Stream Flow Discharge Given Suspended Sediment Load Calculator

Formula Used:

\[ Q = \left( \frac{Qs}{K} \right)^{\frac{1}{n}} \]

Stream Discharge (Q):

Unit Converter ▲

Unit Converter ▼

From:	To:

1. What Is The Stream Flow Discharge Given Suspended Sediment Load Formula?

The formula calculates stream discharge based on suspended sediment load, soil erodibility factor, and a constant n. It's used in hydrology and sediment transport studies to estimate water flow rates from sediment measurements.

2. How Does The Calculator Work?

The calculator uses the formula:

\[ Q = \left( \frac{Qs}{K} \right)^{\frac{1}{n}} \]

Where:

\( Q \) — Stream Discharge (m³/s)
\( Qs \) — Suspended Sediment Load (kg/s)
\( K \) — Soil Erodibility Factor
\( n \) — Constant n for the catchment

Explanation: This formula relates stream discharge to the suspended sediment load, accounting for soil erodibility and catchment-specific characteristics through the constant n.

3. Importance Of Stream Discharge Calculation

Details: Accurate stream discharge estimation is essential for water resource management, flood prediction, sediment transport studies, and environmental impact assessments.

4. Using The Calculator

Tips: Enter suspended sediment load in kg/s, soil erodibility factor, and constant n. All values must be positive numbers greater than zero.

5. Frequently Asked Questions (FAQ)

Q1: What is suspended sediment load?
A: Suspended sediment load refers to the portion of sediment that remains uplifted and transported by flowing water in streams and rivers.

Q2: How is soil erodibility factor determined?
A: Soil erodibility factor is typically determined through soil testing and analysis of soil properties that affect its susceptibility to erosion.

Q3: What does constant n represent?
A: Constant n is a catchment-specific parameter that accounts for the effective rainfall and other hydrological characteristics of the watershed.

Q4: When is this formula most applicable?
A: This formula is particularly useful in sediment transport studies and situations where direct discharge measurements are challenging but sediment data is available.

Q5: Are there limitations to this approach?
A: The accuracy depends on proper determination of the constant n and assumes a consistent relationship between sediment load and discharge for the specific catchment.