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STREAM FLOW DYNAMICS AND SOIL EROSION

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STREAM FLOW DYNAMICS AND SOIL EROSION

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LESSON 3.2

Created by

Grace Balahay
Grace Balahay
United States

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STREAM FLOW DYNAMICS AND SOIL EROSION
 

STREAM FLOW DYNAMICS AND SOIL EROSIONOnline version

LESSON 3.2

by 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.

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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.

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4

affects food sources and migration of fish amongst other wildlife

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5

Rough approximation of flow in a uniform and straight channel

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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.

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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

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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.

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9

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

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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.

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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.

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12

Determining the discharge using Manning’s Flow equations

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13

Equations that determine the discharge in slope-area method

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14

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

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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.

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16

contributions from the delayed interflow and groundwater runoff.

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17

contributions from surface runoff and quick interflow.

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18

analysis refers only to direct runoff.

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19

portion of the hydrograph, composed mostly of surface runoff.

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20

zone of the hydrograph around peak discharge.

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21

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

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22

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

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23

duration from the start of direct runoff to peak flow.

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24

duration that runoff is above the base flow

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25

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

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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

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27

rocky and impermeable

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28

slightly permeable, bare

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29

cultivated or covered with vegetation

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30

cultivated absorbent soil

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31

sandy soil

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32

heavy forest

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