Water molecule bond length: Difference between revisions
From wikiluntti
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=== Newton Equations === | === Newton Equations === | ||
<math>F = ma</math> where <math>F = - \nabla V</math>. | <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>. | ||
=== Integration === | === Integration === | ||
Line 19: | Line 20: | ||
<math> | <math> | ||
a(t) = \frac{ | a(t) = -\frac{\frac{d}{dx}(V(t))}{m} | ||
</math> | </math> | ||
=== Potential Function === | |||
[https://en.wikipedia.org/wiki/Lennard-Jones_potential Lennard--Jones potential] with parameters for [https://en.wikipedia.org/wiki/Water_model TIPS] model: | |||
<math> | <math> | ||
\begin{align} | \begin{align} | ||
A &= 580.0 \times 10^3 kcal A^{12}/mol \\ | |||
B &= 525.0 kcal A^6/mol | |||
\end{align} | \end{align} | ||
</math> | </math> | ||
where <math>A</math> is Ångströms. | |||
==== 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> | ||
=== Temperature/ Initial distribution === | === Temperature/ Initial distribution === |
Revision as of 22:42, 12 October 2020
Introduction
Classical Mechanics
Newton Equations
where . The system is 1D, thus gradient will be differential, and .
Integration
The finite differences (Euler method) are
and
Potential Function
Lennard--Jones potential with parameters for TIPS model:
where is Ångströms.
Velocity Verlet Algorithm
A very good and easy to implement integration method is velocity Verlet:
Temperature/ Initial distribution
The initial velocity of the hydrogen atom is chosen randomly from the Maxwell-Boltzmann distribution at given temperature
Results
Issues
1D statement