1. Draw the different components of stream flow hydrograph. What are the limitations of unit hydrograph?

Structural Analysis
6th Edition
ISBN:9781337630931
Author:KASSIMALI, Aslam.
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Chapter2: Loads On Structures
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1. Draw the different components of stream flow
hydrograph. What are the limitations of unit
hydrograph?
2 A 24 hour storm occurred over a catchment of
2
1.5 km area and the total rainfall observed was
10 cm. An infiltration capacity curve prepared
had the initial infiltration capacity of 1 cm/hr and
attained a constant value of 0.3 cm/hr after 15
hours of rainfall with a Horton's constant k =
5/hr. An evaporation pan installed in the
catchment indicated a decrease of 0.5 cm in the
water level (after allowing for rainfall) during 24
hours of its operation. Other losses were found to
be negligible. Determine the runoff from the
catchment area. Assume a pan coefficient of 0.65.
3. Route the inflow hydrograph using
Muskingum method; hr, = 0.2, = 0.65 hrs.
Time
01 2 3 4 5 6 7 8 9 10 11 1213
(hr)
Inflow 08811013322326523518015513211198550
(cumec)
4. What are the standard rain-gauge density for
different land topographical conditions? Briefly
describe the isohyet method for precipitation
measurement.
5. What is remote sensing? What are the
common characteristics of water resources data?
Transcribed Image Text:1. Draw the different components of stream flow hydrograph. What are the limitations of unit hydrograph? 2 A 24 hour storm occurred over a catchment of 2 1.5 km area and the total rainfall observed was 10 cm. An infiltration capacity curve prepared had the initial infiltration capacity of 1 cm/hr and attained a constant value of 0.3 cm/hr after 15 hours of rainfall with a Horton's constant k = 5/hr. An evaporation pan installed in the catchment indicated a decrease of 0.5 cm in the water level (after allowing for rainfall) during 24 hours of its operation. Other losses were found to be negligible. Determine the runoff from the catchment area. Assume a pan coefficient of 0.65. 3. Route the inflow hydrograph using Muskingum method; hr, = 0.2, = 0.65 hrs. Time 01 2 3 4 5 6 7 8 9 10 11 1213 (hr) Inflow 08811013322326523518015513211198550 (cumec) 4. What are the standard rain-gauge density for different land topographical conditions? Briefly describe the isohyet method for precipitation measurement. 5. What is remote sensing? What are the common characteristics of water resources data?
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