Term
The portion of rainfall that runs off a catchment surface during a storm is generally called? |
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Definition
Rainfall excess or runoff |
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Term
More runoff is expected to occur from pervious surfaces compared to impervious surfaces:
a. True
b. False |
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Definition
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Term
The distance that sheet flow is expected to occur within an urban area is expected to be within the range of?
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|
Definition
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Term
The stormwater route can be best described as? |
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Definition
The flowpath that runoff will travel from one part of the catchment to the outlet |
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Term
The stormwater discharge from a catchment is dependent on the size of the catchment:
a. True
b. False |
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Definition
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Term
The temporary storage of surface water and subsequent release downstream at a slower rate than the inflow is termed? |
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Definition
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Term
A hydrograph is a plot of? |
|
Definition
A plot of a flow property against time |
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Term
The falling limb of a discharge hydrograph:
a. Always occurs after the peak discharge
b. Is also called the hydrograph recession
c. Includes both quickflow and baseflow components
d. All of the above |
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Definition
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Term
To determine the combined discharge when two creek tributaries join at a confluence, their discharge hydrograph values should be? |
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Definition
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Term
The main processes of hydrograph routing involves:
a. Attenuation of the flow peak
b. Translation of the flow peak
c. Both of the above
d. None of the above |
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Definition
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Term
500 kL of water is equivalent to:
a. 50,000 L
b. 0.5 GL
c. 0.5 ML
d. 1 m3
e. None of the above |
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Definition
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Term
Conservation of Mass is an important concept in water balance in which _______, _______ and _______ are taken into account? |
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Definition
The inflow, outflow and changes in storage volume |
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Term
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Definition
a measure of flow, in metres cubed per second
(m^3 / s) |
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Term
Describe the term Dendritic |
|
Definition
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|
Term
Describe the term, Retention Storage |
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Definition
It is a store that must be filled before the flow can proceed onwards |
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Term
Describe the term 'Quickflow' |
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Definition
Water that is rapidly delivered in response to rainfall. It is associated with surface runoff |
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Term
Describe the term 'Baseflow' |
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Definition
This is water that slowly reaches the hydrograph location, usually through the result of groundwater contributions to the creek flow. |
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Term
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Definition
A creek system that is sustained by baseflow |
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Term
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Definition
A creek system that has little or no baseflow. (only flowing during a rain event) |
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Term
An instrument that measures rainfall intensity is called a: |
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Definition
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Term
The plot of rainfall intensity against time is known as a hydrograph:
a. True
b. False |
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Definition
b. False.
it is a Hyetograph |
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Term
If rainfall of intensity 15 mm/h for 10 minutes is immediately followed by rainfall of intensity 18 mm/h for the next 15 minutes, the total depth of rainfall is (in mm): |
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Definition
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Term
Rainfall of intensity 15 mm/h for 10 minutes is immediately followed by rainfall of intensity 18 mm/h for the next 15 minutes. What is the average rainfall intensity for the event: |
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Definition
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Term
The Thiessen Polygonal Method is a means of estimating: |
|
Definition
Areal rainfall from point rainfall |
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Term
In terms of flow measurement in rivers and streams, the term stage means: |
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Definition
The water elevation at a particular point along the river |
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Term
The plot of river stage against discharge at a streamgauge is known as a: |
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Definition
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Term
The total volume of surface runoff can be estimated from: |
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Definition
The area between the total runoff hydrograph and the baseflow hydrograph |
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Term
Daily-read rain gauges provide data on: |
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Definition
The rainfall depth that occurred in the previous 24 hours to 9am |
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Term
A rainfall of 12mm during a time period of 6 minutes is equivalent to a rainfall intensity of: |
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Definition
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Term
Contours of equal rainfall plotted on a catchment plan are known as: |
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Definition
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Term
The evapotranspiration from a vegetated surface is expected to be less than pan evaporation:
a. True
b. False |
|
Definition
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Term
The annual series comprises? |
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Definition
The maximum instantaneous discharge recorded in every year of record |
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Term
