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of this approach is 100% sequence coverage of prote<strong>in</strong> and improved detection of post-translational modifications [9,10].<br />
It is disadvantaged for the reason it requires high field magnetic fields. The most popular and widely used approach<br />
for identify<strong>in</strong>g prote<strong>in</strong>s and determ<strong>in</strong><strong>in</strong>g details of their sequence and posttranslational modifications is the bottom-up<br />
approach [6,11]. In bottom-up approach prote<strong>in</strong>s of <strong>in</strong>terest are digested with proteolytic enzyme like tryps<strong>in</strong> and then<br />
analyzed by mass spectrometry. In First step masses of peptides are determ<strong>in</strong>ed followed by fractionation of these peptide<br />
ions for further downstream analysis. This approach is useful for identify<strong>in</strong>g prote<strong>in</strong>s because tryptic peptides solubilize<br />
and separate readily than the parent prote<strong>in</strong>s. The disadvantage with this approach is that only a small fraction of tryptic<br />
peptides are normally detected and as a result some <strong>in</strong>formation gets deleted that would be crucial <strong>in</strong> construction of<br />
what are called ‘fragmentation ladders’. Whatever the method or methods utilized to generate the data, a large set of data<br />
is generated that needs to be further analyzed to derive mean<strong>in</strong>gful <strong>in</strong>formation. Second step of mass spectrometry based<br />
prote<strong>in</strong> characterization is data analysis and <strong>in</strong>terpretation. The First step here is deduc<strong>in</strong>g am<strong>in</strong>o acid sequence from large<br />
datasets generated to be followed by peptide identity. Although many software tools exist for such analysis nevertheless<br />
they are deemed to be <strong>in</strong> need of more accuracy and consistency to reduce results from data redundancy. Of late there has<br />
been an emphasis on <strong>in</strong>tegrat<strong>in</strong>g <strong>in</strong>formation from bio<strong>in</strong>formatics with results that come from proteomics experiments.<br />
Three major prote<strong>in</strong> databases SWISS-PROT, TrEMBL and NCBI have been successful <strong>in</strong> achiev<strong>in</strong>g the goals of ability to<br />
store, allow search<strong>in</strong>g and retriev<strong>in</strong>g <strong>in</strong>formation generated from proteomics [12]. A statistical analysis of the results is an<br />
important consideration to ensure confidence <strong>in</strong> the outcomes [7].<br />
Sedimentation<br />
Sedimentation as the term implies is ability of suspended particles to settle dur<strong>in</strong>g course of motion as a consequence<br />
of effect of different operational forces <strong>in</strong> sediment<strong>in</strong>g solution. Prote<strong>in</strong>s like other macromolecules can also undergo<br />
sedimentation and this ability of prote<strong>in</strong>s to settle <strong>in</strong> solution has been exploited <strong>in</strong> their characterization through use of<br />
analytical ultracentrifugation (AUC).<br />
In analytical ultracentrifugation prote<strong>in</strong> solutions to be studied are subjected to a high gravitational field and result<strong>in</strong>g<br />
changes <strong>in</strong> concentration distribution are monitored <strong>in</strong> real time us<strong>in</strong>g various optical methods. The optical systems that<br />
are currently available for analytical ultracentrifuges <strong>in</strong>clude absorbance, fluorescence and <strong>in</strong>terference [13,14]. Although<br />
analytical ultracentrifugation places few restrictions on the sample and nature of solvent, there are few fundamental<br />
requirements; (i) That sample has a differentiable or dist<strong>in</strong>guish<strong>in</strong>g optical property, (ii) It sediments or floats at an<br />
gravitational field that is achievable experimentally and (iii) that it is chemically compatible with the sample cell [13]. The<br />
