B. Soil and Water Conservation Engineering Flashcards
Portion of the precipitation that makes its way toward streams, channels, lakes or oceans as surface or subsurface flow.
a. Drainage
b. Runoff
c. Flow
d. None of the above
b. Runoff
The time required for water to flow from the most remote (in time of flow) point of the area to the outlet once the soil has become saturated and minor depressions filled.
a. Time of concentration
b. Lag time
c. Time to peak
d. None of the above
a. Time of concentration
The only design of small farm reservoir that is suited to flat areas, where water is stored below the ground level and pumping is required to draw out water.
a. Dugout pond
b. Straight embankment
c. Shallow well
d. Reservoir
a. Dugout pond
In constructing SFR, the soil profile in the reservoir site must be analyzed at what depth?
a. 1.5 m
b. 2.0 m
c. 3.0 m
d. 1.0 m
a. 1.5 m
Small scale earth dam structure constructed across a narrow depression or valley to collect and store rainfall and runoff during rainy season for immediate and future use?
a. Small farm reservoir
b. Small water impounding project
c. Diversion dam
d. All of the above
b. Small water impounding project
The maximum dam height for a small farm reservoir (SFR)?
a. 3.0 m
b. 4.0 m
c. 5.0 m
d. 6.0 m
b. 4.0 m
The maximum dam height for a small water impounding project
a. 5.0 m
b. 10.0 m
c. 15.0 m
d. 20.0 m
c. 15.0 m
What is the maximum depth to be classified as shallow tube well?
a. 5.0 m
b. 10.0 m
c. 15.0 m
d. 20.0 m
c. 15.0 m
The volume of water stored in reservoir between the minimum water level and normal water level.
a. Active storage
b. Dead storage
c. Normal storage
d. Storage capacity
a. Active storage
The maximum elevation the water surface which can be attained by the dam or reservoir without flow in the spillway.
a. Normal storage elevation
b. Seepage line
c. Spillway
d. Storage capacity
a. Normal storage elevation
Graphical representation of the instantaneous runoff rate against time.
A. Hydrograph
C. Pearson hydrograph
B. Log-Normal Distribution hydrograph
D. Normal hydrograph
A. Hydrograph
It is the natural or synthetic hydrograph for one unit of direct runoff from the catchments in a specific unit of time:
A. Basic hydrograph
C. Design hydrograph
B. Unit hydrograph
D. Runoff hydrograph
B. Unit hydrograph
Run-off is produced when this property of the soil surface is exceeded:
A. Percolation rate
C. Infiltration capacity
B. Erodibility
D. Permeability
C. Infiltration capacity
In discharged measurement, the readings in the staff gage are useless without this:
A. Synthetic hydrograph
C. Unit hydrograph
B. Rating curve
D. Matching curve
B. Rating curve
On the weather map, lines representing points of equal pressure is called.
A. Isohyets
C. Contour lines
B. Isobars
D. None of these
B. Isobars
Which is not an advantage in using isohyetal method in determining average rainfall over an area?
A. It is subject to only slight errors in computation
C. It utilizes stations outside the basin
B. It is easy at a glance to see rainfall pattern
D. It is possible to account for topography
A. It is subject to only slight errors in computation
A plot of line of equal potential and paths of flow conveniently drawn so that the flow between any two adjacent streamlines is equal to the flow between any other two adjacent streamlines;
A. Contour lines
C. Isohyets
B. Flow net
D. Isobars
B. Flow net
A plot of line of equal elevation is;
A. Contour lines
C. Isohyets
B. Flow net
D. Isobars
A. Contour lines
A plot of line of equal rainfall is;
A. Contour lines
C. Isohyets
B. Flow net
D. Isobars
C. Isohyets
Term for solar radiation received at the earth’s surface.
A. Insolation
C. Radiation
B. Illuminance
D. Reflection
A. Insolation
Computer aided method wherein it averages estimated precipitation at all points of a superimposed grid.
