Transmissibility about straight-line slope Calculator

✖The Discharge refers to the volumetric flow rate of water that is transported through a given cross-sectional area. It includes any suspended solids, dissolved chemicals, or biologic material.ⓘ Discharge [Q]			+10% -10%
✖Slope represents a straight line when plot of residual drawdown s' vs t/t' on semi-log paper.ⓘ Slope [m]			+10% -10%

✖Transmissibility is most simply defined as the effective hydraulic conductivity of an aquifer or other water-bearing unit multiplied by the thickness of that unit.ⓘ Transmissibility about straight-line slope [T]

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Transmissibility about straight-line slope Solution

STEP 0: Pre-Calculation Summary

Formula Used

Transmissibility = 2.302*Discharge/(4*pi*Slope)
T = 2.302*Q/(4*pi*m)
This formula uses 1 Constants, 3 Variables

Constants Used

pi - Archimedes' constant Value Taken As 3.14159265358979323846264338327950288

Variables Used

Transmissibility - (Measured in Square Meter per Second) - Transmissibility is most simply defined as the effective hydraulic conductivity of an aquifer or other water-bearing unit multiplied by the thickness of that unit.
Discharge - (Measured in Cubic Meter per Second) - The Discharge refers to the volumetric flow rate of water that is transported through a given cross-sectional area. It includes any suspended solids, dissolved chemicals, or biologic material.
Slope - Slope represents a straight line when plot of residual drawdown s' vs t/t' on semi-log paper.

STEP 1: Convert Input(s) to Base Unit

Discharge: 3 Cubic Meter per Second --> 3 Cubic Meter per Second No Conversion Required
Slope: 0.157 --> No Conversion Required

STEP 2: Evaluate Formula

Substituting Input Values in Formula

T = 2.302*Q/(4*pi*m) --> 2.302*3/(4*pi*0.157)

Evaluating ... ...

T = 3.50039502226952

STEP 3: Convert Result to Output's Unit

3.50039502226952 Square Meter per Second --> No Conversion Required

FINAL ANSWER

3.50039502226952 ≈ 3.500395 Square Meter per Second <-- Transmissibility

(Calculation completed in 00.004 seconds)

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Created by Mithila Muthamma PA

Coorg Institute of Technology (CIT), Coorg

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< Recovery of Piezometric Head Calculators

Equation for Residual Drawdown for small values of Distance and large values of Time

LaTeX Go Residual Drawdown = (2.302*Discharge/4*pi*Transmissibility)*log10(Time from start of pump/Time since Stoppage of Pumping)

Equation for Residual Drawdown

LaTeX Go Residual Drawdown = (Discharge/4*pi*Transmissibility)*(Well Function of u-Well Function after the Cessation of Pumping)

Equation for Slope of Line

LaTeX Go Slope = 2.302*Discharge/(4*pi*Transmissibility)

Discharge about straight-line slope

LaTeX Go Discharge = 4*pi*Transmissibility*Slope/2.302

Transmissibility about straight-line slope Formula

LaTeX Go

Transmissibility = 2.302*Discharge/(4*pi*Slope)
T = 2.302*Q/(4*pi*m)

What is Discharge?

Discharge is the volumetric flow rate of water that is transported through a given cross-sectional area. It includes any suspended solids, dissolved chemicals, or biologic material in addition to the water itself.

How to Calculate Transmissibility about straight-line slope?

Transmissibility about straight-line slope calculator uses Transmissibility = 2.302*Discharge/(4*pi*Slope) to calculate the Transmissibility, The transmissibility about straight-line slope is defined as the ability of the aquifer to transmit groundwater throughout its entire saturated thickness. Transmissibility is denoted by T symbol.

How to calculate Transmissibility about straight-line slope using this online calculator? To use this online calculator for Transmissibility about straight-line slope, enter Discharge (Q) & Slope (m) and hit the calculate button. Here is how the Transmissibility about straight-line slope calculation can be explained with given input values -> 3.500395 = 2.302*3/(4*pi*0.157).

FAQ

What is Transmissibility about straight-line slope?

The transmissibility about straight-line slope is defined as the ability of the aquifer to transmit groundwater throughout its entire saturated thickness and is represented as T = 2.302*Q/(4*pi*m) or Transmissibility = 2.302*Discharge/(4*pi*Slope). The Discharge refers to the volumetric flow rate of water that is transported through a given cross-sectional area. It includes any suspended solids, dissolved chemicals, or biologic material & Slope represents a straight line when plot of residual drawdown s' vs t/t' on semi-log paper.

How to calculate Transmissibility about straight-line slope?

The transmissibility about straight-line slope is defined as the ability of the aquifer to transmit groundwater throughout its entire saturated thickness is calculated using Transmissibility = 2.302*Discharge/(4*pi*Slope). To calculate Transmissibility about straight-line slope, you need Discharge (Q) & Slope (m). With our tool, you need to enter the respective value for Discharge & Slope and hit the calculate button. You can also select the units (if any) for Input(s) and the Output as well.

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