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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 />

OMICS Group eBooks<br />

06

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