Pressure in a liquid is given by:
p = hdg
where
p is pressure at a point in the liquid
h is the height of the liquid above the point
d is the density pf the liquid
g is the acceleration of free-fall
So, water pressure = 150(1000)(10) = 1.5 x 106 Pa
The water pressure at a depth of 1500m is approximately 147 atmospheres or 2200 pounds per square inch (psi). This high pressure is due to the weight of the water above exerting a force on the water below.
Depth charges are typically set to detonate at a specific depth, depending on the target being pursued. Depths can vary, but they are often set between 50 to 150 meters below the water's surface. This depth is chosen to optimize the effectiveness of the explosion against submarines or underwater targets.
The average water depth of shelf breaks typically ranges from 200 to 500 meters, but this can vary depending on the specific location and geological structures present. Shelf breaks mark the point where the continental shelf drops off steeply into the deeper oceanic basin.
For liquids in containers (liquids in static conditions), the pressure in the liquid will depend on the pressure at liquid-vapor interface, the density of the liquid and the depth measured from the liq-vap interface down. As an example let's assume we want to know the hydrostatic pressure in the ocean at a depth of 150 m. We will assume: An atmospheric (barometric) pressure of Po = 100 kPa (kilpascal). Density of sea water of ρw = 1.03 x 103 kg/m3 Depth Δh = 150 m Gravity acceleration g = 9.81 m/s2 Hydrostatic increment of pressure owed to depth Δh relation: ΔP = ρgΔh Total pressure PT at a depth of Δh: PT = Po + ρwgΔh = 100 x 103 Pa + !.03 x 103 kg/m3 ( 9.81 m/s2 )(150 m) ≈ 1 620 x 103 Pa ≈ 1 620 x 103 Pa [ 1 atm/101 325 Pa] ≈ 16.0 atm The pressure increment we experiment at a depth of 150 m in the ocean is about 15 atmospheres (ΔP = ρgΔh).
The pressure at a depth of 100m below the surface of the sea can be calculated using the formula P = ρgh, where P is pressure, ρ is density of the fluid, g is acceleration due to gravity, and h is the depth. Plugging in the values, we get P = (1,150 kg/m^3) * (9.81 m/s^2) * (100m) = 1,131,150 Pa.
Because water is denser than air.
The water pressure at a depth of 1500m is approximately 147 atmospheres or 2200 pounds per square inch (psi). This high pressure is due to the weight of the water above exerting a force on the water below.
Because water is denser than air.
There are 22,500 square meters in 150 meters x 150 meters. 150 meters x 150 meters = 22,500 square meters
Answer: 150 meters is just under 500 feet (492.125 feet).
Water is in the liquid phase at 1 ATM pressure and 150 degrees Celsius. At this temperature and pressure, water exists as a liquid.
Depth charges are typically set to detonate at a specific depth, depending on the target being pursued. Depths can vary, but they are often set between 50 to 150 meters below the water's surface. This depth is chosen to optimize the effectiveness of the explosion against submarines or underwater targets.
Gaseous. If that is 150 degrees C, that would be steam.
330 feet deep at Ilha do Patacho.
150 meters = 0.0932056788 miles.
The average water depth of shelf breaks typically ranges from 200 to 500 meters, but this can vary depending on the specific location and geological structures present. Shelf breaks mark the point where the continental shelf drops off steeply into the deeper oceanic basin.
For liquids in containers (liquids in static conditions), the pressure in the liquid will depend on the pressure at liquid-vapor interface, the density of the liquid and the depth measured from the liq-vap interface down. As an example let's assume we want to know the hydrostatic pressure in the ocean at a depth of 150 m. We will assume: An atmospheric (barometric) pressure of Po = 100 kPa (kilpascal). Density of sea water of ρw = 1.03 x 103 kg/m3 Depth Δh = 150 m Gravity acceleration g = 9.81 m/s2 Hydrostatic increment of pressure owed to depth Δh relation: ΔP = ρgΔh Total pressure PT at a depth of Δh: PT = Po + ρwgΔh = 100 x 103 Pa + !.03 x 103 kg/m3 ( 9.81 m/s2 )(150 m) ≈ 1 620 x 103 Pa ≈ 1 620 x 103 Pa [ 1 atm/101 325 Pa] ≈ 16.0 atm The pressure increment we experiment at a depth of 150 m in the ocean is about 15 atmospheres (ΔP = ρgΔh).