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.
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.
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.
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.
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.
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.
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.
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.
could it calculate by short thumb rule i.e seepage = (0.01xwetted ares (sq.ft))/1.75
When the discharge of a stream increases, so does it's velocity. When it decreases, so does the velocity.
The discharge of a liquid from a surface, such as pores or incisions, is known as seepage. Seepage can occur naturally through porous materials like soil, rock, or concrete, as well as through engineered structures like dams or retaining walls. It is important to manage seepage to prevent erosion, instability, or damage to surrounding areas.
When a stream's discharge increases, erosive energy increases.
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.
i think it is width X depth X velocity=discharge ?
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.
it is the velocity (V) divided by the retardation of the contaminant. The velocity, V is different from the regular velocity (which is Discharge/Area). V = regular velocity/porosity
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.
If in a given stream the velocity doubles, the discharge: Choose one answer
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.