STREAM FLOW DYNAMICS AND SOIL EROSION

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LESSON 3.2

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Grace Balahay

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STREAM FLOW DYNAMICS AND SOIL EROSION


STREAM FLOW DYNAMICS AND SOIL EROSIONVersion en ligne LESSON 3.2 par Grace Balahay 1 Also known as runoff water, at a particular outlet in a river is the total collection of water coming from its watershed or drainage basin. Written answer 2 volume of water that moves over a designated point over a fixed period of time. Written answer 3 show information on changes in discharge valuable for predicting flooding, estimating long-term trends in water and sediment discharges, and for distinguishing possible long-term climate change. Written answer 4 affects food sources and migration of fish amongst other wildlife Written answer 5 Rough approximation of flow in a uniform and straight channel Written answer 6 Velocity of the float gives the surface or maximum velocity of water in the channel, and should be multiplied by about ______ to approximate the average velocity. Written answer 7 A wheel is rotated by water flow and the rate of the rotation signifies the water velocity. It is primarily used in measuring discharge Written answer 8 Velocity is proportional to the downstream frequency of the vortex flow and is read on a digital readout. It used for measuring flow in pipes. Written answer 9 Electronic pulses determine water velocity. Can be used in large bodies of water like oceans to measure the current Written answer 10 Based on many field tests, for flow depths less than ______, the average velocity of the stream vertical is at six-tenths depth below the surface. Written answer 11 For depths of _______, the average of the velocities at two-tenths and eight-tenths depth below the surface, equals the mean velocity in the vertical. Written answer 12 Determining the discharge using Manning’s Flow equations Written answer 13 Equations that determine the discharge in slope-area method Written answer 14 of a river outlet is a graph of stage or discharge versus time. Written answer 15 obtained from a recorder of water level or discharge installed at the gaging station of the river. • A result of the runoff processes compromising overland flow, interflow, and base flow that are generated by precipitation storms. Written answer 16 contributions from the delayed interflow and groundwater runoff. Written answer 17 contributions from surface runoff and quick interflow. Written answer 18 analysis refers only to direct runoff. Written answer 19 portion of the hydrograph, composed mostly of surface runoff. Written answer 20 zone of the hydrograph around peak discharge. Written answer 21 zone of the hydrograph after the peak discharge. Duration to fall from peak to base flow Written answer 22 is the normal flow of water in the river derived from throughflow and groundwater flow Written answer 23 duration from the start of direct runoff to peak flow. Written answer 24 duration that runoff is above the base flow Written answer 25 duration of water from farthest point in the watershed to reach outlet Written answer 26 lag time of the basin is the time between the center of mass of the runoff-producing rainfall to the peak rate of flow Written answer 27 rocky and impermeable Written answer 28 slightly permeable, bare Written answer 29 cultivated or covered with vegetation Written answer 30 cultivated absorbent soil Written answer 31 sandy soil Written answer 32 heavy forest Written answer

STREAM FLOW DYNAMICS AND SOIL EROSION

Test

À propos de cette activité

Créé par

Téléchargez la version pour jouer sur papier

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STREAM FLOW DYNAMICS AND SOIL EROSIONVersion en ligne

par Grace Balahay

Also known as runoff water, at a particular outlet in a river is the total collection of water coming from its watershed or drainage basin.

volume of water that moves over a designated point over a fixed period of time.

show information on changes in discharge valuable for predicting flooding, estimating long-term trends in water and sediment discharges, and for distinguishing possible long-term climate change.

affects food sources and migration of fish amongst other wildlife

Rough approximation of flow in a uniform and straight channel

Velocity of the float gives the surface or maximum velocity of water in the channel, and should be multiplied by about ______ to approximate the average velocity.

A wheel is rotated by water flow and the rate of the rotation signifies the water velocity. It is primarily used in measuring discharge

Velocity is proportional to the downstream frequency of the vortex flow and is read on a digital readout. It used for measuring flow in pipes.

Electronic pulses determine water velocity. Can be used in large bodies of water like oceans to measure the current

Based on many field tests, for flow depths less than ______, the average velocity of the stream vertical is at six-tenths depth below the surface.

For depths of _______, the average of the velocities at two-tenths and eight-tenths depth below the surface, equals the mean velocity in the vertical.

Determining the discharge using Manning’s Flow equations

Equations that determine the discharge in slope-area method

of a river outlet is a graph of stage or discharge versus time.

obtained from a recorder of water level or discharge installed at the gaging station of the river. • A result of the runoff processes compromising overland flow, interflow, and base flow that are generated by precipitation storms.

contributions from the delayed interflow and groundwater runoff.

contributions from surface runoff and quick interflow.

analysis refers only to direct runoff.

portion of the hydrograph, composed mostly of surface runoff.

zone of the hydrograph around peak discharge.

zone of the hydrograph after the peak discharge. Duration to fall from peak to base flow

is the normal flow of water in the river derived from throughflow and groundwater flow

duration from the start of direct runoff to peak flow.

duration that runoff is above the base flow

duration of water from farthest point in the watershed to reach outlet

lag time of the basin is the time between the center of mass of the runoff-producing rainfall to the peak rate of flow

rocky and impermeable

slightly permeable, bare

cultivated or covered with vegetation

cultivated absorbent soil

sandy soil

heavy forest