WebOct 15, 2024 · The sand bed was 17.2 m long, 1.0 m wide, and 0.22 m deep. The experiments were carried out always with the same approaching discharge Q = 0.0242 m 3 /s but under three different conditions: no seepage, seepage discharge equal to 10% of Q, and seepage discharge equal to 15% of Q. In the no-seepage experiment, the valve, … WebA stream discharge was measured using standard current meter and mean velocity method.Calculate the discharge of the river ,the equation of current meter is V= 0.51 N + 0.03m/s.Given the data of river measurement below
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WebAug 23, 2013 · See answer (1) Copy. Discharge Velocity is obtained by Dividing the Total Discharge by the total cross Sectional Area , Where Total cross sectional area Consists … WebExpress the derived equation to relay seepage velocity (v s) and discharge velocity (v) as follows:. q = v A = v s A s. Here, q is the flow rate, v is the discharge velocity, A is the gross cross sectional area, v s is the seepage velocity, and A s is the area of void in the cross section of the specimen. Seepage velocity is based upon the void space of the … rockingham gym hire
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WebThe relation between discharge velocity and seepage velocity will be initiated from Darcy’s law. Relation between discharge velocity and … WebApr 28, 2024 · Darcy Velocity and Seepage Velocity In groundwater calculations, Darcy Velocity and Seepage Velocity are used for different purposes. For any calculation where the actual flow rate in units of volume per time (such as liters per day or gallons per minute) is involved, the original Darcy Equation should be used (calculate V D , Equation 1 ... WebAnswer: Seepage velocity is the velocity of groundwater calculated from Darcy's law.Seepage velocity is not the actual velocity of the water in the pores,but the apparent velocity through the bulk of the porous medium.Actual velocity is higher than seepage velocity by a factor which combines the ... other term for woes