Mithila Muthamma PA
Coorg Institute of Technology (CIT), Coorg
Mithila Muthamma PA has created this Calculator and 500+ more calculators!
Himanshi Sharma
Bhilai Institute of Technology (BIT), Raipur
Himanshi Sharma has verified this Calculator and 500+ more calculators!

11 Other formulas that you can solve using the same Inputs

Observed Drawdown in the Unconfined Aquifer
Possible Drawdown in Confined Aquifer=Observed Drawdown in the Unconfined Aquifer-(Observed Drawdown in the Unconfined Aquifer^2/2*Aquifer Thickness at Midpoint ) GO
Porosity of the Soil when Infiltration Capacity is Given from Green-Ampt Equation
Volume percent of porosity=((Infiltration Capacity into Soil/Hydraulic Conductivity-1)*Cumulative Infiltration Capacity/Capillary Suction at the Wetting Front) GO
Green-Ampt Equation
Infiltration Capacity into Soil=Hydraulic Conductivity*(1+Porosity*Capillary Suction at the Wetting Front/Cumulative Infiltration Capacity) GO
Sorptivity when Cumulative Infiltration Capacity is Given from Philip's Equation
Sorptivity=(Cumulative Infiltration Capacity-Hydraulic Conductivity*Duration of the Rainfall)/(Duration of the Rainfall^0.5) GO
Philip's Equation
Cumulative Infiltration Capacity=(Sorptivity*Duration of the Rainfall^0.5)+Hydraulic Conductivity*Duration of the Rainfall GO
Sorptivity when Infiltration Capacity is Given
Sorptivity=(Infiltration Capacity into Soil-Hydraulic Conductivity)*2/(Duration of the Rainfall^-0.5) GO
Equation for Infiltration Capacity
Infiltration Capacity into Soil=0.5*Sorptivity*Duration of the Rainfall^-0.5+Hydraulic Conductivity GO
Darcy's Law
Quantity of water=Hydraulic Conductivity*Cross sectional area*Hydraulic Gradient GO
The Rate of Movement Through an Aquifer and a Confining Bed
Groundwater Velocity=(Hydraulic Conductivity/Porosity)*Hydraulic Gradient GO
Thickness of Aquifer when Transmissivity is Given
Aquifer Thickness at Midpoint =Transmissivity/Hydraulic Conductivity GO
Transmissivity of Aquifer
Transmissivity=Hydraulic Conductivity*Aquifer Thickness at Midpoint GO

5 Other formulas that calculate the same Output

Quantity of Water in Steady-State Unsaturated Flow in the Direction of Downward Movement
Quantity of water=(Effective Hydraulic Conductivity *Cross sectional area*((Water Rise-Length of the Water Column)/Length of the Water Column))-Hydraulic Gradient GO
Quantity of Water in Steady-State Unsaturated Flow in the Direction of Upward Movement
Quantity of water=(Effective Hydraulic Conductivity *Cross sectional area*((Water Rise-Length of the Water Column)/Length of the Water Column))+Hydraulic Gradient GO
Darcy's Law
Quantity of water=Hydraulic Conductivity*Cross sectional area*Hydraulic Gradient GO
Quantity of Water when Transmissivity is Given
Quantity of water=Transmissivity*Large Width of Aquifer*Hydraulic Gradient GO
Velocity Equation of Hydraulics
Quantity of water=Cross sectional area*Groundwater Velocity GO

Flow Through any Square from Darcy's law for Ground Water Flow Nets Formula

Quantity of water=Hydraulic Conductivity*Distance Between Flow Lines*Aquifer Thickness at Midpoint *(Difference in Head Between Equipotential Lines/Distance Between Equipotential Lines)
Q=K*w*b*(dh/dl)
More formulas
Quantity of Water in Steady-State Unsaturated Flow in the Direction of Downward Movement GO
Quantity of Water in Steady-State Unsaturated Flow in the Direction of Upward Movement GO
Total Flow through any Set or Group of Equipotential Lines GO
Number of Squares Through Which the Flow occurs when Total Flow is given GO
Flow Through any Square when Total Flow is Given GO

What is Groundwater Flownet ?

