Pumping Rate given Transmissivity for Inconsistent Units from Distance-Drawdown Graphs Calculator

✖Transmissivity is the rate at which groundwater flows horizontally through an aquifer or the degree to which a medium allows something, in particular electromagnetic radiation, to pass through it.ⓘ Transmissivity [T]			+10% -10%
✖The Drawdown Across One Log Cycle is referred as change in water level (or hydraulic head) in an aquifer due to pumping from a well.ⓘ Drawdown Across One Log Cycle [Δs]			+10% -10%

✖The Pumping Rate is referred as volume of water (or other fluid) that is pumped per unit of time. It’s typically measured in units like liters per second (L/s) or cubic meters per hour (m³/h).ⓘ Pumping Rate given Transmissivity for Inconsistent Units from Distance-Drawdown Graphs [q]

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Pumping Rate given Transmissivity for Inconsistent Units from Distance-Drawdown Graphs Solution

STEP 0: Pre-Calculation Summary

Formula Used

Pumping Rate = Transmissivity*Drawdown Across One Log Cycle/70
q = T*Δs/70
This formula uses 3 Variables

Variables Used

Pumping Rate - (Measured in Cubic Meter per Second) - The Pumping Rate is referred as volume of water (or other fluid) that is pumped per unit of time. It’s typically measured in units like liters per second (L/s) or cubic meters per hour (m³/h).
Transmissivity - (Measured in Square Meter per Second) - Transmissivity is the rate at which groundwater flows horizontally through an aquifer or the degree to which a medium allows something, in particular electromagnetic radiation, to pass through it.
Drawdown Across One Log Cycle - The Drawdown Across One Log Cycle is referred as change in water level (or hydraulic head) in an aquifer due to pumping from a well.

STEP 1: Convert Input(s) to Base Unit

Transmissivity: 11 Square Meter per Second --> 11 Square Meter per Second No Conversion Required
Drawdown Across One Log Cycle: 44.55 --> No Conversion Required

STEP 2: Evaluate Formula

Substituting Input Values in Formula

q = T*Δs/70 --> 11*44.55/70

Evaluating ... ...

q = 7.00071428571429

STEP 3: Convert Result to Output's Unit

7.00071428571429 Cubic Meter per Second --> No Conversion Required

FINAL ANSWER

7.00071428571429 ≈ 7.000714 Cubic Meter per Second <-- Pumping Rate

(Calculation completed in 00.004 seconds)

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< Distance Drawdown Analysis Calculators

Storage Coefficient from Distance-Drawdown Graphs

LaTeX Go Storage Coefficient = 2.25*Transmissivity*Total Drawdown/Distance from Pumping Well to Point Intersection^2

Drawdown across One Log Cycle from Distance Drawdown Graphs given Transmissivity

LaTeX Go Drawdown Across Log Cycle = 2.3*Pumping Rate/(Transmissivity*2*pi)

Transmissivity from Distance Drawdown Graphs

LaTeX Go Transmissivity = 2.3*Pumping Rate/(2*pi*Drawdown Across Log Cycle)

Pumping Rate from Distance Drawdown Graphs

LaTeX Go Pumping Rate = Transmissivity*2*pi*Drawdown Across Log Cycle/2.3

Pumping Rate given Transmissivity for Inconsistent Units from Distance-Drawdown Graphs Formula

LaTeX Go

Pumping Rate = Transmissivity*Drawdown Across One Log Cycle/70
q = T*Δs/70

What is Aquifer Pumping?

Aquifer Pumping involve the pumping of an aquifer at a known rate and the measurement of the corresponding changes in water levels in the pumped and observation wells. Aquifer hydraulic testing may also be performed by injecting water into a well.

How to Calculate Pumping Rate given Transmissivity for Inconsistent Units from Distance-Drawdown Graphs?

Pumping Rate given Transmissivity for Inconsistent Units from Distance-Drawdown Graphs calculator uses Pumping Rate = Transmissivity*Drawdown Across One Log Cycle/70 to calculate the Pumping Rate, The Pumping Rate given Transmissivity for Inconsistent Units from Distance-Drawdown Graphs formula is defined as the rate at which a well is pumped at a controlled rate and drawdown is measured in one or more surrounding observation wells. Pumping Rate is denoted by q symbol.

How to calculate Pumping Rate given Transmissivity for Inconsistent Units from Distance-Drawdown Graphs using this online calculator? To use this online calculator for Pumping Rate given Transmissivity for Inconsistent Units from Distance-Drawdown Graphs, enter Transmissivity (T) & Drawdown Across One Log Cycle (Δs) and hit the calculate button. Here is how the Pumping Rate given Transmissivity for Inconsistent Units from Distance-Drawdown Graphs calculation can be explained with given input values -> 7.000714 = 11*44.55/70.

FAQ

What is Pumping Rate given Transmissivity for Inconsistent Units from Distance-Drawdown Graphs?

The Pumping Rate given Transmissivity for Inconsistent Units from Distance-Drawdown Graphs formula is defined as the rate at which a well is pumped at a controlled rate and drawdown is measured in one or more surrounding observation wells and is represented as q = T*Δs/70 or Pumping Rate = Transmissivity*Drawdown Across One Log Cycle/70. Transmissivity is the rate at which groundwater flows horizontally through an aquifer or the degree to which a medium allows something, in particular electromagnetic radiation, to pass through it & The Drawdown Across One Log Cycle is referred as change in water level (or hydraulic head) in an aquifer due to pumping from a well.

How to calculate Pumping Rate given Transmissivity for Inconsistent Units from Distance-Drawdown Graphs?

The Pumping Rate given Transmissivity for Inconsistent Units from Distance-Drawdown Graphs formula is defined as the rate at which a well is pumped at a controlled rate and drawdown is measured in one or more surrounding observation wells is calculated using Pumping Rate = Transmissivity*Drawdown Across One Log Cycle/70. To calculate Pumping Rate given Transmissivity for Inconsistent Units from Distance-Drawdown Graphs, you need Transmissivity (T) & Drawdown Across One Log Cycle (Δs). With our tool, you need to enter the respective value for Transmissivity & Drawdown Across One Log Cycle 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 Pumping Rate?

In this formula, Pumping Rate uses Transmissivity & Drawdown Across One Log Cycle. We can use 1 other way(s) to calculate the same, which is/are as follows -

Pumping Rate = Transmissivity*2*pi*Drawdown Across Log Cycle/2.3

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