Equations are solved with dense grids
- Potential has a general form of
$ax^{2}+bx^{4}$ - While negative
$a$ corresponds to a double-well potential, the single well potential with a positive$a$ can also be solved
- Potential has a general form of
$V(x)=D_{e}(e^{-2\alpha(x-x_{e})}-2e^{-\alpha(x-x_{e})})$ - This is not a symmetric potential. The local minima of excited state CMES need to be searched before calculating frequencies.
Instead of dense grids with finite difference method, now the Fourier grid method is used
- The 2D potential has a general form of:
$V(x,y)=a_{x}x^{2}+a_{y}y^{2}+b_{x}x^{4}+b_{y}y^{4}+c_{xy}xy+c_{x^{2}y}x^{2}y$ - Unless
$c_{x^{2}y}= 0$ , this is also not a symmetric potential. The local minima of excited state CMES need to be searched before calculating frequencies - "surface_generator" file will provide 9 points for local hessian matrix calculation