Water's density is a critical factor in various industries and scientific fields. Understanding its precise value is crucial for accurate measurements, calculations, and efficient water management.
At 4 degrees Celsius (39.2 degrees Fahrenheit), the standard density of pure water is defined as 8.34 pounds per gallon (lb/gal). This value is used as a reference point for comparison and is widely accepted across scientific disciplines.
The density of water has significant implications in numerous applications:
While the standard density is 8.34 lb/gal, water density can vary slightly under certain conditions:
Temperature (Celsius) | Density (lb/gal) |
---|---|
0 | 8.38 |
4 | 8.34 |
10 | 8.29 |
20 | 8.21 |
30 | 8.14 |
40 | 8.07 |
50 | 8.01 |
60 | 7.95 |
70 | 7.89 |
80 | 7.83 |
90 | 7.77 |
100 | 7.71 |
Pressure (atmospheres) | Density (lb/gal) |
---|---|
1 | 8.34 |
10 | 8.35 |
50 | 8.36 |
100 | 8.37 |
500 | 8.39 |
1000 | 8.40 |
Salinity (parts per thousand) | Density (lb/gal) |
---|---|
0 (pure water) | 8.34 |
5 | 8.35 |
10 | 8.36 |
15 | 8.38 |
20 | 8.39 |
25 | 8.41 |
30 | 8.43 |
35 (seawater) | 8.46 |
The unique density of water enables its utilization in various innovative applications:
The density of water is a fundamental property that underpins numerous scientific and industrial applications. Understanding its precise value and variations is crucial for accurate measurements, efficient water management, and innovative technological advancements.
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