Lecture 6 - Streamflow Flashcards

1
Q

The flow of water in an open channel (or discharge) is defined as the volume of water passing a specified point in a given interval of time

A

Streamflow

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2
Q

The ————from a particular watershed can be measured at a particular gauging station by measuring the stage at the station and then converting the stage to an associated discharge using a rating curve.

A

Streamflow

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3
Q

generally measured by observing stage or elevation above a specified datum, in a channel and then relating stage to discharge via a rating curve.

A

Streamflow

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4
Q

are plots of water level vs. discharge.

A

Rating curves

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5
Q

The stage of a river is the height of the water surface above an established reference plane.

A

Water Stage

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6
Q

Requirements for the Watercourse During Measurement:

A

The watercourse has to be straight for at least 100 m upstream and downstream from the point of measurement for a regular velocity distribution in the water. No backwater effect. Close to the point of measurement, measurements of velocity have to be near as possible so stage-discharge curves can be compiled.

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7
Q

This gage may consist of a vertical scale attached to a bridge pier, piling, wharf, or other structure that extends into the low-water channel of the stream.

A

Staff Gage.

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8
Q

Lowered structure surface,

to the and readings are taken as a function of time through a storm event.

A

Wire-Weight Gage.

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9
Q

Uses a small amount of cork inside an enclosed staff gage. The cork floats as the water rises, and some adheres to the stick at the highest level reached by the water.

A

Crest Gage.

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10
Q

The only direct system measurement, which can measure the water stage continuously and automatically.

A

Float Gage.

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11
Q

Used mainly as an inside stilling well reference gage for a water level recorder and consist s of a float attached to a counterweight by means of cable or a stainless steel tape.

A

Float Gage.

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12
Q

Based on the measurement of pressure needed to produce bubbles against water pressure.

A

Bubble-Type Pneumatic Gage.

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13
Q

Mainly used when the location is not suitable for a float gage.

A

Bubble-Type Pneumatic Gage.

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14
Q

Most common method of measuring the stage of a river is through the use of a stilling well.

A

Stage Height

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15
Q

are located on the bank of a stream or on a bridge pier and are topped by a shelter that holds recorders and other instruments associated with the station.

A

Stilling wells

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16
Q

has a sensor located at either a fixed point above the water surface or a fixed point below water surface.

A

Ultrasonic Water Level Gage.

17
Q

Determination of the discharge of a river every time is laborious and time consuming that’s why it is a common practice to establish a relationship between the stage and discharge (rating curve) at a particular station.

A

Rating Curves

18
Q

DISCHARGE/STREAMFLOW MEASUREMENT

A
Velocity-Area Method.
Slope-Area Method.
Sluice gate and Spillway.
Weirs and Flumes.
Dilution Gauging.
Floats.
19
Q

Obtain a near instantaneous value of the discharge of a river. The discharge Q of a river being measured by means of measuring velocities (vi), representative for the part Ai of the area (A), in a suitable cross section.

A

Velocity-Area Method.

20
Q

is used to the measure velocity in a channel.

A

Current Meter

21
Q

Usually used in computing flood discharges. This method is less accurate and application is usually considered as an ad hoc method if other methods are not feasible.

A

Slope-Area Method.

22
Q

High-water or flood marks along reach of channel permit determination of the water-surface slope at the time of peak and cross sections of the channel are determined by leveling or sounding.

A

Slope-Area Method.

23
Q

The area and hydraulic radius are then calculated and the discharge is computed using the Manning’s formula.

A

Slope-Area Method.

24
Q

Usually used in computing discharges at dams.

A

Sluice gate and Spillway.

25
Q

It has the same hydraulic properties as the orifice.

A

Sluice gate and Spillway.

26
Q

Calibration tests are advisable if accurate measurements are to be determined since its coefficient of discharge varies widely

A

Sluice gate and Spillway.

27
Q

Usually used for flow measurements in small streams

A

Weirs and Flumes.

28
Q

Such structures have the advantage that they are less sensitive to the downstream conditions like the channel roughness and backwater effect.

A

Weirs and Flumes.

29
Q

These devices are rated on the basis of laboratory calibration, although the rating may be checked in place with current meters.

A

Weirs and Flumes.

30
Q

Usually used in very small streams in the mountainous areas.

A

Dilution Gauging.

31
Q

Rough measurements of discharge can be made by timing the speed of floats.

A

Floats.

32
Q

During peak flows, floats are the most appropriate instruments used for measuring discharges since they are cheap and easy to improvise.

A

Floats.