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RESEARCH· ·1970·

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GEO'LOGICAL SURVEY RESEARCH 1970<br />

COMPARISON OF A PROPELLER FLOWMETER WITH A<br />

HOT -FILM ANEMOMETER IN MEASURING TURBULENCE<br />

IN MOVABLE-BOUNDARY OPEN-CHANNEL FLOWS<br />

By J. P. BENNETT and R. S. McOUIVEY,<br />

Fort Collins, Colo.<br />

Abstract.-The hot-film anemometer may be used in measuring<br />

turbulence in large-scale movable-boundary open-channel flows<br />

if a correction is made for the drift of the velocity-voltage<br />

relation of the sensor. The propeller flowmeter may be used for<br />

making turbulence measurements in such flows if corrections<br />

are made for the frequency response and spatial averaging of the<br />

propeller. The true power spectral density, S(w), of the turbulence<br />

velocity may be obtained from S(w) =Soo(w) IH(w) l- 2 '17(w)- 1 ,<br />

where S 00 (w) is the power spectral density of the propeller meter,<br />

IH(w) I is the amplitude of the meter system function, and '17(w)<br />

is the efficiency of spatial resolution. Measurements of turbulence<br />

intensity and power spectral density were made with both hotfilm<br />

anemometer and propeller flowmeter in large-scale openchannel<br />

flows. The power spectral densities from the instruments<br />

are similar in shape except at the higher frequencies where<br />

effects of propeller spatial averaging appear. The efficiency of the<br />

propeller flowmeter as a device for measuring turbulence increases<br />

as the scale of the turbulence increases.<br />

In hydraulic-engineering research the present great<br />

need is for an instrument that can measure the characteristics<br />

of turbulence in flowing water in all situations.<br />

To obtain the statistical parameters describing<br />

turbulence, one should use a measuring system which<br />

has ( 1) a frequency response adequate to follow the<br />

velocity fluctuations instantaneously (2) a sensor<br />

smaller than the areal extent o£ the smallest velocity<br />

fluctuations containing significant energy, and (3) a<br />

readily obtainable and stable relation between the system<br />

output and the actual velocity. If the system does<br />

not satisfy these requirements in some respect, suitable<br />

corrections .mus.t be applied to the measurements.<br />

Two instruments which can be used to determine the<br />

characteristics of turbulence in water are the hot-film<br />

anemometer and the propeller flowmeter. Neither of<br />

these is, however, completely satisfactory for making<br />

turbulence measurements under the conditions encountered<br />

in natural flows. The hot-film anemometer is unstable<br />

when used in water containing suspended or dissolved<br />

impurities, and the propeller flowmeter has too<br />

low a frequency response and covers too great an area<br />

to respond completely to the turbulence-velocity fluctuations<br />

at a point.<br />

This paper is presented to show how, despite their<br />

· shortcomings, the hot-film anemometer and the propeller<br />

flowmeter can be used to measure the characteristics<br />

of turbulence in water and to compare measurements<br />

made with them in large-scale movable-boundary<br />

open-channel flow.<br />

INSTRUMENTATION SYSTEMS<br />

The transformation of the output of a measuring<br />

system to obtain turbulence statistics requires an application<br />

of the theories of the transient response of systems;<br />

however, before these theories can be applied,<br />

one must understand the systems to be used. The hotfilm<br />

anemometer and the propeller flowmeter measuring<br />

systems can best be understood by discussing the<br />

princi pies of operation of the sensors and the equipment<br />

necessary to convert sensor behavior into an<br />

analyzable output.<br />

The hot-film anemometer is similar to the hot-wire<br />

anemometer used in airflow measurements. The velocity<br />

sensor is ·electrically heated, and the heat is convected<br />

a·way by the flow, the rate of convection being proportional<br />

to the flow velocity. In water, a constant-temperature<br />

anemometer is generally used. In the constanttemperature<br />

anemometer, the circuitry is designed to<br />

keep the temperature of the velocity sensor constant by<br />

keeping its resistance constant. This is accomplished<br />

by varying the voltage across the sensor so that the<br />

B254<br />

U.S. GEOL. SURVEY PROF. PAPER 70o-B, PAGES B254-B262

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