*Hi,*

*Here are few statements from Hydrology which has made their place in GATE Civil Engineering(CE). The bold letter represents the answer which are absent in actual question.*

- A linear reservoir is one in which storage varies linearly with outflow rate.
- When there is an increase in the atmospheric pressure, the water level in a well penetrating in a confined aquifer does not undergo any change.
- During a 6-hour storm, rainfall intensity was 0.8 cm/hour on a catchment of area 8.6 km^2. The measured runoff volume during this period was 2,56,000 m^3. The total rainfall that was lost due to infiltration, evaporation, and transpiration (in cm/hour) is 0.304.
- Vertical hydraulic conductivity of the top soil at certain is 0.2 cm/hr. A storm of intensity 0.5 cm/hr occurs over the soil for an indefinite period. Assuming surface drainage to be adequate, infiltration rate after the storm has lasted for a very long time, shall be 0.2 cm/hr.
- While applying Rational formula for computing design discharge, the rainfall duration is stipulated as the time of concentration because this leads to the largest possible rainfall intensity.
- The plan area of a reservoir is 1 km^2. Water level in the reservoir is observed to decline by 20 cm in a certain period. During this period, the reservoir receives a surface inflow of 10 hectares-meters, and 20 hectares-meters are abstracted from the reservoir for irrigation and power. The pan evaporation and rainfall recorded during the same period at a near by meteorological station are 12 cm and 3 cm respectively. The calibrated pan factor is 0.7. The seepage loss from the reservoir during this period in hectare-meters is 4.6.

to be contd...

- Get link
- Other Apps

- Get link
- Other Apps

- Get link
- Other Apps

All the engineering fluids can be classified into two broad classes and then further sub-classes as follows:

(1) Newtonian fluids

(2) Non- Newtonian Fluids

**Newtonian Fluids: **These are the fluids which follow the Newton's law of viscosity. So shear stress of the fluids is directly proportional to the the velocity gradient, so it varies linearly with it. Newtonian fluids have constant viscosity which does not depend upon the stress. Sometimes it may vary under some specific conditions when the velocity gradient changes with the layer to layer.

**Non- Newtonian Fluids: **These fluids exhibit non-Newtonian characteristics, i.e. shear stress is not linearly dependent upon the velocity gradient, so doesn't follow the Newton's law of viscosity.

*T = A.(du/dy)^n + B ; *Where A and B are constants which depend upon type of fluid and conditions imposed on the flow. Value of n is 1 and of B is 0 for the Newtonian fluids. n is also known as power index, and depending upon its value non-Newto…

(1) Newtonian fluids

(2) Non- Newtonian Fluids

- Get link
- Other Apps

Hello,

Here is a brief comparison of Kennedy's theory and Lacey's theory for the design of channels for canal etc.

The concept of silt transportation is same in both the cases, both agree that the silt is carried by the vertical eddies generated due to friction of the flowing water against rough surface of canal. Kennedy considered a trapezoidal channel section and, therefore, he neglected eddies generated from the sides. For this reason, Kennedy's critical velocity formula was derived only in terms of depth of flow(y). Lacey considered that an irrigation channel achieves a cup-shaped section(semi-ellipse) and that entire wetted perimeter of the channel contributes to the generation of silt supporting eddies. He, thus, used hydraulic mean radius(R) as a variable in his regime velocity formulas instead of depth(y).Kennedy stated all the channels to be in state of regime provided they did not silt or scour. But Lacey differentiated between two regime conditions, i.e. initia…

Here is a brief comparison of Kennedy's theory and Lacey's theory for the design of channels for canal etc.

The concept of silt transportation is same in both the cases, both agree that the silt is carried by the vertical eddies generated due to friction of the flowing water against rough surface of canal. Kennedy considered a trapezoidal channel section and, therefore, he neglected eddies generated from the sides. For this reason, Kennedy's critical velocity formula was derived only in terms of depth of flow(y). Lacey considered that an irrigation channel achieves a cup-shaped section(semi-ellipse) and that entire wetted perimeter of the channel contributes to the generation of silt supporting eddies. He, thus, used hydraulic mean radius(R) as a variable in his regime velocity formulas instead of depth(y).Kennedy stated all the channels to be in state of regime provided they did not silt or scour. But Lacey differentiated between two regime conditions, i.e. initia…

- Get link
- Other Apps

## Comments

## Post a Comment