To calculate the specific weight of water with ease, it's essential to understand the concept of specific weight and its significance in various engineering and scientific applications. Specific weight, denoted by the symbol γ (gamma), is defined as the weight of a substance per unit volume. For water, this value is crucial in hydrostatics, fluid dynamics, and engineering designs involving water systems, such as dams, canals, and pipelines.
Understanding Specific Weight

The specific weight of water is calculated using the formula γ = ρg, where ρ (rho) is the density of water, and g is the acceleration due to gravity. The density of water varies with temperature; at 4°C (39.2°F), the density of pure water is approximately 1000 kg/m³. The acceleration due to gravity is about 9.81 m/s² on Earth’s surface. Thus, the specific weight of water at 4°C can be calculated as γ = 1000 kg/m³ * 9.81 m/s² = 9810 N/m³.
Density of Water at Different Temperatures
It’s crucial to note that the density of water changes with temperature. Water is most dense at approximately 4°C. As water temperature increases or decreases from this point, its density decreases. This phenomenon is critical in certain applications, such as in the design of water storage tanks or in understanding ocean currents. The following table provides the density of water at different temperatures:
Temperature (°C) | Density (kg/m³) |
---|---|
0 | 999.8 |
4 | 1000 |
10 | 999.7 |
20 | 998.2 |
30 | 995.6 |

Calculating Specific Weight with Ease

To calculate the specific weight of water with ease, follow these steps:
- Determine the temperature of the water. This is crucial because, as discussed, the density of water varies with temperature.
- Look up or calculate the density of water at the given temperature. For simplicity, you can use the density at 4°C, which is 1000 kg/m³, for many applications.
- Use the formula γ = ρg, where ρ is the density of water at the given temperature, and g is the acceleration due to gravity (approximately 9.81 m/s² on Earth).
- Perform the calculation: γ = 1000 kg/m³ * 9.81 m/s² = 9810 N/m³.
Key Points
- The specific weight of water is a critical parameter in various engineering and scientific applications.
- The density of water varies with temperature, with the highest density at approximately 4°C.
- The formula for calculating the specific weight of water is γ = ρg, where ρ is the density of water, and g is the acceleration due to gravity.
- For practical purposes, using the density of water at 4°C (1000 kg/m³) provides a reliable calculation for many applications.
- Considering the temperature of the water is essential for accurate calculations, especially in applications where small variations in density can have significant effects.
Applications and Considerations
The calculation of specific weight is not limited to water but applies to all substances. However, water’s unique properties, such as its high surface tension and the fact that it expands when frozen, make its specific weight particularly noteworthy in various fields. In engineering, understanding the specific weight of water is crucial for designing structures that interact with water, such as ships, bridges, and water towers. In environmental science, the specific weight of water helps in understanding ocean currents, water cycles, and the behavior of aquatic ecosystems.
In conclusion, calculating the specific weight of water with ease involves understanding the concept of specific weight, recognizing the density of water at different temperatures, and applying the formula γ = ρg. This calculation is fundamental in a wide range of applications, from engineering designs to environmental studies, and its accuracy can significantly impact the outcomes of these applications.
What is the specific weight of water at 20°C?
+To find the specific weight of water at 20°C, first, determine the density of water at this temperature, which is approximately 998.2 kg/m³. Then, use the formula γ = ρg, where ρ = 998.2 kg/m³ and g = 9.81 m/s². Thus, γ = 998.2 kg/m³ * 9.81 m/s² = 9793.3 N/m³.
Why does the density of water change with temperature?
+The density of water changes with temperature due to the way water molecules interact. At lower temperatures, water molecules are more closely packed, increasing density. At higher temperatures, the molecules have more kinetic energy, causing them to move more and occupy more space, which decreases density. However, water exhibits an anomalous behavior near 4°C, where it reaches its maximum density, before expanding as it freezes or heats up further.
How does the specific weight of water affect engineering designs?
+The specific weight of water is a critical factor in engineering designs involving water, such as dams, canals, and ships. Accurate calculations of water’s specific weight are necessary to ensure the stability and safety of these structures. For instance, in the design of a dam, the specific weight of water helps engineers calculate the pressure exerted by the water on the dam structure, which is essential for determining the required strength and materials of the dam.