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Discharge Velocity is obtained by Dividing the Total Discharge by the total cross Sectional Area , Where Total cross sectional area Consists of void+solid. In contrast .. Seepage Velocity is defined as the total discharge by the Area of voids only. So Seepage velocity always greater than Discharge Velocity.

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Seepage velocity is the rate at which water moves through soil or rock, typically due to a pressure gradient. Discharge velocity refers to the flow velocity of water in a channel or conduit, such as a river or pipe. Seepage velocity is generally slower than discharge velocity due to the porous nature of the material through which water is moving.

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Q: Seepage velocity and discharge velocity
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What is difference between discharge velocity and seepage velocity?

Discharge velocity refers to the rate at which water flows through a porous medium, such as soil or rock. Seepage velocity, on the other hand, represents the average velocity of water moving through the interconnected void spaces in the porous medium. While discharge velocity focuses on the overall flow rate, seepage velocity gives a more detailed view of how water moves within the porous medium.


What is the relationship between the carrying capacity of a stream and it's discharge and velocity?

The carrying capacity of a stream is influenced by its discharge and velocity. A higher discharge and velocity typically allow a stream to transport larger sediments and materials downstream, increasing its carrying capacity. Conversely, lower discharge and velocity may limit the stream's ability to carry sediment and materials.


What is the relationship between the carrying capacity of a stream and its discharge and velocity?

The carrying capacity of a stream is influenced by its discharge and velocity. Higher discharge and faster velocity can increase the stream's ability to transport sediment and debris, thus raising its carrying capacity. Conversely, lower discharge and slower velocity may result in a reduced carrying capacity as the stream has less energy to move material.


What happens to discharge and velocity near base level?

As an Alluvial stream stream approaches its base level, the discharge decreases, causing a reduction in velocity. This reduction in velocity leads to sediment deposition and the formation of a delta near the base level.


What is discharge and how does it affect velocity?

Discharge is the volume of water flowing in a river at a certain point over a specific period of time, usually measured in cubic meters per second. It directly affects velocity in rivers because as discharge increases, the amount of water flowing through the river also increases, leading to higher velocity. Conversely, lower discharge results in slower velocities.