The annual exceedance probability (AEP) is defined as? |
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Definition
The probability that the flood will be equalled or exceeded in any one year |
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Term
The average recourance interval (ARI) is? |
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Definition
The average period between exceedances of the given discharge |
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Term
An appropriate design standard for the spillway of a major storage might be the flood event corresponding to an ARI of:
a. 1 year
b. 5 years
c. 10 years
d. More than 500 years
e. None of these answers |
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Definition
e. None of these answers
typical would be 10000 to 1000000 years |
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Term
If the peak probability of occurrence is less than the mean, then the probability distribution is said to be? |
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Definition
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Term
The Normal probability distribution is? |
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Definition
Symmetrical around the mean |
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Term
What is the risk of failure of at least one 1 in 20 AEP flood occurring within a 6 year time period? |
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Definition
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Term
A 200 year ARI flood has en equivalent AEP of |
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Definition
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Term
The plotting position used in Annual flood frequency is? |
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Definition
An estimate of the AEP of each of the Annual peak discharges |
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Term
The moments of the LP3 distribution are? |
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Definition
The Mean, Standard Deviation and the Skew |
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Term
The Partial Series is best suited for the determination of Design Floods |
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Definition
Equal to 10 year ARI or less |
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Term
The number of flood peaks above the threshold is used to calculate the plotting position in a Partial Series analysis:
a. True
b. False |
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Definition
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|
Term
Rainfall intensity increases with ARI
a. True
b. False |
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Definition
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|
Term
Rainfall intensity increases with storm duration
a. True
b. False |
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Definition
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Term
50I12 is the:
a. 50 year ARI rainfall for the 12 hour duration design storm
b. 12 year ARI rainfall for the 50 hour duration design storm
c. 50% AEP rainfall for the 12 hour duration design storm
d. 50 year ARI rainfall intensity for the 12 hour duration design storm
e. None of these answers |
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Definition
d. 50 year ARI rainfall intensity for the 12 hour duration design storm |
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Term
Design IFD rainfalls are used for:
a. Flood frequency analysis
b. Rainfall-based design flood estimation
c. Spatial interpolation of point rainfalls
d. Plotting histograms
e. None of these answers |
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Definition
b. Rainfall-based design flood estimation |
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Term
Standard durations of IFD rainfalls range from 5 minutes to 72 hours.
a. True
b. False |
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Definition
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Term
The standard ARIs of design rainfalls are 1, 2, 5, 10, 50 and 100 years.
a. True
b. False |
|
Definition
b. False
20 year ARI is also a standard:
1, 2, 5, 10, 20, 50 and 100 years
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Term
Design temporal patterns for IFD rainfalls are used to: |
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Definition
Provide estimates for design purposes of how the rainfall intensity varies with time for a given duration |
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Term
For a given catchment area, the areal reduction factor increases with storm duration.
a. True
b. False |
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Definition
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Term
The total rainfall (in mm) for a design storm event corresponding to an 100I6 of 35 mm/h is:
a. 3500
b. 3.5
c. 210
d. 35
e. None of these answers |
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Definition
c. 210
35mm/hr x 6hr = 210mm |
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Term
The probabilistic Rational method is a rainfall-based procedure to estimate design discharges.
a. True
b. False |
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Definition
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Term
The probabilistic Rational Method uses average areal rainfalls for the catchment.
a. True
b. False |
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Definition
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Term
The probabilistic Rational Method used for eastern New South Wales is generally only applicable to rural catchments not exceeding a size (in km2 ):
a. 25
b. 100
c. 1000
d. 250 |
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Definition
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Term
The runoff coefficient for the probabilistic Rational Method for rural catchments is always greater than one:
a. True
b. False |
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Definition
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Term
The critical storm duration used to determine the maximum design discharge when using the probabilistic Rational Method is:
a. Always greater than the time of concentration of the catchment
b. Equals the time of concentration of the catchment
c. Not dependent on the catchment size
d. Calculated based on a flood frequency analysis |
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Definition
b. Equals the time of concentration of the catchment |
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Term
The estimated time of concentration for a rural Victorian catchment with an area of 210 km2 is:
a. 5.8 hours
b. 58 minutes
c. 158 minutes
d. 58 hours |
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Definition
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Term
The appropriate conversion factor to use in the Rational Method is 0.278 when the area is in km2 and the discharge is in cumecs.
a. True
b. False |
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Definition
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Term
The frequency factor for the probabilistic Rational Method is always less than one.
