Transmissivity given Discharge Quantity Calculator

✖The Total Water Volume refers to the quantity of water during the entire event under consideration, for example, tide period.ⓘ Total Water Volume [V_w]			+10% -10%
✖The Aquifer Thickness is referred as vertical distance between the top and bottom boundaries of an aquifer, typically measured in feet or meters.ⓘ Aquifer Thickness [b]			+10% -10%
✖The Distance Between the Points is often used to calculate various parameters such as slope, hydraulic gradient, and flow characteristics.ⓘ Distance Between the Points [dl]			+10% -10%
✖Change in Head Between the Points refers to the difference in the hydraulic head at two different points in a fluid system separated by a small distance dl.ⓘ Change in Head Between the Points [ΔH]			+10% -10%

✖The Transmissivity refers to the measure of how much water can be transmitted horizontally through an aquifer is the product of the hydraulic conductivity of the aquifer and its saturated thickness.ⓘ Transmissivity given Discharge Quantity [τ]

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Transmissivity given Discharge Quantity Solution

STEP 0: Pre-Calculation Summary

Formula Used

Transmissivity = (Total Water Volume/Aquifer Thickness)*(Distance Between the Points/Change in Head Between the Points)
τ = (V_w/b)*(dl/ΔH)
This formula uses 5 Variables

Variables Used

Transmissivity - (Measured in Square Meter per Second) - The Transmissivity refers to the measure of how much water can be transmitted horizontally through an aquifer is the product of the hydraulic conductivity of the aquifer and its saturated thickness.
Total Water Volume - (Measured in Cubic Meter per Second) - The Total Water Volume refers to the quantity of water during the entire event under consideration, for example, tide period.
Aquifer Thickness - (Measured in Meter) - The Aquifer Thickness is referred as vertical distance between the top and bottom boundaries of an aquifer, typically measured in feet or meters.
Distance Between the Points - (Measured in Meter) - The Distance Between the Points is often used to calculate various parameters such as slope, hydraulic gradient, and flow characteristics.
Change in Head Between the Points - (Measured in Meter) - Change in Head Between the Points refers to the difference in the hydraulic head at two different points in a fluid system separated by a small distance dl.

STEP 1: Convert Input(s) to Base Unit

Total Water Volume: 50 Cubic Meter per Second --> 50 Cubic Meter per Second No Conversion Required
Aquifer Thickness: 29 Meter --> 29 Meter No Conversion Required
Distance Between the Points: 0.51 Meter --> 0.51 Meter No Conversion Required
Change in Head Between the Points: 0.5 Meter --> 0.5 Meter No Conversion Required

STEP 2: Evaluate Formula

Substituting Input Values in Formula

τ = (V_w/b)*(dl/ΔH) --> (50/29)*(0.51/0.5)

Evaluating ... ...

τ = 1.75862068965517

STEP 3: Convert Result to Output's Unit

1.75862068965517 Square Meter per Second --> No Conversion Required

FINAL ANSWER

1.75862068965517 ≈ 1.758621 Square Meter per Second <-- Transmissivity

(Calculation completed in 00.004 seconds)

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< Transmissivity of Aquifer Calculators

Transmissivity given Discharge Quantity

LaTeX Go Transmissivity = (Total Water Volume/Aquifer Thickness)*(Distance Between the Points/Change in Head Between the Points)

Quantity of Water for Transmissivity

LaTeX Go Total Water Volume = Transmissivity*Aquifer Thickness*Hydraulic Gradient

Transmissibility when Coefficient of Permeability is Considered

LaTeX Go Transmissivity = Coefficient of Permeability at 20° C*Aquifer Thickness

Unit Dimension of Aquifer about Transmissivity

LaTeX Go Aquifer Thickness = Transmissivity/Coefficient of Permeability at 20° C

Transmissivity given Discharge Quantity Formula

LaTeX Go

Transmissivity = (Total Water Volume/Aquifer Thickness)*(Distance Between the Points/Change in Head Between the Points)
τ = (V_w/b)*(dl/ΔH)

What is Transmissivity?

The Capacity of an aquifer to transmit water of the prevailing Kinematic Viscosity is referred to as its Transmissivity. The Transmissivity (T) of an aquifer is equal to the hydraulic conductivity of the aquifer multiplied by the saturated thickness of the aquifer.

How to Calculate Transmissivity given Discharge Quantity?

Transmissivity given Discharge Quantity calculator uses Transmissivity = (Total Water Volume/Aquifer Thickness)*(Distance Between the Points/Change in Head Between the Points) to calculate the Transmissivity, The Transmissivity given Discharge Quantity formula is defined as the capacity of an aquifer to transmit water of the prevailing kinematic viscosity. Transmissivity is denoted by τ symbol.

How to calculate Transmissivity given Discharge Quantity using this online calculator? To use this online calculator for Transmissivity given Discharge Quantity, enter Total Water Volume (V_w), Aquifer Thickness (b), Distance Between the Points (dl) & Change in Head Between the Points (ΔH) and hit the calculate button. Here is how the Transmissivity given Discharge Quantity calculation can be explained with given input values -> 3.4 = (50/29)*(0.51/0.5).

FAQ

What is Transmissivity given Discharge Quantity?

The Transmissivity given Discharge Quantity formula is defined as the capacity of an aquifer to transmit water of the prevailing kinematic viscosity and is represented as τ = (V_w/b)*(dl/ΔH) or Transmissivity = (Total Water Volume/Aquifer Thickness)*(Distance Between the Points/Change in Head Between the Points). The Total Water Volume refers to the quantity of water during the entire event under consideration, for example, tide period, The Aquifer Thickness is referred as vertical distance between the top and bottom boundaries of an aquifer, typically measured in feet or meters, The Distance Between the Points is often used to calculate various parameters such as slope, hydraulic gradient, and flow characteristics & Change in Head Between the Points refers to the difference in the hydraulic head at two different points in a fluid system separated by a small distance dl.

How to calculate Transmissivity given Discharge Quantity?

The Transmissivity given Discharge Quantity formula is defined as the capacity of an aquifer to transmit water of the prevailing kinematic viscosity is calculated using Transmissivity = (Total Water Volume/Aquifer Thickness)*(Distance Between the Points/Change in Head Between the Points). To calculate Transmissivity given Discharge Quantity, you need Total Water Volume (V_w), Aquifer Thickness (b), Distance Between the Points (dl) & Change in Head Between the Points (ΔH). With our tool, you need to enter the respective value for Total Water Volume, Aquifer Thickness, Distance Between the Points & Change in Head Between the Points 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 Transmissivity?

In this formula, Transmissivity uses Total Water Volume, Aquifer Thickness, Distance Between the Points & Change in Head Between the Points. We can use 2 other way(s) to calculate the same, which is/are as follows -

Transmissivity = Coefficient of Permeability at 20° C*Aquifer Thickness
Transmissivity = Equivalent Permeability*Aquifer Thickness

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