This looks like the simplest oscillating system ever,
md2xdt2=−2mc2ln(cosh(G√2mc2x))+ψd
d2xdt2=−2c2ln(cosh(G√2mc2x))+ψdm
Compared to,
md2xdt2=−kx
it is not linear. So, consider,
(2mc2ln(cosh(G√2mc2x)))′=c√2mG.tanh(G√2mc2x)
limx→largec√2mG.tanh(G√2mc2x)=c√2mG
Then we have,
md2xdt2=−c√2mG.x+ψd
and so, the approximate natural oscillating frequency is,
fosc=√c√2mGm=(2m)1/4√cG
where m is the mass density of the particle and G is the constant of integration from solving Fρ. c is the speed of light.
(fosc)4=2c2G2m
It is expected that since the lower gradient values are less than or equal to the approximate value, as we let x→large, the actual oscillation frequencies given a large population of particles, spread to higher values of fosc. In other words, blue.