330 8.2 Molecular Simulation Methods
KEY POINT 8.4
A set of two paired electrons with opposite spins in an outer atomic orbital are
considered a lone pair if they are not involved in a chemical bond. In the water mol
ecule, the oxygen atom in principle has two such lone pairs, which act as electronega
tive sources facilitating the formation of hydrogen bonds and accounting for the fact
that bond angle between the two hydrogen atoms and oxygen in a water molecule is
greater than 90° (and in fact is closer to 104.5°).
To limit excessive computational demands on using an explicit solvent, periodic boundary
conditions (PBCs) are imposed. This means that the simulation occurs within a finite, geo
metrically well-defined volume, and if the predicted trajectory of a given water molecule
takes it beyond the boundary of the volume, it is forced to reemerge somewhere on the
other side of the boundary, for example, through the point on the other side of the volume
boundary that intersects with a line drawn between the position at which the water molecule
moved originally beyond the boundary and the geometrical centroid of the finite volume, for
example, if the simulation was inside a 3D cube, then the 2D projection of this might show a
square face, with the water molecule traveling to one edge of the square but then reemerging
on the opposite edge. PBCs permit the modeling of large systems, though they impose spatial
periodicity where there is none in the natural system.
The minimum size of the confining volume of water surrounding the biomolecule needs
must be such that it encapsulates the solvation shell (also known as the solvation sphere,
also as the hydration layer or hydration shell in the specific case of a water solvent). This is
the layer of water molecules that forms around the surface of biomolecules, primarily due to
hydrogen bonding between water molecules. However, multiple layers of water molecules
can then form through additional hydrogen bond interactions with the primary layer water
molecules. The effects of a solvent shell can extend to ~1 nm away from the biomolecule
surface, such that the mobility of the water molecules in this zone is distinctly lower than
that exhibited in the bulk of the solution, though in some cases, this zone can extend beyond
2 nm. The time scale of mixing between this zone and the bulk solution is in the range 10−15
to 10−12 s and so simulations may need to extend to at least these time scales to allow adequate
mixing than if performed in a vacuum. The primary hydration shell method used in classical
MD with explicit solvent assumes two to three layers of water molecules and is reasonably
accurate.
An implicit solvent uses a continuum model to account for the presence of water. This
is far less costly computationally than using an explicit solvent but cannot account for any
explicit interactions between the solvent and solute (i.e., between the biomolecule and any
specific water molecule). In its very simplest form, the biomolecule is assumed only to interact
only with itself, but the electrostatic interactions are modified to account for the solvent by
assuming the value of the relative dielectric permittivity term εr in the Coulomb potential. For
example, in a vacuum, εr = 1, whereas in water εr ≈ 80.
If the straight-line joining atoms for a pairwise interaction are through the structure of
the biomolecule itself, with no accessible water present, then the relative dielectric permit
tivity for the biomolecule itself should be used, for example, for proteins and phospholipid
bilayers, εr can be in the range ~2–4, and nucleic acids ~8; however, there can be consider
able variation deepening on specific composition (e.g., some proteins have εr ≈ 20). This very
simple implicit solvation model using a pure water solvent is justified in cases where the PMF
results in a good approximation to the average behavior of many dynamic water molecules.
However, this approximation can be poor in regions close to the biomolecule such as the
solvent shell, or in discrete hydration pockets of biomolecules, which almost all molecules in
practice have, such as in the interiors of proteins and phospholipid membranes.
The simplest formulation for an implicit solvent that contains dissolved ions is the
generalized Born (or simply GB) approximation. GB is semiheuristic (which is a polite way of
saying that it only has a physically explicable basis in certain limiting regimes), but which still