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RESEARCH· ·1970·

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B258<br />

HYDROLOGIC TECHNIQUES<br />

1.0<br />

~<br />

Qj<br />

c.<br />

• e<br />

0..<br />

18, 2-3, 0.22<br />

12, 1-3, 0.45<br />

12, 1, 0.74<br />

[] :2.0 feet per second<br />

18, 1-3. 0.23<br />

I:' 0.1 ~<br />

Run No.<br />

u<br />

12 0.17<br />

16 0.13<br />

17 0.11<br />

18 0.17<br />

18, 1, 0.37<br />

16. 2-3, 0.22<br />

16, 1-3. 0.20<br />

17. 2-3, 0.36<br />

17. 1-3, 0.36<br />

[] = 3.2 feet per second<br />

16. 1, 0.33<br />

17. 1, 0.43<br />

0.01 ~1 ----'-------'------'---..___1_._0 ____ ..~--___ ~-----....J<br />

f, IN HERTZ<br />

FIGURE 4.-Efficiency of spatial resolution, 71 (f), as a function<br />

of frequency, f, for three Ott minor propellers tested in an<br />

open-channel flow with an artificially roughened boundary.<br />

iJ = 4.1 feet per second<br />

0.1~--~L---~---L~~----~----~---L~~~<br />

1.0<br />

V = 5.0 feet per second<br />

W, IN RADIANS PER SECOND<br />

n1easuren1ents was taken in the Atrisco Feeder Canal,<br />

15 miles north of Albuquerque; the second set in the<br />

Bernardo conveyance channel, 70 1niles· south. The<br />

mean values of the flow parmneters lor the cross section<br />

are given in table 1. All the flowmeter Ineasurements<br />

were taken using an Ott minor 1-3 propeller.<br />

The 1neasurements in a particular vertical were taken<br />

by first traversing the entire depth with the hot-fihn<br />

sensor, then with the propeller flown1eter; the vertical<br />

positions of the two instrmnents during 1neasurements<br />

were not always the same.<br />

Richardson and McQuivey (1968) report that 111<br />

·,,<br />

EXPLANATION<br />

Radius of<br />

oscillation,<br />

in inches<br />

• 6 0.969<br />

c 0.688<br />

• 0.469<br />

• 0 0.109<br />

FrauRE 3.-Absolute value of the system function, jH(w) j,<br />

as a function of angular frequency, w, for a 1-3 propeller.<br />

Two symbols for the same radius indicate measurements<br />

were .made on different days.<br />

FI.ELD MEASUREMENTS OF TUR'BULENCE-VELOCITY<br />

INTENSITIES AND POWER SPECTRAL DENSITIES<br />

The clatn. were taken at byo cross sections on the Rio<br />

Grande ncar Albuquerque, N. ~1cx. The first set of<br />

TABLE 1.-Flow parameters for the field measurements<br />

Flow parameter<br />

Depth (ft) ________ _<br />

Width (ft) ___ -·- ___ _<br />

Mean velocity<br />

(ft per sec) ______ _<br />

Discharge<br />

(ft a per sec) ____ _<br />

Slope __ - __ - ------­<br />

Shear velocity<br />

.(ft per sec) ______ _<br />

Manning's n ______ _<br />

Bed form _________ _<br />

Atrisco Feeder Canal 1<br />

1. 70<br />

56<br />

2. 13<br />

203<br />

. 00057<br />

. 177<br />

. 024<br />

Ripples and small<br />

dunes.<br />

Bernardo conveyance<br />

cbannel2<br />

2. 80<br />

68<br />

2.46<br />

468<br />

. 00055<br />

. 222<br />

. 028<br />

Dunes and plane<br />

with sediment<br />

motion.<br />

1 Power spectral densities and turbulence intensities were measured. The measurements<br />

of power spectral densities were taken at a velocity or 1.59 feet per second,<br />

mean depth of 1.83 feet, and 12 feet left of canal centerline.<br />

2 Turbulence intensities were measured. Right-hand half of channel had 8- to<br />

12-inch-high dunes, the rest was plane.

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