A. Inverse Distance Ratio Method
C. Grid-Point Method
B. Isohyetal Method
D. Thiessen polygon Method
C. Grid-Point Method
Station locations and amounts of rainfall are plotted on a suitable map, and contours of equal precipitation (isohyets) are then drawn.
A. Inverse Distance Ratio Method
C. Grid-Point Method
B. Isohyetal Method
D. Thiessen polygon Method
B. Isohyetal Method
Location of the rain gauges are plotted on the map of the area and stations are connected by straight lines.
A. Inverse Distance Ratio Method
C. Grid-Point Method
B. Isohyetal Method
D. Thiessen polygon Method
D. Thiessen polygon Method
Time for surface and interflow to recede; duration of flooding.
A. Recession time
C. Base time
B. Surface time
D. Surface interflow time
A. Recession time
This property of run-off is used for flood forecasting and water quality analysis. It is the time where the flood flow is highest.
A. Recession time
C. Run-off time
B. Time to lag
D. Time to peak
D. Time to peak
Used for flood forecasting and water quality studies; watershed response time.
A. Surface time
C. Recession time
B. Time to peak
D. Peak recession time
B. Time to peak
It is the time required for water to flow from the most remote point of the water shed to the outlet.
A. Time of concentration
C. Runoff coefficient
B. Rainfall coefficient
D. Rational method
A. Time of concentration
In the Soil Conservation Service method (curve number method), if the curve number is 100, this indicates that:
A. Rainfall is equal to runoff
C. Rainfall is less than runoff
B. Runoff is zero
D. Rainfall is highly erosive
A. Rainfall is equal to runoff
The ratio of peak rate of runoff to the rainfall intensity is:
A. Time of concentration
C. Runoff coefficient
B. Rainfall coefficient
D. Rational method
C. Runoff coefficient
Same as interflow:
A. Surface runoff
C. Groundwater runoff
B. Subsurface runoff
D. Runoff volume
B. Subsurface runoff
Total water yield from a storm for a given watershed.
A. Surface runoff
C. Groundwater runoff
B. Subsurface runoff
D. Runoff volume
A. Surface runoff
That which travels over the ground surface and through the channels to reach the basin outlet.
A. Surface runoff
C. Groundwater runoff
B. Subsurface runoff
D. Runoff volume
A. Surface runoff
Surface runoff plus interflow.
A. Base flow
C. Groundwater runoff
B. Direct runoff
D. Peak flow
B. Direct runoff
Groundwater discharge into a stream due to deep percolation of the infiltrated water into groundwater aquifers.
A. Groundwater surface runoff
C. Groundwater runoff
B. Groundwater subsurface runoff
D. Groundwater runoff volume
C. Groundwater runoff
Advanced stage of rill erosion. Rills when neglected develop in size and become gullies.
A. Slip erosions
C. Stream bank erosion
B. Wind erosions
D. Gully erosion
D. Gully erosion
Detachment and transport of soil particles by concentrated flow of water creating channels larger and deeper than rills.
A. Interrill erosion
C. Stream channel erosion
B. Rill erosion
D. Gully erosion
D. Gully erosion
Combination of sheet and splash erosion.
A. Interrill erosion
C. Gully erosion
B. Rill erosion
D. Stream channel erosion
A. Interrill erosion
Removal of soil by water from small but well-defined channels when there is concentration of overland flow.
A. Interrill erosion
C. Gully erosion
B. Rill erosion
D. Stream channel erosion
D. Stream channel erosion
Consists of soil removal from stream banks or soil movement in the channel.
A. Interrill erosion
C. Gully erosion
B. Rill erosion
D. Stream channel erosion
D. Stream channel erosion
The type of erosion that takes place in small channels which cannot be obliterated by tillage operations is called:
A. Sheet erosion
C. Interrill erosion
B. Rill erosion
D. Gully erosion
D. Gully erosion
Soil detachment and transport resulting from the impact of water drops directly on soil particles or on thin water surfaces.
