ISO 4359:2013
(Main)Flow measurement structures — Rectangular, trapezoidal and U-shaped flumes
Flow measurement structures — Rectangular, trapezoidal and U-shaped flumes
ISO 4359:2013 specifies methods for the measurement of flow in rivers and artificial channels under steady or slowly varying flow conditions, using certain types of standing-wave, or critical-depth, flumes. A wide variety of flumes has been developed, but only those which have received general acceptance after adequate research and field testing, and which therefore do not require in situ calibration, are considered. The flow conditions considered are uniquely dependent on the upstream head, i.e. subcritical flow must exist upstream of the flume, after which the flow accelerates through the contraction and passes through its critical depth. The water level downstream of the structure is low enough to have no influence upon its performance. ISO 4359:2013 is applicable to three commonly used types of flumes, covering a wide range of applications, namely rectangular-throated, trapezoidal-throated and U-throated. It is not applicable to a form of flume referred to in the literature (sometimes called a "Venturi" flume) in which the flow remains subcritical throughout.
Structures de mesure du débit — Canaux jaugeurs à col rectangulaire, à col trapézoïdal et à col en U
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Standards Content (Sample)
INTERNATIONAL ISO
STANDARD 4359
Second edition
2013-02-15
Flow measurement structures —
Rectangular, trapezoidal and
U-shaped flumes
Structures de mesure du débit — Canaux jaugeurs à col rectangulaire,
à col trapézoïdal et à col en U
Reference number
ISO 4359:2013(E)
©
ISO 2013
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ISO 4359:2013(E)
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ISO 4359:2013(E)
Contents Page
Foreword .v
1 Scope . 1
2 Normative references . 1
3 Terms and definitions . 1
4 Symbols . 2
5 Flume types and principles of operation . 3
6 Installation . 6
6.1 Selection of site . 6
6.2 Installation conditions. 8
7 Maintenance .10
8 Measurement of head .11
8.1 General .11
8.2 Location of head measurement(s) .11
8.3 Gauge wells .11
8.4 Zero setting .12
9 General equations for discharge .12
9.1 Discharge based on critical flow in the flume throat .12
9.2 Discharge based on observed upstream head .13
9.3 Calculation of stage-discharge relationships .27
9.4 Approach velocity and coefficient of velocity .27
9.5 Selection of flume size and shape .28
10 Rectangular-throated flume .30
10.1 Description .30
10.2 Location of head measurement section .30
10.3 Provision for modular flow .30
10.4 Evaluation of discharge for a given observed upstream head .31
10.5 Computation of stage-discharge relationship .35
10.6 Limits of application.35
11 Trapezoidal-throated flumes .36
11.1 Description .36
11.2 Location of head measurement section .36
11.3 Provision for modular flow .37
11.4 Evaluation of discharge — Coefficient method .37
11.5 Computation of stage-discharge relationship .40
11.6 Limits of application.42
12 U-throated (round-bottomed) flumes .43
12.1 Description .43
12.2 Location of head measurement section .44
12.3 Provision for modular flow .44
12.4 Evaluation of discharge — Coefficient method .44
12.5 Computation of stage-discharge relationship .48
12.6 Limits of application.50
13 Uncertainties of flow measurement .51
13.1 General .51
13.2 Combining measurement uncertainties .52
13.3 Percentage uncertainty of discharge coefficient u*(C) for critical-depth flumes .54
13.4 Uncertainty budget.54
14 Example of uncertainty calculations .55
14.1 General .55
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ISO 4359:2013(E)
14.2 Characteristics — Gauging structure .55
14.3 Characteristics — Discharge calculation .55
14.4 Characteristics — Discharge coefficient .55
14.5 Characteristics — Gauged head instrumentation .56
14.6 Characteristics — Throat width .56
14.7 Overall uncertainty in discharge .57
Annex A (informative) Simplified head-discharge relationships for flume .58
Annex B (informative) Introduction to measurement uncertainty .63
Annex C (informative) Sample measurement performance for use in hydrometric
worked examples .72
Annex D (informative) Spreadsheets for use with this International Standard .75
Bibliography .77
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ISO 4359:2013(E)
Foreword
ISO (the International Organization for Standardization) is a worldwide federation of national standards
bodies (ISO member bodies). The work of preparing International Standards is normally carried out
through ISO technical committees. Each member body interested in a subject for which a technical
committee has been established has the right to be represented on that committee. International
organizations, governmental and non-governmental, in liaison with ISO, also take part in the work.
ISO collaborates closely with the International Electrotechnical Commission (IEC) on all matters of
electrotechnical standardization.
