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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.
discharge velocity is the quantity of flow that flows through a unit cross sectional area of the soil in a unit time discharge velocity is used to determine the quantity of flow through soil seepage velocity the actual rate of movement of the water as measured with dye tracer for instance, is the seepage velocity
velocity = displacement / time taken
Velocity/wavelength=frequency
Acceleration is the rate of change of the magnitude of velocity and the direction in which the velocity changes.
When the discharge of a stream increases, so does it's velocity. When it decreases, so does the velocity.
The higher the velocity of the stream the larger carrying capacity it has.
the competence and capacity of a steam depend on a streams velocity and discharge. Because the velocity and discharge of a given stream are not constant , the competence and capacity of a stream are not constant . competence and capacity vary along a stream and change throughout the year.
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.
When a stream's discharge increases, erosive energy increases.
discharge velocity is the quantity of flow that flows through a unit cross sectional area of the soil in a unit time discharge velocity is used to determine the quantity of flow through soil seepage velocity the actual rate of movement of the water as measured with dye tracer for instance, is the seepage velocity
i think it is width X depth X velocity=discharge ?
starting with the same velocity
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
If in a given stream the velocity doubles, the discharge: Choose one answer
Capacity Velocity
The velocity and discharge volume of the stream or river.