Water molecule bond length: Difference between revisions
(16 intermediate revisions by the same user not shown) | |||
Line 4: | Line 4: | ||
=== Newton Equations === | === Newton Equations === | ||
<math>F = ma</math> where <math>F = - \nabla V</math>. The system is 1D, thus gradient will be differential, and <math>F= - \frac{d V}{dx}</math>. | |||
The mass <math>m</math> should be the [https://en.wikipedia.org/wiki/Reduced_mass reduced mass] of the oxygen--hydrogen system, but we use mass <math>m=1</math> here. | |||
=== Potential Function === | |||
[https://en.wikipedia.org/wiki/Lennard-Jones_potential Lennard--Jones potential] with dimensionless parameters for [https://en.wikipedia.org/wiki/Water_model TIPS] model: | |||
<math> | |||
V(x) = 4 \left[ \left( \frac1x\right)^{12} - \left( \frac1 x\right)^6 \right] | |||
</math> | |||
where the distance <math>x</math> is given in Ångstroms. | |||
=== Integration === | === Integration === | ||
=== | The finite differences (Euler method) are | ||
<math> | |||
\begin{align} | |||
v(t) &= \frac{x(t+\Delta t) - x(t)}{\Delta t} \\ | |||
a(t) &= \frac{v(t+\Delta t) - v(t)}{\Delta t} | |||
\end{align} | |||
</math> | |||
and | |||
<math> | |||
a(t) = -\frac{\frac{d}{dx}(V(x(t)))}{m} | |||
</math> | |||
=== Velocity Verlet Algorithm === | |||
A very good and easy to implement integration method is velocity Verlet: | |||
<math> | <math> | ||
\begin{align | \begin{align} | ||
x(t + \Delta t) &= x(t) + v(t) \Delta t + \frac12 a \Delta t^2 \\ | |||
v(t + \Delta t) &= v(t) + \frac12\left( a(t) + a(t+\Delta t) \right) \Delta t | |||
\end{align | \end{align} | ||
</math> | </math> | ||
where <math> | |||
where <math>a(t) = a(x(t)) = - \frac1m \frac{d}{dx}V(x(t))</math> is given at Section . . . | |||
=== Temperature/ Initial distribution === | === Temperature/ Initial distribution === | ||
Line 27: | Line 57: | ||
\exp\left[- \frac12 \frac{mv^2}{k_B T} \right] | \exp\left[- \frac12 \frac{mv^2}{k_B T} \right] | ||
</math> | </math> | ||
The mean speed (for 3d?) is | |||
<math> | |||
v_\text{mean} = \sqrt{\frac{8k_B T}{\pi m}} | |||
</math> | |||
where <math>k_B</math> is Boltzmann constant, here <math>k_B = 1</math>. | |||
== Results == | == Results == | ||
Line 33: | Line 71: | ||
1D statement | 1D statement | ||
== References == | |||
D.T.W. Lin and C.-K. Chen: A molecular dynamics simulation of TIP4P and Lennard-Jones water in nanochannel, acta Mechanica 173, 181.194 (2004). |
Latest revision as of 23:12, 12 October 2020
Introduction
Classical Mechanics
Newton Equations
where . The system is 1D, thus gradient will be differential, and .
The mass should be the reduced mass of the oxygen--hydrogen system, but we use mass here.
Potential Function
Lennard--Jones potential with dimensionless parameters for TIPS model:
where the distance is given in Ångstroms.
Integration
The finite differences (Euler method) are
and
Velocity Verlet Algorithm
A very good and easy to implement integration method is velocity Verlet:
where is given at Section . . .
Temperature/ Initial distribution
The initial velocity of the hydrogen atom is chosen randomly from the Maxwell-Boltzmann distribution at given temperature
The mean speed (for 3d?) is
where is Boltzmann constant, here .
Results
Issues
1D statement
References
D.T.W. Lin and C.-K. Chen: A molecular dynamics simulation of TIP4P and Lennard-Jones water in nanochannel, acta Mechanica 173, 181.194 (2004).