standard plastic pipe fittings
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Venturi Meter
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Nozzle Meter Simplified form of venturi meter
Gradual downstream expansion of venturi is eliminated Higher head loss than venturi Full pipe flow required Not used extensively in irrigation
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Nozzle Meter
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Orifice Meter Another differential pressure meter
Often used for measuring well discharge Also used to measure chemical injections Typically small meters with details provided by manufacturer Requires long straight pipe lengths Full pipe flow required Limited discharge ratio
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Orifice Meter
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Elbow Meters Measure pressure difference between inside and outside of an elbow
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Propeller Meters Used at end of pipes and in conduits flowing full
Multiple blades that rotate on horizontal axle Must have full pipe flow Basically operate on Q=vA principle Usually have totalizer plus instantaneous discharge display Accuracy can be ±2-5% of actual flow
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Propeller Meters
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Saddle type propeller meter
Propeller Meters Saddle type propeller meter
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Propeller Meters
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Propeller Meters Should be selected to operate near middle of design discharge range If system has oversized pipes, some sections may need replaced with smaller pipes to provide correct velocity and approach Must be installed to manufacturer’s specifications for accurate measurement Must have full pipe flow
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Propeller Meters Advantages Commercially available Totalizing meter
Can achieve good accuracy
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Propeller Meters Disadvantages
Operating conditions different from manufacturer’s calibration conditions will affect accuracy Only tolerate small amount of weeds and debris Moving parts operating underwater Can require a good deal of maintenance and inspection
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Other Conduit Devices Pitot Tube Velocity Measurements Piezometer
Straight tube attached flush to wall and perpendicular Senses pressure head in pipe Pitot Tube Right angle bend inserted with horizontal leg pointed upstream and parallel to flow Senses both velocity and pressure head Velocity head, flow area, and coefficient can then be used to calculate flow rate
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Pitot Tube Velocity
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Other Conduit Devices Magnetic Flowmeters Deflection Meters
Use the principle that voltage is induced in an electrical conductor moving through a magnetic field. Conductor is flowing water For a given field strength, the magnitude of the induced voltage is proportional to velocity Deflection Meters Vane or plate projecting into flow and a sensing element to measure deflection Calibrated to indicate flow in desired units Vortex Flowmeters Obstructions in flow generate vortex shedding trails Properly shaped obstructions create vortices that can be sensed and related to velocity
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Other Conduit Methods Trajectory Method
Measure the horizontal and vertical coordinates of a point in the jet of water issuing from the end of a pipe Accurate ±15% Coordinates can be difficult to accurately measure
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Trajectory Method Vertical Pipe Horizontal Pipe
Two kinds of flow occur, depending on how high water rises <0.37d, circular weir Transistional region between >1.4d, jet flow Horizontal Pipe Pipe must be truly horizontal; slope will skew results Vertical component can be difficult to measure
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Trajectory Method
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Trajectory Method
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Trajectory Methods
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Other Conduit Methods Power Consumption Coefficients
Volume discharged from wells can be estimated using power consumption records Wells must be analyzed to determine the energy needed to pump a certain volume of water Relationship can then be used to estimate discharge volume Only certified well testers can perform the tests and develop the power consumption coefficient Must recalibrate every 4 years, or more often depending on conditions
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Other Conduit Methods Siphon Tubes
Estimate discharge based on head, diameter, and length of siphon tubes Accuracy ±10-15% Provides an in-field method of estimating flow Information also available in irrigator’s guides and NRCS Engineering Field Manual, Chapter 15
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Siphon Tubes
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Siphon Tubes
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Summary Water measurement is an important component of IWM
BoR Water Measurement Manual Continuity equation Q=vA Irrigator’s equation Qt=dA 1 cfs≈450 gpm 1 cfs≈1 ac-in/hr
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Summary Open channel devices Pressurized conduit devices Flumes Weirs
Submerged orifices Pressurized conduit devices Propeller meters Differential head meters
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Summary Installation requirements Other opportunities for measurement
Examine existing structures Other opportunities for measurement Canal gates Float method Power consumption coefficient Pipe trajectory Siphon tubes
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Questions?
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