Formula Used:
From: | To: |
The Hagen-Poiseuille equation describes laminar flow through conduits and porous media. It provides a relationship between flow parameters and the mean particle size of the porous medium, helping in the analysis of fluid flow through granular materials.
The calculator uses the formula:
Where:
Explanation: The equation calculates the mean particle size based on permeability, fluid properties, and shape characteristics of the porous medium.
Details: Determining the mean particle size is crucial for understanding flow characteristics through porous media, designing filtration systems, and analyzing groundwater flow in soil mechanics.
Tips: Enter all required parameters with appropriate units. Ensure values are positive and within reasonable physical ranges for accurate results.
Q1: What is the significance of the shape factor?
A: The shape factor accounts for the geometry and packing of particles in the porous medium, affecting flow characteristics.
Q2: How does fluid viscosity affect the result?
A: Higher viscosity fluids experience greater resistance to flow, which influences the calculated particle size.
Q3: What are typical values for permeability coefficient?
A: Permeability varies widely depending on the material, from 10⁻¹² m/s for clay to 10⁻¹ m/s for gravel.
Q4: When is this equation most applicable?
A: This equation is most accurate for laminar flow conditions through homogeneous porous media.
Q5: How does unit weight affect the calculation?
A: Unit weight represents the fluid's density and gravity effects, influencing the driving force for flow through the medium.