A. Interrill erosion
C. Splash / raindrop erosion
B. Rill erosion
D. Stream channel erosion
C. Splash / raindrop erosion
Landslides and slips due to saturation of steep hills and slopes.
A. Slip erosions
C. Coastal erosions
B. Wind erosions
D. Stream bank erosion
A. Slip erosions
Erosion caused by wave action on the seashore.
A. Slip erosions
C. Coastal erosions
B. Wind erosions
D. Stream bank erosion
C. Coastal erosions
Caused by high velocity winds moving over barren land surfaces.
A. Slip erosions
C. Coastal erosions
B. Wind erosions
D. Stream bank erosion
B. Wind erosions
Primarily caused by raindrop.
A. Slip erosions
C. Coastal erosions
B. Wind erosions
D. Splash/Raindrop erosion
D. Splash/Raindrop erosion
The type of erosion that takes place in small channels which cannot be obliterated by tillage operations is called.
A. Sheet
C. Interrill
B. Rill
D. Gully
D. Gully
It is type of erosion where small channels are formed on the surface of the soil.
A. Sheet
C. Splash
B. Rill
D. Gully
B. Rill
Finger-like rills appear on the soil surface.
A. Gully erosion
C. Sheet erosions
B. Rill erosions
D. Interill erosions
B. Rill erosions
Detachment and transport of soil by concentrated flow of water creating shallow rills or furrows.
A. Gully erosion
C. Stream channel erosion
B. Rill erosions
D. Interill erosions
B. Rill erosions
The USLE is a method of computing soil erosion. What type of soil erosion does it estimate?
A. Sheet erosion only
C. Sheet, rill and gully erosion
B. Sheet and rill erosion only
D. All types of erosion
B. Sheet and rill erosion only
Uniform removal of soil in thin layers from sloping land resulting from over land flow:
A. Stream channel erosion
C. Gully erosion
B. Rill erosion
D. Sheet erosion
D. Sheet erosion
A thin film of soil layer detached and transported by water flowing on the land surface:
A. Slip erosions
C. Splash/Raindrop erosion
B. Wind erosions
D. Sheet erosions
D. Sheet erosions
How does a gully develop?
i. Stabilization stage
ii. Channel erosion by downward scour of the topsoil
iii. Healing stage
iv. Upward movement of gully head and enlargement of the gully width
A. ii, iv, i, iii
C. ii, iii, iv, i
B. iv, ii, iii, i
D. ii, iv, iii, i
D. ii, iv, iii, i
Type of flow wherein the depth of flow in a prismatic channel is constant at any point in the channel.
A. Laminar flow
C. Steady flow
B. Uniform flow
D. Critical flow
C. Steady flow
Type of flow wherein the discharge or flow in a prismatic channel is constant with respect to time.
A. Laminar flow
C. Steady flow
B. Uniform flow
D. Critical flow
C. Steady flow
Type of open channel flow in which the flow depth does not change with time is:
A. Uniform flow
C. Steady flow
B. Critical flow
D. Unsteady flow
C. Steady flow
Discharge is constant with respect to time.
A. Spatially variable flow
C. Steady flow
B. Turbulent flow
D. Laminar flow
C. Steady flow
Same as groundwater runoff.
A. Base flow
C. Groundwater runoff
B. Subsurface runoff
D. Runoff volume
A. Base flow
When is the best/recommended time to sample sediment load in the stream?
A. Base flow
C. Peak flow
B. Intermittent flow
D. Perennial flow
C. Peak flow
Used to determine the magnitude of floods and a valuable consideration in the design of structures.
A. Peak flow
C. Base flow
B. Subsurface runoff
D. Groundwater runoff
A. Peak flow
If the depth changes abruptly over a comparatively short distance such as in a hydraulic jump.
A. Turbulent flow
C. Rapidly varied flow
B. Gradually varied flow
D. Unsteady flow
C. Rapidly varied flow
A hydraulic jump is a classic example of this type of flow:
A. Unsteady flow
C. Rapidly Varied flow
B. Gradually varied flow
D. Critical flow
C. Rapidly Varied flow