Sea Water Pressure Formula:
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Definition: This calculator estimates the total pressure at a given depth in sea water, accounting for both atmospheric pressure and hydrostatic pressure.
Purpose: It helps divers, engineers, and marine researchers understand the pressure conditions at different ocean depths.
The calculator uses the formula:
Where:
Explanation: The total pressure is the sum of atmospheric pressure and the hydrostatic pressure caused by the weight of the water column above.
Details: Accurate pressure calculations are crucial for diving safety, submarine design, underwater construction, and scientific research.
Tips: Enter the depth in meters, sea water density (default 1025 kg/m³), atmospheric pressure (default 101325 Pa), and gravity (default 9.81 m/s²). Depth and atmospheric pressure can be 0, others must be > 0.
Q1: Why do we include atmospheric pressure?
A: The total pressure at depth includes both the water pressure and the atmospheric pressure pushing down on the ocean's surface.
Q2: What's a typical sea water density?
A: Ocean water averages about 1025 kg/m³, but this varies with salinity and temperature.
Q3: How does pressure change with depth?
A: Pressure increases linearly with depth - about 1 atmosphere (101325 Pa) for every 10 meters of seawater.
Q4: When would I adjust the atmospheric pressure value?
A: For high-altitude bodies of water or precise scientific work, you might use the local atmospheric pressure.
Q5: How accurate is this calculation?
A: It provides a good estimate, but actual pressure can vary slightly due to water temperature, salinity, and local gravity variations.