a. True
b. False |
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Definition
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Term
For any given rainfall excess which is temporally and spatially uniform over a catchment, the greatest peak discharge at the outlet will occur when the duration of rainfall excess is:
a. Less than the time of concentration
b. Equal or greater than the time of concentration
c. Greater than the rainfall duration
d. Less than the travel time for the furthest isochrones |
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Definition
b. Equal or greater than the time of concentration |
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Term
The time of concentration may be defined as the time taken for:
a. All rainfall to be converted to rainfall excess
b. Runoff to appear at the outlet from the commencement of rainfall
c. All parts of the catchment to contribute to runoff at the outlet from the commencement of rainfall
d. All parts of the catchment to contribute to runoff at the outlet from the commencement of rainfall excess |
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Definition
d. All parts of the catchment to contribute to runoff at the outlet from the commencement of rainfall excess |
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Term
In runoff routing, it is generally preferable to divide the catchment into at least 5 smaller subcatchments.
a. True
b. False |
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Definition
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Term
In general terms, routing is the process whereby:
a. Rainfall is converted to rainfall excess
b. The course of the river changes over time
c. The hydrograph changes as it progresses through storage
d. Runoff is lost due to evaporation
e. None of these answers |
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Definition
c. The hydrograph changes as it progresses through storage |
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Term
Storage routing can occur within:
a. The subcatchment as runoff moves across the surface
b. Flow channels, both natural and man-made
c. Reservoirs such as dams and ponds
d. All of these answers |
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Definition
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Term
A discharge hydrograph is:
a. A plot of channel discharge against channel flow depth
b. A plot of instantaneous discharge against time
c. Not dependent on the catchment size
d. A plot of discharge against rainfall intensity
e. None of these answers |
|
Definition
b. A plot of instantaneous discharge against time |
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Term
To determine the combined hydrograph at a creek junction, the tributary discharge hydrographs should be:
a. Numerically added together
b. Multiplied by the ratio of their catchments areas and then added together
c. Compared, and the hydrograph with the largest discharges used as the combined hydrograph
d. Multiplied by the ratio of their discharge peaks and then added together
e. None of these answers |
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Definition
a. Numerically added together |
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Term
As a flood wave travels from some upstream point to some downstream point, the peak discharge decreases due to storage. The reduction in peak discharge is known specifically as:
a. Routing
b. Lag
c. Attenuation
d. Delay
e. None of these answers |
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Definition
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Term
A flood wave travels from some upstream point to some downstream point. If there is no net change in retention storage between the two points then the:
a. Peak inflow lags the peak outflow
b. Peak outflow is greater than the peak inflow
c. Total volume of inflow equals the total volume of outflow
d. Total volume of inflow is less than the total volume of outflow
e. None of these answers |
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Definition
c. Total volume of inflow equals the total volume of outflow |
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Term
Loss models are used to estimate:
a. Peak outflow from peak inflow
b. Hydrograph lag
c. Hydrograph attenuation
d. Rainfall excess from rainfall
e. None of these answers |
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Definition
d. Rainfall excess from rainfall |
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Term
An initial-proportional loss model includes:
a. An initial depth of loss followed by a continuing fixed rate of loss
b. An initial depth of loss followed by a continuing rate of loss at a fixed fraction of the rainfall rate
c. An initial rate of loss followed by a continuing rate of loss at a fixed fraction of the rainfall rate
d. An initial depth of loss followed by a continuing fixed depth of loss
e. None of these answers |
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Definition
b. An initial depth of loss followed by a continuing rate of loss at a fixed fraction of the rainfall rate |
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Term
A rainfall hyetograph comprises values of 12, 15 and 18 mm/h, each over a time interval of 20 minutes. The total depth of rainfall excess using 10mm initial loss and 2 mm/h continuing loss is (in mm):
a. 45
b. 35
c. 5
d. 16
e. None of these answers |
|
Definition
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Term
If, following the passage of a flood wave through a dam, the volume of storage in the dam is the same before and after the event, then:
a. The inflow discharge was greater than the outflow discharge
b. The inflow discharge was equal to the outflow discharge
c. The total volume of inflow was equal to the total volume of outflow
