[RASMB] New UltraScan release
Borries Demeler
demeler at biochem.uthscsa.edu
Tue Mar 16 11:52:22 PDT 2010
Dear Colleagues,
I am happy to announce a new release of UltraScan 9.9 (release ver. 1100).
The new release contains a number of bug fixes and feature enhancements,
most notably in the US-SOMO module, which are further described below.
UltraScan is free and open source, and source code and binaries for Linux,
Macintosh and Microsoft windows (XP, Vista, Windows 7) can be obtained
from our website: http://www.ultrascan.uthscsa.edu
(please note installation comment for Windows 7 on the download page).
Best regards, -Borries
P.S. We will teach a workshop on UltraScan and SOMO bead modeling on
June 4-8 in San Antonio. Registration information at:
http://www.ultrascan.uthscsa.edu/workshop/
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This new US-SOMO release contains a number of major improvements
and bug-fixes. Within the rigid-body hydrodynamics framework, this
can be considered a fully functional release producing reliable,
publication-quality parameters, especially for what concerns translational
diffusion properties. Using the direct correspondence method (SoMo)
method, an accuracy within ±2% should be expected for the calculation
of the translational diffusion coefficient of rigid biomacromolecules
for which all residues/atoms are present and are properly defined in the
somo.residue table. As for the sedimentation coefficient, its accuracy
depends also on the partial specific volume; our tests indicate that
an experimental value is advisable, as it produces more consistent
results, usually within ±3%, while the accuracy decreases to within
±5% using computed psv values. The rotational diffusion and intrinsic
viscosity accuracies are more difficult to evaluate, given the greater
uncertainties in the experimental data, but can be expected between
±5-10%. Further work is in progress to improve these computations,
which are heavily dependent on the volume correction used.
New features and improvements:
1-The AtoB (Grid) method is now also fully functional, and performs as well
as the direct correspondence method, especially at high grid resolution
(3-5 A). The improvements have been made possible by the assignment of the
theoretically-bound water of hydration at the atom level instead than at
the residue level (see point 2), and by the installment of a screening
procedure distinguishing exposed from buried beads before overlap
reduction, allowing the outward translation of the exposed beads.
2-The somo.residue editor allows the definition the water of hydration at
the atom level within each residue, which can, however, be bypassed to
assign a global residue value. In the somo.residue table distributed with
this version, the atomic hydration has been already defined for the amino
acid residues only, while global residue hydration values are defined for
all other residues. We will post updated somo.residue tables when they will
become available. Users are also encouraged to send us any somo.residue
tables containing new residue or changes in residues properties that they
might have developed.
3-US-SOMO can now fully process PBD files with missing atoms within coded
residues or with non-coded residues, using the PDB parsing options
provided. This should allow for a quick, although potentially less
accurate, evaluation of the hydrodynamic parameters of such files. BE AWARE
THAT FOR ACCURATE HYDRODYNAMIC COMPUTATIONS, ALL ATOMS PRESENT IN SOLUTION
SHOULD BE REPRESENTED IN THE ATOMIC STRUCTURE!
4-The thermodynamic conditions (solvent temperature, viscosity, and
density) at which the parameters are computed can now be changed at will in
the Hydrodynamic Computations Options panel (the default is still water @
20 °C). A buffer name and acronym can be entered as well, and printed in
the output files. The partial specific volume is also corrected for the
chosen temperature, but the value stored in the bead model files is ALWAYS
that at 20 °C.
5-The computed parameters can now be optionally saved in a comma-separated
format in an additional file, for easy importing into spreadsheets. The
parameters to be saved can be chosen from a dedicated menu.
6-A batch mode processing capability has been implemented, allowing the
uploading of multiple files and their unattended processing. The files can
be either PDB or previously-generated bead models. The batch module
pre-screens the files to verify that they comply with the current settings
(completeness and coding of residues, overlaps in bead models), prompting
for corrective action to be taken, if necessary. Batch loading also permits
the computation of the average parameters of the models, something that
previously was available only for NMR-style PDB files.
7-The SAXS/SANS module is still under development, but the P(r) vs. r
computation is already operational. For PDB files, three options are
offered, Raw (simple computation of the pairwise distance between the
atoms), SAXS (weighted by the number of electrons in each atom), and SANS
(weighted by the neutron scattering lengths of the atoms at the set D2O
fraction). For bead models, only the Raw calculation is currently
implemented. Absolute and normalized P8r) values are computed, and stored
in a single file.
Important bug fixes:
1-The water density and viscosity at 20 °C values, Avogadro's number
and Boltzmann's constant used in the previous US-SOMO releases had
slightly different values from the current accepted values, used elsewhere
in UltraScan. While this resulted in relatively minor errors in the
hydrodynamic parameters computations (<1%), this has now been fixed. The
water density viscosity at 20 °C values can nevertheless be changed at will
in the Hydrodynamic Calculations options panel, while Avogadro's number and
Boltzmann's constant can be accessed from the main UltraScan menu.
2-Precision/rounding issues in the MW calculations produced slightly
different MW values when different bead generation options were used
(especially using the Grid procedure). This has now been fixed.
Final note: most improvements/additions in the new release are described
and tested in a paper in press (Brookes et al., Macromol. Biosci.)
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