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Charlie Kay
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Does anyone know a simple formula to calculate the acceleration of gravity underwater?
What makes you think that the acceleration due to gravity is different underwater?Charlie Kay said:Does anyone know a simple formula to calculate the acceleration of gravity underwater?
And where did you get this formula?Charlie Kay said:I have this, "m(d2x/dt2)=(rhoB-rhoA)(g*V)-0.5(Cd)(rhoA)(A)(dx/dt)^2"
When m=body's mass, rhoA=fluid density, rhoB=body density, g=gravity, x=displacement, t=time, Cd=drag coefficient, V=body volume and A=body area
Help??!
SteamKing said:What makes you think that the acceleration due to gravity is different underwater?
Charlie Kay said:a) there is more drag underwater...
The acceleration due to gravity is g, by definition. That equation you have is the net force due to gravity + buoyancy + drag.Charlie Kay said:I have this, "m(d2x/dt2)=(rhoB-rhoA)(g*V)-0.5(Cd)(rhoA)(A)(dx/dt)^2"
When m=body's mass, rhoA=fluid density, rhoB=body density, g=gravity, x=displacement, t=time, Cd=drag coefficient, V=body volume and A=body area
Help??!
nasu said:Yes, but this has nothing to do with the presence of water.
The sea level is just a convenient reference level. You can be under the sea level but not underwater. Or way above the sea level and underwater.
It would be misleading to attribute the change in g due to altitude change to being (or not) "underwater".
XZ923 said:Thanks that's pretty much what I figured. I knew that the presence of water wouldn't matter, I was just curious as to the sea level reference. I understand that it's simply the reference point that was chosen when they calculated the gravitational constant. I guess my question was more along the lines of "is the difference in gravitational force at the bottom of the Mariana's trench and the peak of Mt. Everest (because point A is closer to the center of the Earth's mass than point B; the water of course is irrelevant) significant enough to factor into calculations?
XZ923 said:simply the reference point that was chosen when they calculated the gravitational constant
I stand corrected. Thank you sir. You're right, poor choice of words on my part. And SteamKing thanks for satisfying my curiosity!davenn said:careful with your choice of words there
Gravitational Constant = G = approximately = 6.674×10−11 N⋅m2/kg2 a whole different thing
acceleration due to gravity ( eg at Earth's surface) = g = ~9.81 m/s2
which is the one being discussed
Dave
Charlie Kay said:When I said underwater I mean deep, as in 11,000 m below sea level!
This is pretty deep for diving or submarines.Charlie Kay said:When I said underwater I mean deep, as in 11,000 m below sea level!
nasu said:This is pretty deep for diving or submarines.
But for change in gravity is not much. You compare 11 km with the radius of the Earth which is around 6,400 km. About 0.2%.
You should not expect a significant change. As g goes like r^2, the change in g may be some 0.4% or about 0.04 m/s^2.
nasu said:The bottom of the ocean is not inside a solid sphere, is it?
There may be some corrections if we are looking at a deep narrow oceanic valley but I intended just an estimation of the effect that 11 km will have on g.
It also apply if you go up 11 km.
If you are going inside, the effect is smaller by a factor of 2, in first approximation. But I don't think is relevant here.
nasu said:One more time, I was not talking about what happens inside the Earth.
And I don't contest the 1/r dependence inside a solid, homogeneous, perfectly spherical Earth.
However, if you want to estimate the effect of going on the bottom of the ocean, a large, shallow deep in the crust rather than a narrow pith, I don't think that the 1/r applies.
There is no solid material above you. The 1/r^2 is also not exactly true. The dependence is more complicated. But it was just an order of magnitude estimate.
The difference between 1/r and 1/r^2 is less than an order of magnitude for that small difference so it does not even matter.
If you want to be very accurate, the 1/r does not even work for the real Earth, at that depth. g increases as you go down in the crust, for at least 11 km.
On the average, of course.
Charlie Kay said:Guys, i think I've got it!
someone told me that the acceleration due to gravity = 9.81
m/s2 is meters per second per secondCharlie Kay said:which stands for?
The acceleration of gravity, denoted as g, is the same underwater as it is on land. It is a constant value of 9.8 meters per second squared (m/s2) regardless of the medium.
The formula for calculating the acceleration of gravity underwater is the same as on land: g = F/m, where F is the force of gravity and m is the mass of the object. However, in water, the value for m may change due to buoyancy.
No, the depth of the water does not affect the acceleration of gravity. As long as the object is submerged in water, the acceleration of gravity remains constant at 9.8 m/s2.
The density of water does not directly affect the acceleration of gravity. However, it can affect the buoyancy of an object, which in turn can affect the value of m in the acceleration of gravity formula.
Yes, the same formula can be used to calculate the acceleration of gravity in any body of water, as long as the object is fully submerged. However, the value for m may vary depending on the density of the water.