d. The total volume of inflow was greater than the total volume of outflow
e. None of these answers |
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Definition
c. The total volume of inflow was equal to the total volume of outflow |
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Term
In reservoir routing, the outflow hydrograph:
a. Has a greater peak than the inflow hydrograph
b. Has an earlier peak that the inflow hydrograph
c. Intersects the inflow hydrograph at the time of the peak inflow
d. Intersects the inflow hydrograph at the time of the peak outflow
e. None of these answers |
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Definition
d. Intersects the inflow hydrograph at the time of the peak outflow |
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Term
In reservoir routing, the volume in storage:
a. Reaches a maximum at the time of peak of the outflow hydrograph
b. Reaches a minimum at the time of peak of the outflow hydrograph
c. Reaches a minimum at the time of peak of the inflow hydrograph
d. Reaches a maximum at the time of peak of the inflow hydrograph
e. None of these answers |
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Definition
a. Reaches a maximum at the time of peak of the outflow hydrograph |
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Term
If the weighting factor x in the Muskingum channel routing method is equal to zero, then:
a. Wedge storage is made up of an equal weighting of inflow and outflow
b. Wedge storage is greater than zero
c. Wedge storage is equal to zero
d. Total storage depends only on the inflow
e. None of these answers |
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Definition
c. Wedge storage is equal to zero |
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Term
The weighting factor x in the Muskingum channel routing method generally lies in the range between 0 and 0.5:
a. True
b. False |
|
Definition
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Term
The time constant K in the Muskingum channel routing method is a measure of:
a. The volume in storage along the reach at any particular time
b. The time taken for a flood wave to travel the length of the reach
c. The timestep used in computations
d. The time taken for all storage to drain out of the reach
e. None of these answers |
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Definition
b. The time taken for a flood wave to travel the length of the reach |
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|
Term
In order of increasing size and flows, urban drainage includes the following sequence of systems:
a. Trunk drainage, street drainage and roof & property drainage
b. Roof & property drainage, street drainage and trunk drainage
c. Roof & property drainage, trunk drainage and street drainage
d. Street drainage, roof & property drainage and trunk drainage
e. None of these answers |
|
Definition
b. Roof & property drainage, street drainage and trunk drainage |
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Term
Inter allotment drainage is:
a. Required if the allotment slopes away from the road
b. Designed to convey roof drainage
c. Often located within a drainage easement
d. All of these answers |
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Definition
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Term
Which of the following is likely to be a design standard for the Minor system of an urban drainage scheme:
a. 2 year ARI
b. 33 year ARI
c. 100 year ARI
d. Probable maximum flood
e. None of these answers |
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Definition
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Term
In the Major design storm, a flow depth of 0.5m and a flow velocity of 2.0 m/s at the road gutter would be considered to be acceptable:
a. True
b. False |
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Definition
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Term
The time of concentration for overland flow in urban drainage design is determined using:
a. Friend’s equation
b. Weeks equation
c. Pilgrim and McDermott formula
d. Rational equation
e. None of these answers |
|
Definition
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Term
Standard inlet times are commonly used to:
a. Estimate the flow travel time along the road gutter
b. Estimate the total flow travel time to the pit
c. Estimate the time to drain the road pit
d. Estimate the road gutter velocity
e. None of these answers |
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Definition
Estimate the total flow travel time to the pit |
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Term
The minimum time of concentration used in urban drainage design is generally:
a. 2 minutes
b. 5 minutes
c. 1 minute
d. 20 minutes
e. None of these answers |
|
Definition
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Term
Pipe discharges should not be taken into account in analysing the capacity of an urban drainage system under the Major design storm:
a. True
b. False |
|
Definition
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Term
What is the runoff volume (in ML) corresponding to 25mm runoff from a 20 km2 catchment:
a. 5
b. 50
c. 500
d. 5000
e. None of these answers |
|
Definition
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Term
What is the volumetric runoff coefficient corresponding to a storm when 55mm runoff occurred in response to 85 mm rainfall:
a. 0.65
b. 0.35
c. 1.0
d. 0.065
e. None of these answers |
|
Definition
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Term
AWBM , E2 and SYMHYD are all examples of:
a. Runoff routing models
b. Runoff –rainfall models
c. Rainfall excess routing models
d. Rainfall- runoff models
e. All of these answers |
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Definition
d. Rainfall- runoff models |
