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Temperature%20and%20pressure%20coupling

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Title: Temperature%20and%20pressure%20coupling


1
Temperature and pressure coupling
  • MD workshops
  • 26-10-2004

2
Why control the temperature and pressure?
  • isothermal and isobaric simulations (NPT) are
    most relevant to experimental data
  • constant NPT ensemble constant number of
    particles, pressure, and temperature

3
Causes of temperature and pressure fluctuations
  • the temperature and pressure of a system tends to
    drift due to several factors
  • drift as a result of integration errors
  • drift during equilibration
  • heating due to frictional forces
  • heating due to external forces

4
Temperature coupling methods in GROMACS
  • weak coupling
  • exponential relaxation Berendsen
    temperature coupling (Berendsen, 1984)
  • extended system coupling
  • oscillatory relaxation Nosé-Hoover
    temperature coupling (Nosé, 1984 Hoover, 1985)

5
Berendsen temperature coupling
  • there is weak coupling to an external heat bath
  • deviation of system from a reference temperature
    To is corrected
  • exponential decay of temperature deviation

6
  • the temperature of a system is related to its
    kinetic energy, therefore, the temperature can
    be easily altered by scaling the velocities vi by
    a factor ?
  • is the temperature coupling time constant
  • need to specify in input file (.mdp file)

7
Some notes on Berendsen weak coupling algorithm
  • very efficient for relaxing a system to the
    target temperature
  • prolonged temperature differences of the separate
    components leads to a phenomenon called
    hot-solvent, cold-solute, even though the
    overall temperature is at the correct value
  • Solutions
  • apply temperature coupling separately to the
    solute and to the solvent problem with
    unequal distribution of energy between the
    different components

8
solutions continued
  • stochastic collisions (Anderson, 1980)
  • - a random particles velocity is reassigned by
    random selection from the Maxwell-Boltzmann
    distribution at set intervals does not
    generate a smooth trajectory, less realistic
    dynamics
  • extended system (Nosé, 1984 Hoover 1985)
  • - the thermal reservoir is considered an
    integral part of the system and it is represented
    by an additional degree of freedom s
  • - used in GROMACS

9
Nosé-Hoover extended system
  • canonical ensemble (NVT)
  • more gentle than Anderson where particles
    suddenly gain new random velocities
  • the Hamiltonian is extended by including a
    thermal reservoir term s and a friction parameter
    ?, in the equations of motion
  • H K V Ks Vs

10
Nosé-Hoover extended system
  • The particles equation of motion
  • ? is a dynamic quantity with its own equation of
    motion
  • is proportional to the temperature coupling
    time constant (specified in .mdp file)

11
  • the strength of coupling between the reservoir
    and the system is determined by
  • - when is too high slow energy
    flow between system and reservoir
  • - when is too low rapid
    temperature fluctuations

12
  • Nosé-Hoover produces an oscillatory relaxation,
    it takes several times longer to relax with
    Nosé-Hoover coupling than with weak coupling
  • can use Berendsen weak coupling for equilibration
    to reach desired target, then switch to
    Nosé-Hoover
  • Nosé-Hoover chain the Nose-Hoover thermostat is
    coupled to another thermostat or a chain of
    thermostats and each are allowed to fluctuate

13
Pressure coupling
  • The system can be coupled to a pressure bath as
    in temperature coupling
  • weak coupling
  • exponential relaxation Berendsen pressure
    coupling
  • extended ensemble coupling
  • oscillatory relaxation Parrinello-Rahman
    pressure coupling (Parrinello and Rahman, 1980,
    1981, 1982)

14
Berendsen pressure coupling
  • equations of motion are modified with a
  • first order relaxation of P towards a
    reference Po
  • rescaling the edges and the atomic coordinates ri
    at each step by a factor u leads to volume change
  • u is proportional to ß which is the isothermal
    compressibility of the system and which is the
    pressure coupling time constant. Both values
    must be specified in .mdp file

15
  • Berendsen scaling can be done
  • 1. isotropically scaling factor is equal for
    all three directions i.e. in water
  • 2. semi-isotropically where the x/y directions
    are scaled independently from the z direction
    i.e. lipid bilayer
  • 3. anisotropically scaling factor is
    calculated independently for each of the three
    axes

16
Parrinello-Rahman pressure coupling
  • volume and shape are allowed to fluctuate
  • extra degree of freedom added, similar to
    Nosé-Hoover temperature coupling, the Hamiltonian
    is extended
  • box vectors and W-1 are functions of M
  • W-1 determines the strength of coupling
  • have to provide ß and
  • in the input file (.mdp file)

17
  • if your system is far from equilibrium, it may be
    best to use weak coupling (Berendsen) to reach
    target pressure and then switch to
    Parrinello-Rahman as in temperature coupling
  • in most cases the Parrinello-Rahman barostat is
    combined with the Nosé-Hoover thermostat
  • the extended methods are more difficult to
    program but safer

18
Weak coupling in .mdp file
  • OPTIONS FOR WEAK COUPLING ALGORITHMS
  • Temperature coupling
  • tcoupl berendsen
  • Groups to couple separately
  • tc-grps Protein SOL_Na
  • Time constant (ps) and reference temperature
    (K)
  • tau-t 0.1 0.1
  • ref-t 300 300
  • Pressure coupling
  • Pcoupl berendsen
  • Pcoupltype isotropic
  • Time constant (ps), compressibility (1/bar) and
    reference P (bar)
  • tau-p 1.0
  • compressibility 4.5E-5
  • ref-p 1.0

19
Extended system coupling in .mdp file
  • OPTIONS FOR WEAK COUPLING ALGORITHMS
  • Temperature coupling
  • tcoupl nose-hoover
  • Groups to couple separately
  • tc-grps PROTEIN SOL_Na
  • Time constant (ps) and reference temperature
    (K)
  • tau-t 0.5 0.5
  • ref-t 300 300
  • Pressure coupling
  • Pcoupl parrinello-rahman
  • Pcoupltype isotropic
  • Time constant (ps), compressibility (1/bar) and
    reference P (bar)
  • tau-p 5.0
  • compressibility 4.5E-5
  • ref-p 1.0

20
References
  • Berendsen, H.J.C., Postma, J.P.M., DiNola, A.,
    Haak, J.R. Molecular dynamics with coupling to an
    external bath. J. Chem. Phys. 813684-3690, 1984
  • Nosé, S. A molecular dynamics method for
    simulations in the canonical ensemble. Mol.
    Phys. 52255-268, 1984
  • Hoover, W.G. Canonical dynamics equilibrium
    phase-space distributions. Phys. Rev. A
    311695-1697, 1985
  • Berendsen, H.J.C. Transport properties computed
    by linear response through weak coupling to a
    bath. In Computer Simulations in Material
    Science. Meyer, M., Pontikis, V. eds. Kluwer
    1991, 139-155
  • Parrinello, M., Rahman, A. Polymorphic
    transitions in single crystals A new molecular
    dynamics method. J. Appl. Phys. 527182-7190,
    1981
  • Nosé, S., Klein, M.L. Constant pressure molecular
    dynamics for molecular systems. Mol. Phys. 50
    1055-1076, 1983

21
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