molecular weights that are suitable for AUC vary from between hundred Daltons like peptides, oligosaccharides to million<br />
Daltons like viruses and cellular organelles.<br />
Sedimentation dur<strong>in</strong>g ultracentrifugation can be considered as an outcome of three forces [2,13-16]. The centrifugal<br />
force that a prote<strong>in</strong> molecule experiences because of sp<strong>in</strong>n<strong>in</strong>g is M p<br />
ω 2 r, where M p<br />
is mass of prote<strong>in</strong>, ω is rotor speed <strong>in</strong><br />
radians/sec (ω=2π*rpm/60) and r is the distance from centre of rotor. A counter force M s<br />
ω 2 r exerted on prote<strong>in</strong> molecule<br />
is generated by mass M s<br />
of the solvent displaced as the prote<strong>in</strong> molecule sediments. The mass of solvent that is displaced<br />
equals Mp * v * ρ, where v is partial specific volume (<strong>in</strong> cm 3 /g) of the particle and ρ (<strong>in</strong> g/cm 3 ) is density of the solvent.<br />
Therefore the effective buoyant mass M b<br />
of prote<strong>in</strong> molecule equals M p<br />
(1- v ρ). The net force (M p<br />
-M s<br />
)ω 2 r or M p<br />
(1- v ρ)ω 2 r<br />
contributes to the overall viscous drag of prote<strong>in</strong> molecule undergo<strong>in</strong>g sedimentation. This gets balanced by a frictional<br />
force. This frictional force is represented by fv, where f is the frictional coefficient and v is the velocity. A net outcome will<br />
be molecule mov<strong>in</strong>g at a velocity that is bare enough to make the total force equivalent to zero.<br />
M p<br />
(1- v ρ) ω 2 r – fv = 0 (4)<br />
Multiply<strong>in</strong>g equation 4 by Avogadro’s number (NA) to put entities on molar basis and rearrang<strong>in</strong>g to place molecular<br />
parameters on one side of equation and experimentally measured ones on other we get<br />
Mp( 1−<br />
vρ<br />
) v<br />
NA*<br />
= = s<br />
2<br />
(5)<br />
f ω r<br />
This velocity divided by centrifugal field strength is called sedimentation coefficient, s. Units of s are ‘second’ and values<br />
of 10 -13 are commonly encountered, the quantity of 1*10 -13 sec has been called 1 Svedberg. Svedberg is named after T.<br />
Svedberg a pioneer <strong>in</strong> sedimentation analysis. Sedimentation coefficient is directly proportional to molecular weight and<br />
<strong>in</strong>versely proportional to frictional coefficient and is experimentally measurable as ratio of velocity to field strength. It can<br />
be presumed that sedimentation coefficient will <strong>in</strong>crease with <strong>in</strong>creas<strong>in</strong>g molecular weight; however it also depends on<br />
friction f, which <strong>in</strong> turn depends on size, shape and hydration of a prote<strong>in</strong> molecule.<br />
Application: As expla<strong>in</strong>ed above analytical ultracentrifugation (AUC) relies on properties of mass and fundamental<br />
laws of gravitation, it has therefore diverse applicability. Also dur<strong>in</strong>g analytical centrifugation prote<strong>in</strong> samples can be<br />
characterized <strong>in</strong> their native state and under physiologically and biologically relevant solution conditions. AUC can<br />
deliver <strong>in</strong>formation about two aspects of solution behavior; hydrodynamic and thermodynamic [2,13-15,17]. Information<br />
about hydrodynamic properties like size and shape of prote<strong>in</strong> molecules is deduced from sedimentation velocity while<br />
as <strong>in</strong>formation about thermodynamic properties like molar mass, stoichiometry and association constant comes from<br />
sedimentation equilibrium.<br />
Sedimentation equilibrium is a more effective method for determ<strong>in</strong>ation of molecular mass as well as one of the effective<br />
methods for characterization of macromolecular <strong>in</strong>teractions. This is for reasons that sedimentation equilibrium estimations<br />
are not dependent upon macromolecular shape and the reaction k<strong>in</strong>etics are not part of data analysis [15]. In sedimentation<br />
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