Answer:
[tex]p = g*\rho*h+p_{atm}[/tex]
Explanation:
The pressure will vary with the hydrostatic pressure ([tex]g*\rho*h[/tex]), which is the pressure of a column of liquid with height h, the total pressure under the water will be the hydrostatic pressure plus the atmospheric pressure, the equation is:
[tex]p = g*\rho*h+p_{atm}[/tex]
Where:
- [tex]p=[/tex] total pressure.
- [tex]g=[/tex] gravitational acceleration.
- [tex]\rho=[/tex] fluid density.
- [tex]h=[/tex] height.
- [tex]p_{atm}=[/tex] atmospheric pressure.
In this planet, [tex]g\textrm{ and } p_{atm} \textrm{ could be different than in the Earth.}[/tex]
This is a reasonable estimation because many liquids can be considered incompressible, then we can assume a constant density throughout the liquid.
