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Density of Water at Different Temperatures

Water Density Formula:

\[ \rho = \frac{\rho_0}{1 + \beta \times (T - T_0)} \]

°C
kg/m³
/°C
°C

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1. What is Water Density Calculator?

Definition: This calculator estimates the density of water at different temperatures using thermal expansion properties.

Purpose: It helps scientists, engineers, and students understand how water density changes with temperature, which is crucial for fluid dynamics, thermodynamics, and environmental studies.

2. How Does the Calculator Work?

The calculator uses the formula:

\[ \rho = \frac{\rho_0}{1 + \beta \times (T - T_0)} \]

Where:

Explanation: The formula accounts for thermal expansion effects on water density as temperature changes from the reference point.

3. Importance of Water Density Calculation

Details: Water density affects buoyancy, heat transfer, ocean currents, and many industrial processes. The maximum density occurs at 4°C.

4. Using the Calculator

Tips: Enter the water temperature in °C. Default values are provided for standard conditions (ρ₀=1000 kg/m³, β=0.0002/°C, T₀=4°C).

5. Frequently Asked Questions (FAQ)

Q1: Why is 4°C used as reference temperature?
A: Water reaches its maximum density at 4°C, making it a natural reference point for density calculations.

Q2: How accurate is this calculation?
A: This provides a good approximation for most purposes, but for precise work, consult detailed water property tables.

Q3: Does this work for ice or steam?
A: No, this formula is only valid for liquid water. Phase changes require different calculations.

Q4: Why does water density decrease above 4°C?
A: Thermal expansion causes water molecules to move farther apart as temperature increases, reducing density.

Q5: What's the density of water at room temperature?
A: At 20°C, pure water has a density of about 998.21 kg/m³.

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