International Standards are drafted in accordance with the rules given in the ISO/IEC Directives, Part 2.
The main task of technical committees is to prepare International Standards. Draft International
Standards adopted by the technical committees are circulated to the member bodies for voting.
Publication as an International Standard requires approval by at least 75 % of the member bodies
casting a vote.
Attention is drawn to the possibility that some of the elements of this document may be the subject of
patent rights. ISO shall not be held responsible for identifying any or all such patent rights.
ISO 4359 was prepared by Technical Committee ISO/TC 113, Hydrometry, Subcommittee SC 2, Flow
measurement structures.
This second edition cancels and replaces the first edition (ISO 4359:1983), which has been technically
revised. It also incorporates the Technical Corrigendum ISO 4359:1983/Corr.1:1999.
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INTERNATIONAL STANDARD ISO 4359:2013(E)
Flow measurement structures — Rectangular, trapezoidal
and U-shaped flumes
1 Scope
This International Standard specifies methods for the measurement of flow in rivers and artificial
channels under steady or slowly varying flow conditions, using certain types of standing-wave, or
critical-depth, flumes.
A wide variety of flumes has been developed, but only those which have received general acceptance after
adequate research and field testing, and which therefore do not require in situ calibration, are considered.
The flow conditions considered are uniquely dependent on the upstream head, i.e. subcritical flow
must exist upstream of the flume, after which the flow accelerates through the contraction and passes
through its critical depth (see Figure 1). The water level downstream of the structure is low enough to
have no influence upon its performance.
This International Standard is applicable to three commonly used types of flumes, covering a wide
range of applications, namely rectangular-throated, trapezoidal-throated and U-throated. Typical field
installations are shown in Figure 2. Site conditions are important and Figure 3 shows acceptable velocity
profiles in the approach channel.
Detailed illustrations of the three types of flumes covered by this International Standard are given as follows:
a) rectangular-throated (see Figure 4);
b) trapezoidal-throated (see Figure 5);
c) U-throated, i.e. round-bottomed (see Figure 6).
It is not applicable to a form of flume referred to in the literature — sometimes called a “Venturi” flume
— in which the flow remains subcritical throughout.
NOTE This form is based on the same principle as a Venturi meter used within a closed conduit system and
relies upon gauging the head at two locations and the application of Bernoulli’s energy equation.
2 Normative references
The following documents, in whole or in part, are normatively referenced in this document and are
indispensable for its application. For dated references, only the edition cited applies. For undated
references, the latest edition of the referenced document (including any amendments) applies.
ISO 772, Hydrometry — Vocabulary and symbols
3 Terms and definitions
For the purposes of this document, the terms and definitions given in ISO 772 apply.
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ISO 4359:2013(E)
4 Symbols
Units of measurement are metres (m) and seconds (s) or derivatives of these.
Symbol Quantity Unit of measurement
2
A area of cross-section of flow m
B width of approach channel (width at bed if trapezoidal) m
b width of flume throat (width at bed if trapezoidal) m
C overall coefficient of discharge (rectangular flumes) non-dimensional
C coefficient of contraction non-dimensional
c
C coefficient of discharge non-dimensional
D
C shape coefficient for trapezoidal throated and U-throated flumes non-dimensional
s
C coefficient allowing for the effect of approach velocity non-dimensional
v
D diameter of base of U-throated flume m
d depth of flow m
E specific energy (relative to local invert) m
Fr Froude number non-dimensional
2
g gravitational acceleration m/s
H total head (relative to a specified datum, such as a flume invert) m
H correction to the total head m
*
h gauged head m
k equivalent sand roughness of surface, after Nikuradse mm
s
L length of prismatic section of the contraction at a flume m
L length of bellmouth entrance m
1
L length of slope (if present) between throat and downstream still- m
2
ing basin or channel floor
L length of stilling basin (if present) m
3
m side-slope (m horizontal to 1 vertical) non-dimensional
n number of measurements in series non-dimensional
P wetted perimeter of flow cross-section m
p height of flume invert above the invert of the approach channel m
3
Q discharge m /s
R radius m
Re Reynolds number non-dimensional
r radius of hump m
p
R radius of bellmouth entrance m
1
S standard deviation —
standard error of the mean —
S
average velocity through a cross-section, defined by Q/A m/s
V
w water surface width m
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ISO 4359:2013(E)
Symbol Quantity Unit of measurement
u*(Q) overall percentage uncertainty in the determination of discharge non-dimensional
68
expressed as a percentage standard deviation at 68 % confi-
dence limits
u*(b) percentage uncertainty in b (or D) non-dimensional
u*(C) percentage uncertainty in the combined coefficient value non-dimensional
u*(h) percentage uncertainty in h non-dimensional
u*(m) percentage uncertainty in m non-dimensional
