Storage Remaining at any Time t Calculator

✖Discharge at Time t is the volumetric flow rate of a stream, which volume of water flowing per rate of time at any time t.ⓘ Discharge at Time t [Q_t]			+10% -10%
✖Constant 'a' for Discharge in Exponential Decay. A quantity is subject to exponential decay if it decreases at a rate proportional to its current value.ⓘ Constant 'a' for Discharge in Exponential Decay [a]			+10% -10%

✖Total Storage in Channel Reach is a section of stream or river along which similar hydrologic conditions exist, such as discharge, depth, area, and slope.ⓘ Storage Remaining at any Time t [S]

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Storage Remaining at any Time t Solution

STEP 0: Pre-Calculation Summary

Formula Used

Total Storage in Channel Reach = Discharge at Time t/Constant 'a' for Discharge in Exponential Decay
S = Q_t/a
This formula uses 3 Variables

Variables Used

Total Storage in Channel Reach - (Measured in Cubic Meter) - Total Storage in Channel Reach is a section of stream or river along which similar hydrologic conditions exist, such as discharge, depth, area, and slope.
Discharge at Time t - (Measured in Cubic Meter per Second) - Discharge at Time t is the volumetric flow rate of a stream, which volume of water flowing per rate of time at any time t.
Constant 'a' for Discharge in Exponential Decay - Constant 'a' for Discharge in Exponential Decay. A quantity is subject to exponential decay if it decreases at a rate proportional to its current value.

STEP 1: Convert Input(s) to Base Unit

Discharge at Time t: 1.4162 Cubic Meter per Second --> 1.4162 Cubic Meter per Second No Conversion Required
Constant 'a' for Discharge in Exponential Decay: 1.782 --> No Conversion Required

STEP 2: Evaluate Formula

Substituting Input Values in Formula

S = Q_t/a --> 1.4162/1.782

Evaluating ... ...

S = 0.794725028058361

STEP 3: Convert Result to Output's Unit

0.794725028058361 Cubic Meter --> No Conversion Required

FINAL ANSWER

0.794725028058361 ≈ 0.794725 Cubic Meter <-- Total Storage in Channel Reach

(Calculation completed in 00.004 seconds)

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< Components of a Hydrograph Calculators

Discharge at Initial Time in Alternative Form of Exponential Decay

LaTeX Go Discharge at Time t=0 = Discharge at Time t/exp(-Constant 'a' for Discharge in Exponential Decay*Time)

Discharge in Alternative Form of Exponential Decay

LaTeX Go Discharge at Time t = Discharge at Time t=0*exp(-Constant 'a' for Discharge in Exponential Decay*Time)

Discharge at Initial Time

LaTeX Go Discharge at Time t=0 = Discharge at Time t/(Recession Constant^Time)

Discharge concerning Recession Constant

LaTeX Go Discharge at Time t = Discharge at Time t=0*Recession Constant^Time

Storage Remaining at any Time t Formula

LaTeX Go

Total Storage in Channel Reach = Discharge at Time t/Constant 'a' for Discharge in Exponential Decay
S = Q_t/a

What is Baseflow recession?

A Recession curve of streamflow so adjusted that the slope of the curve represents the runoff depletion rate of the groundwater. A curve is formed by the observed hydrograph during prolonged periods of no precipitation.

How to Calculate Storage Remaining at any Time t?

Storage Remaining at any Time t calculator uses Total Storage in Channel Reach = Discharge at Time t/Constant 'a' for Discharge in Exponential Decay to calculate the Total Storage in Channel Reach, The Storage Remaining at any Time t formula is defined as the water in the system resides or "rests" as it moves from one water reservoir to another. Total Storage in Channel Reach is denoted by S symbol.

How to calculate Storage Remaining at any Time t using this online calculator? To use this online calculator for Storage Remaining at any Time t, enter Discharge at Time t (Q_t) & Constant 'a' for Discharge in Exponential Decay (a) and hit the calculate button. Here is how the Storage Remaining at any Time t calculation can be explained with given input values -> 2.8324 = 1.4162/1.782.

FAQ

What is Storage Remaining at any Time t?

The Storage Remaining at any Time t formula is defined as the water in the system resides or "rests" as it moves from one water reservoir to another and is represented as S = Q_t/a or Total Storage in Channel Reach = Discharge at Time t/Constant 'a' for Discharge in Exponential Decay. Discharge at Time t is the volumetric flow rate of a stream, which volume of water flowing per rate of time at any time t & Constant 'a' for Discharge in Exponential Decay. A quantity is subject to exponential decay if it decreases at a rate proportional to its current value.

How to calculate Storage Remaining at any Time t?

The Storage Remaining at any Time t formula is defined as the water in the system resides or "rests" as it moves from one water reservoir to another is calculated using Total Storage in Channel Reach = Discharge at Time t/Constant 'a' for Discharge in Exponential Decay. To calculate Storage Remaining at any Time t, you need Discharge at Time t (Q_t) & Constant 'a' for Discharge in Exponential Decay (a). With our tool, you need to enter the respective value for Discharge at Time t & Constant 'a' for Discharge in Exponential Decay 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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