Dear Gromacs users,
I have a question related to the use of g_rdf for the calculation of
hydration of a lipid bilayer patch. I used g_rdf with -surf flag (I
tried both mol and res) and two index groups: the oxygens of waters as
first group and the atoms of the headgroups as second group. I used
the above hoping to calculate the distribution of water molecules
around lipid headgroups with the distance calculated from the closest
headgroup atom to each water and counted only once. The resulting
graph does not have the two large and one small hydration peaks
followed by the plateau as expected, but instead has two tiny peaks
and then behaves as increasing function with distance. The hydration
profile of the polar components of the bilayer alltogether is almost
identical to the hydration of a single lipid that I calculated in a
similar manner, which doesn't make sense to me.
In addition to that, the number of oxygens in each one of the 1500
bins (I used the default number of bins) is in average around 1000,
while the number of water molecules in my system is only 6070. This
means that somehow there exists a "degeneracy" in the calculation of
distances.
Is it possible that the problem is correlated to the lack of normalization?
So what does g_rdf calculate in my case? Is there a way with or
without g_rdf to obtain the hydration profile, as well as integration
of the latter up to a distance that I could subsequently decide based
on the results?
Thank you in advance.
Best regards,
Ioannis
--
gmx-users mailing list [email protected]
http://lists.gromacs.org/mailman/listinfo/gmx-users
Please search the archive at
http://www.gromacs.org/Support/Mailing_Lists/Search before posting!
Please don't post (un)subscribe requests to the list. Use the
www interface or send it to [email protected].
Can't post? Read http://www.gromacs.org/Support/Mailing_Lists
