Change in Gravitational Potential Energy in Oscillating water mass

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SUMMARY

The discussion focuses on calculating the change in gravitational potential energy (U) of an oscillating water mass in a lake, specifically during a seiche event. The correct formula for U is established as U=(1/6)bpgL(Yo²), where b is the width of the lake, p is the density of water, g is the gravitational constant, L is the length of the lake, and Yo is the increase in water level. The key error identified in the attempted solution is the misinterpretation of the average height of the water surface, which should not include an arbitrary addition to the constant height (h).

PREREQUISITES
  • Understanding of gravitational potential energy (U=mgh)
  • Basic principles of fluid mechanics, specifically related to oscillating bodies
  • Knowledge of center of mass (COM) calculations
  • Familiarity with the concept of seiche in lakes
NEXT STEPS
  • Study the derivation of gravitational potential energy in oscillating systems
  • Learn about the principles of seiche and its effects on water bodies
  • Explore center of mass calculations in fluid dynamics
  • Investigate the relationship between water surface oscillations and energy changes
USEFUL FOR

Students in physics or engineering, particularly those studying fluid dynamics, environmental science, or anyone interested in the mechanics of oscillating water bodies.

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Homework Statement


Seiche in a lake. The simplest motion of water in a lake can be approximated as simply the water surface tilting but remaining flat.
Imagine a lake of rectangular cross section of length L and with depth h where (h<<L). The problem resembles that of the simple pendulum, the kinetic energy is due to horizontal
motion and potential energy due to small change in height.
So, imagine at some instant the water level at the increased end is +Yo with respect to normal level. Show that the increased gravitational potential energy of whole mass system is given by
U=(1/6)bpgL(Yo2)

Homework Equations


U=mgh
Figure attatched!

The Attempt at a Solution


I know the mass of the water will be defined as the volumeXdensity. the volume would be, if width of lake is defined as b, Lbh. Density is denoted p. Thus, m=Lbhp.
The gravitational constant g is applicable so g=g. Finally, as the height is rising as much as it is falling I can take the average height and thus, h = h+(1/2)Yo?
But, now plugging this into the equation U=mgh I have
U=(Lbhp)g(h+(1/2 Yo), and this is definitely not the 'answer' stated in the problem.
Could anyone help identify where is my logic going wrong?
 

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This one is deadly wrong: h = h+(1/2)Yo (h = h + something?!)
Note that h is the height from the bottom to the average level of the water surface: h = const! What is left is to find the height of the center of mass (COM). Hint: apply the formula of COM's position and express COM's height in term of Yo and D, where D is the height of the left edge of the water surface from the bottom (D is not h!). Then find the geometrical relation between D and Yo.
 

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