α kinetic energy correction coefficient (taking into account non- non-dimensional
uniformity of velocity distribution)
β coefficient dependent on mean curvature of stream lines non-dimensional
γ, φ, ψ coefficients in the uncertainty computation —
δ* boundary layer displacement thickness m
η a numerical coefficient related to the sideslope angle in trapezoi- non-dimensional
dal flumes
2
ν kinematic viscosity of the fluid m /s
θ semi-angle subtended at the centre of curvature of the invert of a non-dimensional
U-throated flume between the water surface and the vertical
σ semi-angle subtended at the centre of curvature of the invert of a non-dimensional
U-throated flume between the water surface and the horizontal
Subscripts
a values in approach channel
c values at critical flow
d values downstream of the flume
e effective values after making allowance for boundary layer
effects
1 values assuming an ideal frictionless fluid
M maximum value
5 Flume types and principles of operation
5.1 The flumes covered by this International Standard are often known as “long-throated” or “critical-
depth” flumes and rely fundamentally on the occurrence of critical flow in the flume throat. When this
occurs, there is a unique relationship, for a given flume geometry, between the upstream head and the
discharge, that is independent of the conditions downstream of the flume throat. Figure 1 shows a
simplified sketch of where the critical depth typically occurs in a critical depth flume and the consequent
water surface profile through a long-throated trapezoidal flume, together with key hydraulic and
geometrical parameters.
a)
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ISO 4359:2013(E)
b) Section in approach channel upstream from throat
c) Section at downstream end of throat
Key
1 total energy line
2 typical flow profile
3 edge of boundary layer displacement thickness
δ* has been exaggerated.
Figure 1 — Trapezoidal-throated flume showing key geometrical parameters, water surface
profile and development of boundary layer displacement thickness (after Figure 8.1, Ref.[9])
5.2 Because the flume design is based on critical flow, this International Standard is largely based on
fundamental hydraulic theory, without the need for the large-scale volumetric testing that has been used
to derive the coefficients for other forms of flow measurement structure. In order to obtain critical flow
within the throat of the flume, the following conditions shall be satisfied.
a) The throat of the flume shall be long enough for the flow to be virtually parallel with the flume
invert, so that hydrostatic pressure conditions occur at the control section.
b) The entrance to the flume throat shall be shaped so that there are virtually no energy losses between
the point where the head is gauged and the point where critical flow occurs.
c) The flume throat shall constrict the channel severely enough to raise the energy level in the throat
sufficiently high above the energy level downstream to ensure that the flume is “modular”.
5.3 Figure 2 shows examples of flow in rectangular-throated, trapezoidal-throated and U-throated
flumes. The choice of flume type from these three depends upon several factors, such as the range of
discharge to be measured, the accuracy required, the head available and whether or not the flow carries
sediment that is liable to accrete. The graphs in Annex A give the user of this International Standard a
means of quickly comparing the idealized performance of a range of flume designs, to aid a preliminary
choice of the size and form of flume needed to deliver the required discharge capacity and stage–discharge
relationship.
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ISO 4359:2013(E)
a) Rectangular-throated flume b) Trapezoidal-throated flume c) U-throated flume
Figure 2 — Examples of rectangular-throated, trapezoidal-throated and U-throated flumes
5.4 The rectangular-throated flume is the simplest to construct. It generally proves necessary to raise
the invert of the flume throat above the bed of the channel upstream, in order to generate a constriction
that is sufficiently severe to allow low flows to be gauged. However, this may result in a regime of cyclic
sediment accretion and erosion upstream, which would affect the accuracy and consistency of gauging.
5.5 The trapezoidal-throated flume is more appropriate where a wide range of discharge is to be
measured with consistent accuracy. This shape of throat is also more likely to be suitable where it is
desirable to produce a particular stage-discharge relationship. In some cases, it is not necessary to raise
the invert of the throat above the approach channel invert when using a trapezoidal-throated flume, so
reducing the risk of upstream sediment accretion.
5.6 The U-throated flume is useful for installation in a U-shaped channel or where the flow is from a
circular-section conduit. It has found particular application in sewers and at sewage works.
5.7 The detailed theory for the critical-depth flume is given in Clauses 9 to 12, but is introduced here in
simplified form, based on the assumption of a uniform velocity across the flow section and disregarding
boundary layer effects. The basic discharge equation for a critical-depth flume can be derived from the
general energy equation:
22
V Q
Hd=+ =+d
2
2g
2gA
(1)
where
H is the total head above the flume invert;
d is the depth of flow;
V
is the average velocity through the section (= Q/A);
Q is the discharge;
A is the area of the flow cross-section;
g is the gravitational acceleration.
