ASAB1
Having acquired the appropriate PDB files, it is necessary to tag each
residue as being either a surface side chain or main chain residue, or a
buried residue. Arbitrary numerical codes are assigned by the program to each
residue component i.e. 1 for surface side or main chain, 6 for buried surface
side chain, and 10 for buried main chain. The program is based on Lee and
Richards' (1971) rolling sphere algorithm to determine surface
accessibility. The steps required to run ASAB1 are listed below.
Prepare the PDB file: ASAB1 only processes information specified in the ATOM
and HETATM fields of the PDB file, terminating at the TER field. Therefore it
is preferable (but usually not necessary) to remove additional information
prior to running ASAB1, while it is mandatory to remove any intermediate TER
field for proteins containing multiple chains, otherwise ASAB1 will terminate
execution prematurely.
Running the program
Launch asab1 at the command line.
Supply information for the size of the rolling sphere probe as
requested by the program. A typical run would use a rolling sphere with
1.4 Å radius Enter the threshold value for surface accessibility
(usualy 10 Å^2).
Insert PDB filename (complete with extension).
Choose between standard output filenames or enter root filename.
The three standard output files generated by the program are named
provaly,
provaly1 and provaly2, which contain the atomic coordinates; atomic
radius,
mass and surface accessibility code; and correspondence i.e. atom name,
residue name and residue name and number. Enter the integration step
(usually 1 Å).
The number of steps appears, confirm to start operation.
ASAB1 can also be used to calculate the surface accessibility of bead
models
(option 3 - recheck), which requires a percentage value for the surface
threshold. This is essentially a ratio of exposed surface area/total
surface
area for each bead. For example, if a value of 50% is used, then the
rolling
sphere has to cover at least half the area of the sphere for it to be
tagged
as being surface accessible. Therefore higher percentage values will
result in
a greater number of buried beads. This feature is used to recompute the
surface accessible beads after SOMO generation. By using only the
surface accessible beads in the computation, the
hydrodynamic parameters for the model can be calculated much more
quickly. This should not be confused with a shell model just because it
does
not include 'buried' beads. In shell models the beads are much smaller
and
they are more closely packed along the surface. In fact, these
medium-resolution models lie somewhat between shell and low resolution
bead
models (several residues per bead), and completely excluding the buried
beads
from the computations may lead to some errors.