I can't tell you if there is a problem or not.

The only intended difference that I can see is that for 4.5.X:

# grompp by default sets the new nsttcouple parameter equal to nstlist, this means T-coupling is done less frequently; grompp checks if tau_t is large enough # grompp by default sets the new nstpcouple parameter equal to nstlist, this means P-coupling is done less frequently; grompp checks if tau_p is large enough

(see http://www.gromacs.org/About_Gromacs/Release_Notes/Versions_4.5.x )

Note that there were some fixes to P-R scaling in the 4.0.X series -- se http://www.gromacs.org/About_Gromacs/Release_Notes/Revisions_in_4.0

To test this further, I suggest that you need to define a good procedure to ensure that what you are seeing is (b) from a well equilibrated system and is also (b) statistically significant.

I suggest that one way to do this is to cycle through your T- and P- coupling options at a given temperature. For example, at T=500 K, run X ns of Berendsen, then X ns of Parrinello-Rahman, then back to Berendsen, and so on for a few cycles. Each time you switch coupling method, be sure to use the structure output from the previous run. Also be sure that X ns is as long as you can afford. This way, you will be able to pick out systematic changes as temperature/density oscillations with periods that are related to your changes of algorithm. This also ensures that what you are seeing is not simply an artifact of having a poorly equilibrated density in your initial structure.

You could also run the same cycle with Berendsen and V-rescale.

Chris.

-- original message --

Dear gmxers,
According to my recent practice, we find that the Berensen methods for T- and P- coupling can yield reasonable averaged density as a function of temperature, but when the v-rescale method and the Parrinello-Rahman method are employed for T- and P- coupling, somewhat unexpected results (i.e. density at higher temperature is bigger than that at lower tempearature) are obtained. Generally, the latter setup is considered to be prefered to the former one in simulating realistic ensemble. I am using gmx-4.5.3, and previously I have also performed one similar work using 4.0 which can generate expected results using the latter setup. I wonder if this version 4.5.3 has some bugs in calculating T and P, and are they dealt with in 4.5.4? Please give me some hints.

 Yours sincerely,
 Chaofu Wu, Dr.
  ------------------
Department of Chemistry and Materials Science, Hunan University of Humanities, Science and Technology, Loudi 417000, the People?s Republic of China (P.R. China)
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