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ISO 4359:2013(E)
By differentiating the energy Formula (1) with respect to depth, it can be shown that, for critical flow:
3
gA
c
Q=
w
c
(2)
where subscript c refers to conditions at the critical-flow section.
Substituting Formula (2) into Formula (1) and disregarding any energy losses between the gauging
section and the critical-flow section, the following is obtained:
A
c
Hd=+
c
2w
c
(3)
5.8 In general, Formulae (2) and (3) are solved alongside each other for successive values of depth d
c
(with the corresponding values of area and surface width) to obtain the relationship between H and Q, but
for the special case of a flume with a rectangular throat (see Figure 4), they can be combined to produce
the explicit relationship:
2 2g
15,
Q= bH
3 3
(4)
5.9 This is readily recognizable as the same equation that applies (for an ideal fluid) for the flow over
a round-nosed horizontal-crested weir. In order to extend the use of this equation, three additional
coefficients may be introduced, resulting in the following generalized equation for long-throated critical-
depth flumes:
2 2g
15,
Q= CC Cbh
Ds v
3 3
(5)
where the coefficients are as follows:
C is a discharge coefficient that takes account of the non-ideal fluid properties, in particular the
D
effect of the boundary layer in the throat;
C is a shape coefficient, to allow for the effect of a non-rectangular flow section in the throat;
s
C is a velocity coefficient, to allow the upstream gauged head, h, to be used in place of the total
v
head or specific energy, H.
5.10 Equations for these coefficients are given in Clauses 9 to 12 and generally require an iterative
approach to be adopted.
6 Installation
6.1 Selection of site
6.1.1 The flume shall be located in a straight section of channel, avoiding local obstructions, roughness
or unevenness of the bed.
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ISO 4359:2013(E)
6.1.2 A preliminary study shall be made of the physical and hydraulic features of the proposed site, to
check that it conforms (or can be constructed or modified so as to conform) to the requirements necessary
for measurement of discharge by a flume. Particular attention should be paid to the following features in
selecting the site.
a) The availability of a straight length of approach channel of at least 10 times the maximum head
anticipated.
b) The existing velocity distribution.
c) The avoidance of a steep channel, the characteristics of which would induce supercritical flow.
d) The effects of any raised upstream water levels due to the measuring structure.
e) Conditions downstream, including such influences as tides, confluences with other streams, sluice
gates, mill dams and other controlling features which might cause submerged flow.
f) The impermeability of the ground on which the structure is to be founded and the necessity for
piling, grouting or other means of controlling seepage.
g) The necessity for floodbanks, to confine the maximum discharge to the channel.
h) The stability of the banks, and the necessity for trimming and/or revetment in natural channels.
i) The clearance of rocks or boulders from the bed of the approach channel.
j) Wind, which can have a considerable effect on the flow in a river, weir or flume, especially when
these are wide and the head is small and when the prevailing wind is in a transverse direction
(which would introduce a bias whose direction would depend on whether the gauge were at the
windward or leeward side of the approach channel).
6.1.3 If the site does not possess the characteristics necessary for satisfactory measurement, the site
shall be rejected unless suitable improvements are practicable.
6.1.4 If an inspection of the stream shows that the existing velocity distribution is reasonably uniform, then
it may be assumed that the velocity distribution will remain satisfactory after the construction of the flume.
6.1.5 If the existing velocity distribution is markedly non-uniform and no other site for the flume is
feasible, due consideration shall be given to checking the distribution after installation of the flume and
to improving it if necessary.
6.1.6 Several methods are available for obtaining a more precise indication of irregular velocity
distribution: velocity rods, floats or concentrations of dye can be used in small channels, the latter being
useful in checking conditions at the bottom of the channel. A complete and quantitative assessment of
velocity distribution may be made by means of a current-meter and other point velocity measurements.
NOTE Information about the use of current-meters is given in ISO 748. Further information on measuring
river velocities and using acoustic Doppler profilers can be found in ISO/TS 24154.
The user should confirm that the dye material used is acceptable for flow measurement purposes within
a natural channel in the country of operation.
6.1.7 Figure 3 gives typical examples of velocity distributions in channels of varying shape that can be
taken as acceptable for flow measurement purposes.
6.1.8 Flumes can act as obstacles to the movement of fish and other aquatic species. Care should
therefore be taken to ensure that the installation of gauging structures such as flumes does not have a
detrimental affect on the aquatic ecology where this might be an i
...
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