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Flow Discharge Calculator Online

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The Flow Discharge Calculator is a valuable tool for estimating the rate at which water flows through a dam or spillway. It is especially useful in the field of hydraulic engineering and hydrology. By inputting specific variables, this calculator yields precise results, making it indispensable for professionals in these industries.

Formula of Flow Discharge Calculator

The calculator employs the following formula to determine the flow discharge:

Q = C * L * H^1.5

  • Q: Flow discharge in cubic meters per second (m³/s).
  • C: Discharge coefficient, a dimensionless factor.
  • L: Length of the spillway or dam crest in meters (m).
  • H: Head, representing the height of water above the spillway crest in meters (m).
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Table of General Terms

To enhance your understanding and streamline the process of using the calculator, here’s a table of general terms and their meanings:

TermMeaning
Flow Discharge (Q)Rate of water flow in cubic meters per second (m³/s)
Discharge Coefficient (C)A dimensionless factor affecting flow rate
Spillway Length (L)Length of the spillway or dam crest in meters (m)
Water Head (H)Height of water above the spillway crest in meters (m)

Example of Flow Discharge Calculator

Let’s consider an example to illustrate the application of the Flow Discharge Calculator. Suppose you have a dam with a length (L) of 50 meters and a water head (H) of 10 meters. You believe the discharge coefficient (C) is 0.7. Using the formula, you can calculate the flow discharge (Q):

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Q = 0.7 * 50 * 10^1.5

Q ≈ 612.372 m³/s

This means that the flow rate through the dam is approximately 612.372 cubic meters per second.

Most Common FAQs

What is the Flow Discharge Calculator used for?

The Calculator is primarily used to estimate the rate at which water flows through dams and spillways. It is essential for engineering and hydrology applications.

Can I use the calculator for different units?

The calculator is designed for use with the provided units (cubic meters, meters), and any deviations may yield inaccurate results.

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