I've been using SIESTA (with VIBRA) lately to calculate the vibrational
frequencies of brucite (Mg(OH)2) at the gamma point. When I compare the
results with some I have using CRYSTAL06, not only are some of the
frequencies very different, but there is no degeneracy in the SIESTA
calculations (see below)


MODE       SIESTA              CRYSTAL06
   1            -0.0842                 -6.8266
   2             0.0296                 -1.2079
   3             0.0517                 -1.2079
   4           291.9689               309.1325
   5           293.0351               309.1325
   6           334.8122               326.3867
   7           338.7810               326.3867
   8           415.6654               405.3074
   9           475.6206               405.3074
   10         643.3266               483.2689
   11         644.7176               500.6947
   12         917.5655               994.5470
   13         924.3611               994.5470
   14        3395.2587             3514.1542
   15        3469.0307             3611.5673


While some are very near degenerate, others have > 10% splitting, which
seems very large to me despite the fact that SIESTA does not use symmetry. I
have used atomic displacements of .04, .004, and .001 with only very little
change in results.

I have attached my .fdf's for both SIESTA and VIBRA. Are these discrepancies
due to my misuse or is this a numerical inevitability in SIESTA?

Does anyone have any advice?

Thanks,
Ben

Attachment: bru_vib.fdf
Description: Binary data

Attachment: bru_vib-siesta.fdf
Description: Binary data

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