(adsbygoogle = window.adsbygoogle || []).push({}); 1. The problem statement, all variables and given/known data

In a shallow layer of water, the velocity of water in the z direction may be ignored and is therefore [tex](\dot{x},\dot{y})[/tex]. We can define the Lagrangian coordinates such that the depth of water h is satisfied by the relations

Given that [tex]h = \frac{1}{\alpha}[/tex] and [tex]\alpha = \frac{\partial(x,y)}{\partial(a,b)}[/tex]

and the Lagrangian density is given as

[tex]L = \frac{1}{2}\dot{x}^2 + \frac{1}{2}\dot{y}^2 - \frac{1}{2}gh(x_a,x_b,y_a,y_b)[/tex]

where [tex]p_q = \frac{\partial p}{\partial q}[/tex].

Given further that Lagrange's equations for a 2D continuous system are known to be

[tex]

\frac{D}{Dt}\left( \frac{\partial L}{\partial\dot{x}} \right) + \frac{\partial}{\partial a} \left( \frac{\partial L}{\partial x_a} \right) + \frac{\partial}{\partial b} \left( \frac{\partial L}{\partial x_b} \right) - \frac{\partial L}{\partial x} = 0

[/tex]

with a similar equation for the y variable, prove that

[tex] \frac{D\dot{x}}{Dt} + g \frac{\partial h}{\partial x} = 0 [/tex]

2. Relevant equations

I know the general approach of this problem, but my main problem comes in substituting

[tex] \frac{\partial}{\partial a} \frac{\partial L}{\partial x_a} [/tex].

If I apply chain rule on the Lagrangian here,

[tex] \frac{\partial}{\partial a} \frac{\partial L}{\partial h} \frac{\partial h}{\partial x_a} = -\frac{g}{2} \frac{\partial}{\partial a} \frac{\partial h}{\partial x_a} [/tex]

How do I proceed after this point?

**Physics Forums - The Fusion of Science and Community**

# Shallow water Lagrangian

Know someone interested in this topic? Share a link to this question via email,
Google+,
Twitter, or
Facebook

- Similar discussions for: Shallow water Lagrangian

Loading...

**Physics Forums - The Fusion of Science and Community**