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Term
The bucket capacities in AWBM should always equal to one:
a. True
b. False |
|
Definition
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|
Term
To estimate runoff, the AWBM requires as daily inputs:
a. Evapotranspiration
b. Pan evaporation
c. Crop evaporation
d. Potential evaporation
e. None of these answers |
|
Definition
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Term
The slope of the rainfall-runoff relationship in AWBM is 1:1 when:
a. All three area fractions are contributing to runoff
b. Only area A1 is contributing
c. The initial loss is zero
d. Rainfall exceeds evapotranspiration
e. None of these answers |
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Definition
a. All three area fractions are contributing to runoff |
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|
Term
Storage reliability can be defined as:
a. The probability that the storage will be empty
b. The probability that the storage will not be able to supply a demand
c. The probability that the storage will overflow
d. The probability that the storage will be able to supply a demand
e. None of these answers |
|
Definition
d. The probability that the storage will be able to supply a demand |
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|
Term
Draft can be defined as:
a. The average release volume from a dam to meet the required water demand
b. The stored water in the dam unavailable to be used
c. Evaporation loss from the dam surface due to wind
d. The difference between dam inflow and outflow
e. None of these answers |
|
Definition
a. The average release volume from a dam to meet the required water demand |
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Term
In the zone of saturation of a geological formation, the water content is:
a. Less than the field capacity
b. Less than the wilting point
c. Equal to the porosity of the formation
d. Less than the amount of water held by hygroscopic action
e. None of these answers |
|
Definition
c. Equal to the porosity of the formation |
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|
Term
In the capillary zone of a geological formation, the water content is:
a. Equal to the plant available water
b. Increasing with depth
c. Decreasing with depth
d. Independent of porosity
e. None of these answers |
|
Definition
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|
Term
In groundwater hydrology, specific yield is defined as the:
a. Head loss per unit length of aquifer
b. Volume of water released from an unconfined aquifer per unit surface area of aquifer per unit drop in level of the water table
c. Volume of water released from a confined aquifer per unit surface area per unit drop in piezometric head
d. Product of the hydraulic conductivity and the cross sectional area of the aquifer
e. None of these answers |
|
Definition
b. Volume of water released from an unconfined aquifer per unit surface area of aquifer per unit drop in level of the water table |
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Term
Darcy’s Law for flow through porous media states that:
a. Discharge is inversely proportional to hydraulic gradient
b. Hydraulic conductivity is proportional to hydraulic gradient
c. Discharge is proportional to the product of hydraulic gradient and cross sectional area of flow
d. Piezometric head is proportional to hydraulic gradient
e. None of these answers |
|
Definition
c. Discharge is proportional to the product of hydraulic gradient and cross sectional area of flow |
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|
Term
In groundwater hydrology, transmissivity may be defined as:
a. Sum of hydraulic conductivity and saturated aquifer thickness
b. Flow rate per unit width of aquifer
c. Flow rate per unit width of aquifer divided by hydraulic gradient
d. Product of storativity and hydraulic gradient
e. None of these answers |
|
Definition
c. Flow rate per unit width of aquifer divided by hydraulic gradient |
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|
Term
A confined aquifer is a geological formation which:
a. Contains only very small quantities of water
b. Is better known as an aquitard because it allows vertical movement of water into a leaky aquifer
c. Holds but cannot transmit any significant quantity of water
d. Always has a free water table
e. None of these answers |
|
Definition
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|
Term
A subartesian bore is one which:
a. Penetrates an unconfined aquifer and flows to the surface
b. Penetrates an unconfined aquifer and does not flow to the surface
c. Penetrates a confined aquifer and does not flow to the surface
d. Penetrates a confined aquifer and flows to the surface
e. None of these answers |
|
Definition
c. Penetrates a confined aquifer and does not flow to the surface |
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|
Term
In groundwater hydrology, the term cone of depression means:
a. The three dimensional conic shape formed by the piezometric surface during an equilibrium pump test
b. The aura surrounding students at exam time
c. The shape of the fresh/salt water interface to coastal aquifers
d. An instrument used to measure drawdown in a pump test
e. None of these answers |
|
Definition
a. The three dimensional conic shape formed by the piezometric surface during an equilibrium pump test |
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Term
For an equilibrium pump test on an unconfined aquifer:
a. The cross section area of flow is a constant
b. Hydraulic conductivity changes with radial distance from the pumped bore
c. The specific yield may be calculated from the observation bore measurements
d. Best results are achieved by positioning the observation bores as close as possible to the pumped bore
e. None of these answers |
|
Definition
|
|