Water Viscosity Equation:
Where:
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Dynamic viscosity (μ) is a measure of a fluid's resistance to flow. For water, viscosity decreases as temperature increases. This calculator provides the dynamic viscosity of water at a specified temperature.
The calculator uses the Andrade equation:
Where:
Explanation: The equation models the exponential relationship between water viscosity and temperature, with empirically determined constants.
Details: Water viscosity is critical in fluid dynamics calculations, heat transfer analysis, chemical engineering processes, and biological systems. It affects flow rates, pressure drops, and mixing efficiency.
Tips: Enter temperature in Kelvin (between 273.15K and 373.15K). The calculator is valid for liquid water in this temperature range.
Q1: What's the difference between dynamic and kinematic viscosity?
A: Dynamic viscosity (μ) is the fluid's resistance to shear flow, while kinematic viscosity (ν) is μ divided by density (ν = μ/ρ).
Q2: Why does viscosity decrease with temperature?
A: Higher temperatures increase molecular motion, reducing intermolecular forces and making the fluid flow more easily.
Q3: How accurate is this calculation?
A: The Andrade equation provides good estimates (±2%) for pure water in the specified temperature range.
Q4: Does this work for seawater or other liquids?
A: No, this calculator is for pure water only. Salinity and other solutes significantly affect viscosity.
Q5: What are typical water viscosity values?
A: At 20°C (293.15K), μ≈1.002×10⁻³ Pa·s. At 100°C (373.15K), μ≈0.282×10⁻³ Pa·s.