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]

⎘ Copy

👎

Formula

LaTeX

Reset

👍

Download Engineering Hydrology Formula PDF PDF Image

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)

You are here -

Home » Engineering » Civil » Engineering Hydrology » Groundwater Hydrology » Recovery of Piezometric Head » Transmissibility about straight-line slope

Credits

Created by Mithila Muthamma PA

Coorg Institute of Technology (CIT), Coorg

Mithila Muthamma PA has created this Calculator and 2000+ more calculators!

Verified by Chandana P Dev

NSS College of Engineering (NSSCE), Palakkad

Chandana P Dev has verified this Calculator and 1700+ more calculators!

< 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.

Spanish French German Russian Italian Portuguese Polish Dutch

Home

FREE PDFs

🔍 Search