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 = Qt/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 = Qt/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 00.020 seconds)

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!

12 Components of a Hydrograph Calculators

Discharge at Initial Time in Alternative Form of Exponential Decay
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
Go Discharge at Time t = Discharge at Time t=0*exp(-Constant 'a' for Discharge in Exponential Decay*Time)
Recession Constant for Surface Storage
Go Recession Constant for Surface Storage = Recession Constant/Recession Constant for Interflow*Recession Constant for Baseflow
Recession Constant for Interflow
Go Recession Constant for Interflow = Recession Constant/Recession Constant for Surface Storage*Recession Constant for Baseflow
Recession Constant for Base Flow
Go Recession Constant for Baseflow = Recession Constant/Recession Constant for Surface Storage*Recession Constant for Interflow
Recession Constant
Go Recession Constant = Recession Constant for Surface Storage*Recession Constant for Interflow*Recession Constant for Baseflow
Storage Remaining at any Time t
Go Total Storage in Channel Reach = Discharge at Time t/Constant 'a' for Discharge in Exponential Decay
Discharge given Storage
Go Discharge at Time t = Total Storage in Channel Reach*Constant 'a' for Discharge in Exponential Decay
Discharge at Initial Time
Go Discharge at Time t=0 = Discharge at Time t/(Recession Constant^Time)
Discharge concerning Recession Constant
Go Discharge at Time t = Discharge at Time t=0*Recession Constant^Time
Drainage Area given Time Interval from Peak in Straight-Line Method of Baseflow Separation
Go Drainage Area = (Time Interval/0.83)^(1/0.2)
Time Interval from Peak in Straight-Line method of Baseflow Separation
Go Time Interval = 0.83*Drainage Area^0.2

Storage Remaining at any Time t Formula

Total Storage in Channel Reach = Discharge at Time t/Constant 'a' for Discharge in Exponential Decay
S = Qt/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 (Qt) & 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 = Qt/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 (Qt) & 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.
Let Others Know
Facebook
Twitter
Reddit
LinkedIn
Email
WhatsApp
Copied!