Calculating sedimentation coefficient distributions by direct modeling of sedimentation velocity concentration profiles.
نویسندگان
چکیده
The c(s) method results in high-resolution sedimentation coefficient distributions by deconvoluting the effects of diffusion broadening. It is a direct model for sedimentation data covering the complete sedimentation process, based on finite element solutions of the Lamm equation, and algebraically accounts for the systematic noise structure encountered in transport experiments. A continuous sedimentation coefficient distribution is expressed via a Fredholm integral equation and solved using maximum entropy regularization. The extent of diffusion for each species is approximated by hydrodynamic considerations and parameterized with a weight-average frictional ratio of the protein mixture under study. In addition to the sedimentation coefficient distribution, c(s) can be used to estimate protein molar mass, detect trace components of protein aggregates as well as other small and large molar mass impurities, and series of c(s) distributions obtained at different protein concentrations can be used for the study of homogeneous and heterogeneous protein interactions. The present paper provides an overview of the strategy and numerical approaches of the c(s) method, including special cases useful for certain protein studies, briefly discusses experimental requirements, and illustrates the main types of applications to noninteracting and interacting protein systems.
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ورودعنوان ژورنال:
- Methods in enzymology
دوره 384 شماره
صفحات -
تاریخ انتشار 2004