A Groundwater Flownet is a graphical representation of two-dimensional steady-state groundwater flow through aquifers.

How to Calculate Flow Through any Square from Darcy's law for Ground Water Flow Nets?

Flow Through any Square from Darcy's law for Ground Water Flow Nets calculator uses Quantity of water=Hydraulic Conductivity*Distance Between Flow Lines*Aquifer Thickness at Midpoint *(Difference in Head Between Equipotential Lines/Distance Between Equipotential Lines) to calculate the Quantity of water, Flow Through any Square from Darcy's law for Ground Water Flow Nets is defined as direction of ground-water movement to estimate the quantity of water in transit through an aquifer. Quantity of water and is denoted by Q symbol.

How to calculate Flow Through any Square from Darcy's law for Ground Water Flow Nets using this online calculator? To use this online calculator for Flow Through any Square from Darcy's law for Ground Water Flow Nets, enter Hydraulic Conductivity (K), Distance Between Flow Lines (w), Aquifer Thickness at Midpoint (b), Difference in Head Between Equipotential Lines (dh) and Distance Between Equipotential Lines (dl) and hit the calculate button. Here is how the Flow Through any Square from Darcy's law for Ground Water Flow Nets calculation can be explained with given input values -> 0 = (0)*40*35*(20/0.028).

FAQ

What is Flow Through any Square from Darcy's law for Ground Water Flow Nets?
Flow Through any Square from Darcy's law for Ground Water Flow Nets is defined as direction of ground-water movement to estimate the quantity of water in transit through an aquifer and is represented as Q=K*w*b*(dh/dl) or Quantity of water=Hydraulic Conductivity*Distance Between Flow Lines*Aquifer Thickness at Midpoint *(Difference in Head Between Equipotential Lines/Distance Between Equipotential Lines). Hydraulic Conductivity depends on the size and arrangement of the water-transmitting openings and on the dynamic characteristics of the fluid, Distance Between Flow Lines in the series of Flow net, Aquifer Thickness at Midpoint between Equipotential lines, Difference in Head Between Equipotential Lines and Distance Between Equipotential Lines.
How to calculate Flow Through any Square from Darcy's law for Ground Water Flow Nets?
Flow Through any Square from Darcy's law for Ground Water Flow Nets is defined as direction of ground-water movement to estimate the quantity of water in transit through an aquifer is calculated using Quantity of water=Hydraulic Conductivity*Distance Between Flow Lines*Aquifer Thickness at Midpoint *(Difference in Head Between Equipotential Lines/Distance Between Equipotential Lines). To calculate Flow Through any Square from Darcy's law for Ground Water Flow Nets, you need Hydraulic Conductivity (K), Distance Between Flow Lines (w), Aquifer Thickness at Midpoint (b), Difference in Head Between Equipotential Lines (dh) and Distance Between Equipotential Lines (dl). With our tool, you need to enter the respective value for Hydraulic Conductivity, Distance Between Flow Lines, Aquifer Thickness at Midpoint , Difference in Head Between Equipotential Lines and Distance Between Equipotential Lines and hit the calculate button. You can also select the units (if any) for Input(s) and the Output as well.
How many ways are there to calculate Quantity of water?
In this formula, Quantity of water uses Hydraulic Conductivity, Distance Between Flow Lines, Aquifer Thickness at Midpoint , Difference in Head Between Equipotential Lines and Distance Between Equipotential Lines. We can use 5 other way(s) to calculate the same, which is/are as follows -
  • Quantity of water=Hydraulic Conductivity*Cross sectional area*Hydraulic Gradient
  • Quantity of water=(Effective Hydraulic Conductivity *Cross sectional area*((Water Rise-Length of the Water Column)/Length of the Water Column))-Hydraulic Gradient
  • Quantity of water=(Effective Hydraulic Conductivity *Cross sectional area*((Water Rise-Length of the Water Column)/Length of the Water Column))+Hydraulic Gradient
  • Quantity of water=Cross sectional area*Groundwater Velocity
  • Quantity of water=Transmissivity*Large Width of Aquifer*Hydraulic Gradient
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