Determining hydrostatic force on a sphere

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The discussion focuses on calculating the hydrostatic forces on a submerged solid sphere, specifically the vertical and horizontal forces exerted by water. The vertical force is derived by integrating the differential pressure across the sphere's surface, resulting in a formula that confirms the buoyant force as F_V = (4/3)πR³γ. For the horizontal force, it is suggested that the integration should consider the symmetry of the sphere, leading to the conclusion that the horizontal forces cancel out, resulting in a net force of zero. The importance of correctly setting up the coordinate system is emphasized to accurately evaluate the forces. Overall, the discussion highlights the necessity of proper integration techniques and understanding of hydrostatic principles in determining forces on submerged objects.
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Homework Statement


A solid sphere with radius ##R## is submerged on water at a depth ##h_1##. Water's specific weight is ##\gamma##.
Determine both horizontal and vertical forces exerted by the water on the surface of the sphere, in terms of ##R## and ##\gamma##.

Homework Equations


My lecturer wants the solution to be achieved by integrating the differential pressure of the sphere, so I believe the only relevant equations are ##F = p A## and ##p = (p_0 + \gamma h)##. I am also assuming ##p_0 = 0##

The Attempt at a Solution


I started by decomposing the resultant force on the surface of the sphere into its vertical and horizontal components, allowing me to write: ##F_V = F \sin\theta## and ##F_H = F \cos\theta##

3.1. The vertical force
So I divide the sphere into differential rings with area ##dA = 2\pi R^2 \cos\theta dθ##
If ##F_V = F \sin\theta##, then ##dF_V = dF \sin\theta##, but ##dF = p dA## and ##p = (p_0 + \gamma h)##, which yields:
$$dF_V = (p_0 + \gamma h) (2\pi R^2 \cos\theta dθ) \sin\theta$$
The point where I'm evaluating ##h## is ##h = h_1 + R - R\sin\theta##, so we have:
$$dF_V = \gamma (h_1 + R - R\sin\theta) (2\pi R^2 \cos\theta dθ) \sin\theta$$
Finally, the vertical force is given by:
$$F_V = \gamma 2\pi R^2 \left[h_1 \int_{\frac \pi 2}^{\frac {3\pi} 2} \sin\theta \cos\theta\, d\theta + R \int_{\frac \pi 2}^{\frac {3\pi} 2} \sin\theta \cos\theta\, d\theta - R \int_{\frac \pi 2}^{\frac {3\pi} 2} \sin^2\theta \cos\theta\, d\theta\right]$$
Solving the integral we have:
$$F_V = \gamma 2\pi R^2 * (2 R /3) \rightarrow F_V = \frac 4 3 \pi R^3 \gamma$$
Which I believe is the correct answer since it is the buoyancy of a sphere.

3.2 The horizontal force
As far as I know, the method for solving this should be the same as before. The only difference I can see is that the horizontal force is given by ##F_H = F \cos\theta##, so the equation is:
$$F_H = \gamma 2\pi R^2 \left[h_1 \int_{\frac \pi 2}^{\frac {3\pi} 2} \cos^2\theta\, d\theta + R \int_{\frac \pi 2}^{\frac {3\pi} 2} \cos^2\theta\, d\theta - R \int_{\frac \pi 2}^{\frac {3\pi} 2} \sin\theta \cos^2\theta\, d\theta\right]$$
Solving the above integral yields:
$$F_V = \gamma 2\pi R^2 * (h_1\frac \pi 2 + R\frac \pi 2) \rightarrow F_V = \pi^2 R^2 \gamma[h_1 + R]$$
However I am pretty sure that this is wrong. Since the whole sphere is submerged there should be forces cancelling themselves out so that the horizontal force should be just zero. Besides, this solution is in terms of ##h_1##, and my lecturer explicitly said the answer shouldn't be in therms of any variables other than ##R## and ##h_1##
 
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I suggest you redo your coordinate system and use a standard spherical with ## \theta ## being the polar angle measured from the vertical (upward z) direction and ## dA=2 \pi R^2sin(\theta) \, d \theta ## because of the ## \phi ## symmetry. The angle ## \theta ## will then vary from ## 0 ## to ## \pi ##. The vertical force is the z-component. For the horizontal force, you will need to consider the ## x ## and ## y ## components and integrate over ## \phi ##. The horizontal component will have a ## sin(\theta) ## just as the vertical has a ## cos(\theta) ##, but it is the ## \phi ## integrals that will give you the zero answer for the horizontal (x and y) components. For the vertical (z component), the integral over ## d \phi ## is just ## 2 \pi ##. For the x and y components, the ## sin(\phi) ## or ## cos(\phi) ## terms integrate to ## 0 ## when integrated from ## 0 ## to ## 2 \pi ##.
 
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Charles Link said:
I suggest you redo your coordinate system and use a standard spherical with ## \theta ## being the polar angle measured from the vertical (upward z) direction and ## dA=2 \pi R^2sin(\theta) \, d \theta ## because of the ## \phi ## symmetry. The angle ## \theta ## will then vary from ## 0 ## to ## \pi ##. The vertical force is the z-component. For the horizontal force, you will need to consider the ## x ## and ## y ## components and integrate over ## \phi ##. The horizontal component will have a ## sin(\theta) ## just as the vertical has a ## cos(\theta) ##, but it is the ## \phi ## integrals that will give you the zero answer for the horizontal (x and y) components. For the vertical (z component), the integral over ## d \phi ## is just ## 2 \pi ##. For the x and y components, the ## sin(\phi) ## or ## cos(\phi) ## terms integrate to ## 0 ## when integrated from ## 0 ## to ## 2 \pi ##.
Thank you so much for your answer, it does make sense. I didn't really think about the coordinate system before
 
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The book claims the answer is that all the magnitudes are the same because "the gravitational force on the penguin is the same". I'm having trouble understanding this. I thought the buoyant force was equal to the weight of the fluid displaced. Weight depends on mass which depends on density. Therefore, due to the differing densities the buoyant force will be different in each case? Is this incorrect?

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