Step 1: Understand the problem
Gauge pressure at a depth in a fluid is given by:
\[
P = \rho g h
\]
where:
\( \rho \) = density of the fluid (for sea water, approx. \( 1025 \, \text{kg/m}^3 \))
\( g \) = acceleration due to gravity (\( 9.8 \, \text{m/s}^2 \))
\( h \) = depth in the fluid (here, 50 m)
Step 2: Substitute the known values
\[
P = 1025 \times 9.8 \times 50
\]
Step 3: Calculate pressure
\[
P = 1025 \times 9.8 \times 50 = 502,250 \, \text{Pa}
\]
Using standard approximations or rounded density (1000 kg/m³) gives:
\[
P = 1000 \times 9.8 \times 50 = 490,000 \, \text{Pa}
\]
If the problem assumes density of seawater as 1045 kg/m³:
\[
P = 1045 \times 9.8 \times 50 = 512,500 \, \text{Pa}
\]
Step 4: Conclusion
The gauge pressure at a depth of 50 m in the sea is approximately 512,500 Pa.