- #1
curious_being
- 3
- 1
I am struggling to understand shocks in a one dimensional lattice with a linear spring connecting the masses. Say I have a one dimensional lattice with a linear spring constant, k and lattice spacing a. If the particles in the lattice has mass, m then my speed of sound c is a*sqrt(k/m). That is a small disturbance will propagate with speed c. Now if I move one of the end particles in my lattice at a speed greater than c, I should incite a shockwave? Will the dynamics then be governed by the Hugoniot relations?
I guess my confusion is as to how a shock forms if the system is linear... If it is a linear sound wave, the pressure distribution or the structure of the wave propagates unperturbed. If the interaction between granules is non-linear, I see how the structure of the wave eventually becomes a shock wave as the wavefront gets squished as larger loadings will propagate faster.
Back to the linear system, how does the linear interaction bring about a nonlinear compressibility to generate a shock front if k doesn't change...? I think the density behind the front will increase linearly but I don't know how to relate all the state variables let alone know how to derive an EOS for a linear lattice.
Much help would be greatly appreciated!
I guess my confusion is as to how a shock forms if the system is linear... If it is a linear sound wave, the pressure distribution or the structure of the wave propagates unperturbed. If the interaction between granules is non-linear, I see how the structure of the wave eventually becomes a shock wave as the wavefront gets squished as larger loadings will propagate faster.
Back to the linear system, how does the linear interaction bring about a nonlinear compressibility to generate a shock front if k doesn't change...? I think the density behind the front will increase linearly but I don't know how to relate all the state variables let alone know how to derive an EOS for a linear lattice.
Much help would be greatly appreciated!