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Thapar University 2006 B.Tech Civil Engineering Hydrology And Ground Water - Question Paper

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Thapar Institute of Engineering & Technology
C.E. (2nd Year)
Final Term exam
CE004 (Hydrology And Ground Water)

TIME: 3 Hours

DEPARTMENT OF CIVIL ENGINEERING

CE-004 HYDROLOGY AND GROUND WATER END SEMESTER EXAMINATION; December 6,2006 SESSION 2006-2007

M. MARKS: 100

Note: Assume missing data suitably, if required.

Ql:

(a)    Explain how rain falling on earth is disposed off.

(b)    The following information is available from an isohyetal map of a catchment:

Rain gauge station

A

B

C

D

E

F

G

H

Annual rainfall (cm)

120

95

96

60

65

70

45

21

How many additional rainguage stations will be required if the desired limit of error in the mean value of rainfall is not to exceed 10 cm?

(c) The infiltration characteristics of an area was studied and the following data was obtained:

Time (h)

0.25

0.5

0.75

1.0

1.25

1.5

1.75

2.0

2.25

Infiltration (cm/h)

6.5

3.4

2.3

1.8

1.4

1.28

1.0

1.0

1.0

Determine equation of infiltration capacity curve.

(5, 7,8)

Q2:

(a)    A 6 h unit hydrograph for a catchment of area 1000 km2 can be approximated as a triangle with a base of 66 h. If the peak of unit hydrograph occurs after 12 h from the start, calculate the flood hydrograph due to a storm of rainfall 3.2 cm occurring during first 6 h and 5.2 cm during successive second 6 h duration.

Assume infiltration index as 0.2 cm/h and a constant base flow of 30 cumec

(b)    Characteristics of two catchments A and B measured from a map are given below:

Item

Catchment A

Catchment B

Lca

76 km

52 km

L

148 km

106 km

A

2718 km

1400 km-1

For a 6 h unit hydrograph in catchment A, the peak discharge is at 37 h from the start of the rainfall excess and its value is 200 m3/s. Assuming catchments A and B are to be meteorologically similar, determine the elements of 6 h SUH for catchment B by using Snyders method.

(10,10)

Q3:

(a)    What do you understand by flood routing and what is its importance?

(b)    The inflow and outflow hydrographs of a particular reach of a channel are given below.

Time (h)

0

6

12

18

24

30

36

42

48

54

60

66

72

Inflow (mJ/s)

35

135

440

670

685

535

385

235

140

95

60

42

35

Outflow (nrVs)

35

57

200

455

612

617

510

375

246

158

102

68

56

Determine Muskingum coefficients k and x for this reach.

(6,14)

Q4:

(a)    Differentiate between confined and unconfined aquifers

(b)    Rainfall falls at the rate of 10 mm/hr on a strip of land 1 km wide lying between two parallel canals. It is underlain by a horizontal impervious stratum. The water depth above this stratum in the two canals are 12 m and 10 m. Assuming a permeability of 12 m/day with vertical boundaries and all the rainfall infiltrates into the soil, compute the discharge per meter length into each canal. Also, determine the equation of the water table profile and the location of the water table divide. Derive the formulae.

(5,15)

Q5:

(a)    What is a mass curve and how will you determine the storage capacity of a reservoir by using the same?

(b)    Discuss the economics of a flood control project.

(c)    Discuss rational method of determing the peak discharge.

(d)    What is a reservoir? Discuss in brief the different types of reservoirs.

(4x5)







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