Stream Flow Discharge given Suspended Sediment Load Calculator

✖Suspended Sediment Load of a flowing fluid, such as a river, refers to the portion of sediment that remains uplifted by the fluid’s flow during the process of sediment transportation.ⓘ Suspended Sediment Load [Q_s]			+10% -10%
✖Soil Erodibility Factor is the intrinsic susceptibility of a soil to erosion by runoff and raindrop impact.ⓘ Soil Erodibility Factor [K]			+10% -10%
✖Constant n is for the catchment to be determined by the effective rainfall of the catchment.ⓘ Constant n [n]			+10% -10%

✖Stream Discharge is the volumetric flow rate of water that is transported through a given cross-sectional area.ⓘ Stream Flow Discharge given Suspended Sediment Load [Q]

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Stream Flow Discharge given Suspended Sediment Load Solution

STEP 0: Pre-Calculation Summary

Formula Used

Stream Discharge = (Suspended Sediment Load/Soil Erodibility Factor)^(1/Constant n)
Q = (Q_s/K)^(1/n)
This formula uses 4 Variables

Variables Used

Stream Discharge - (Measured in Cubic Meter per Second) - Stream Discharge is the volumetric flow rate of water that is transported through a given cross-sectional area.
Suspended Sediment Load - (Measured in Kilogram per Second) - Suspended Sediment Load of a flowing fluid, such as a river, refers to the portion of sediment that remains uplifted by the fluid’s flow during the process of sediment transportation.
Soil Erodibility Factor - Soil Erodibility Factor is the intrinsic susceptibility of a soil to erosion by runoff and raindrop impact.
Constant n - Constant n is for the catchment to be determined by the effective rainfall of the catchment.

STEP 1: Convert Input(s) to Base Unit

Suspended Sediment Load: 230 Ton (metric) per Day --> 2.66203703703704 Kilogram per Second (Check conversion here)
Soil Erodibility Factor: 0.17 --> No Conversion Required
Constant n: 3 --> No Conversion Required

STEP 2: Evaluate Formula

Substituting Input Values in Formula

Q = (Q_s/K)^(1/n) --> (2.66203703703704/0.17)^(1/3)

Evaluating ... ...

Q = 2.50181422414905

STEP 3: Convert Result to Output's Unit

2.50181422414905 Cubic Meter per Second --> No Conversion Required

FINAL ANSWER

2.50181422414905 ≈ 2.501814 Cubic Meter per Second <-- Stream Discharge

(Calculation completed in 00.004 seconds)

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Coorg Institute of Technology (CIT), Coorg

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< Channel Erosion Calculators

Stream Flow Discharge given Suspended Sediment Load

LaTeX Go Stream Discharge = (Suspended Sediment Load/Soil Erodibility Factor)^(1/Constant n)

Soil Erodibility Factor given Suspended Sediment Load

LaTeX Go Soil Erodibility Factor = Suspended Sediment Load/(Stream Discharge^Constant n)

Equation for Suspended Sediment Load

LaTeX Go Suspended Sediment Load = Soil Erodibility Factor*(Stream Discharge^Constant n)

Stream Flow Discharge given Suspended Sediment Load Formula

LaTeX Go

Stream Discharge = (Suspended Sediment Load/Soil Erodibility Factor)^(1/Constant n)
Q = (Q_s/K)^(1/n)

What is Soil Erodibility?

Soil Erodibility (K) is the intrinsic susceptibility of soil to erosion by runoff and raindrop impact. Values of K range from the lowest erodibility, 0.02, to the highest, 0.69. All other factors being equal, the higher the K value, the greater the susceptibility of the soil to rill and sheet erosion by rainfall.

What is Discharge In Hydrology?

In Hydrology, 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 biological material in addition to the water itself.

How to Calculate Stream Flow Discharge given Suspended Sediment Load?

Stream Flow Discharge given Suspended Sediment Load calculator uses Stream Discharge = (Suspended Sediment Load/Soil Erodibility Factor)^(1/Constant n) to calculate the Stream Discharge, The Stream Flow Discharge given Suspended Sediment Load formula is defined as the volumetric flow rate of water that is transported through a given cross-sectional area. Stream Discharge is denoted by Q symbol.

How to calculate Stream Flow Discharge given Suspended Sediment Load using this online calculator? To use this online calculator for Stream Flow Discharge given Suspended Sediment Load, enter Suspended Sediment Load (Q_s), Soil Erodibility Factor (K) & Constant n (n) and hit the calculate button. Here is how the Stream Flow Discharge given Suspended Sediment Load calculation can be explained with given input values -> 2.501814 = (2.66203703703704/0.17)^(1/3).

FAQ

What is Stream Flow Discharge given Suspended Sediment Load?

The Stream Flow Discharge given Suspended Sediment Load formula is defined as the volumetric flow rate of water that is transported through a given cross-sectional area and is represented as Q = (Q_s/K)^(1/n) or Stream Discharge = (Suspended Sediment Load/Soil Erodibility Factor)^(1/Constant n). Suspended Sediment Load of a flowing fluid, such as a river, refers to the portion of sediment that remains uplifted by the fluid’s flow during the process of sediment transportation, Soil Erodibility Factor is the intrinsic susceptibility of a soil to erosion by runoff and raindrop impact & Constant n is for the catchment to be determined by the effective rainfall of the catchment.

How to calculate Stream Flow Discharge given Suspended Sediment Load?

The Stream Flow Discharge given Suspended Sediment Load formula is defined as the volumetric flow rate of water that is transported through a given cross-sectional area is calculated using Stream Discharge = (Suspended Sediment Load/Soil Erodibility Factor)^(1/Constant n). To calculate Stream Flow Discharge given Suspended Sediment Load, you need Suspended Sediment Load (Q_s), Soil Erodibility Factor (K) & Constant n (n). With our tool, you need to enter the respective value for Suspended Sediment Load, Soil Erodibility Factor & Constant n 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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