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通过沉降速度分析超离心法分析蛋白质自缔合作用

On the analysis of protein self-association by sedimentation velocity analytical ultracentrifugation.

作者信息

Schuck Peter

机构信息

Protein Biophysics Resource, Division of Bioengineering and Physical Science, ORS, OD, National Institutes of Health, Bethesda, MD 20892, USA.

出版信息

Anal Biochem. 2003 Sep 1;320(1):104-24. doi: 10.1016/s0003-2697(03)00289-6.

Abstract

Analytical ultracentrifugation is one of the classical techniques for the study of protein interactions and protein self-association. Recent instrumental and computational developments have significantly enhanced this methodology. In this paper, new tools for the analysis of protein self-association by sedimentation velocity are developed, their statistical properties are examined, and considerations for optimal experimental design are discussed. A traditional strategy is the analysis of the isotherm of weight-average sedimentation coefficients s(w) as a function of protein concentration. From theoretical considerations, it is shown that integration of any differential sedimentation coefficient distribution c(s), ls-g()(s), or g(s()) can give a thermodynamically well-defined isotherm, as long as it provides a good model for the sedimentation profiles. To test this condition for the g(s(*)) distribution, a back-transform into the original data space is proposed. Deconvoluting diffusion in the sedimentation coefficient distribution c(s) can be advantageous to identify species that do not participate in the association. Because of the large number of scans that can be analyzed in the c(s) approach, its s(w) values are very precise and allow extension of the isotherm to very low concentrations. For all differential sedimentation coefficients, corrections are derived for the slowing of the sedimentation boundaries caused by radial dilution. As an alternative to the interpretation of the isotherm of the weight-average s value, direct global modeling of several sedimentation experiments with Lamm equation solutions was studied. For this purpose, a new software SEDPHAT is introduced, allowing the global analysis of several sedimentation velocity and equilibrium experiments. In this approach, information from the shape of the sedimentation profiles is exploited, which permits the identification of the association scheme and requires fewer experiments to precisely characterize the association. Further, under suitable conditions, fractions of incompetent material that are not part of the reversible equilibrium can be detected.

摘要

分析超速离心是研究蛋白质相互作用和蛋白质自缔合的经典技术之一。近期仪器和计算方面的进展显著提升了该方法。本文开发了用于沉降速度分析蛋白质自缔合的新工具,研究了它们的统计特性,并讨论了优化实验设计的注意事项。一种传统策略是分析重均沉降系数s(w)等温线作为蛋白质浓度的函数。从理论考虑可知,只要能为沉降曲线提供良好模型,对任何微分沉降系数分布c(s)、ls-g() (s)或g(s())进行积分都能得到热力学定义明确的等温线。为检验g(s(*))分布的这一条件,提出了向原始数据空间的反变换。在沉降系数分布c(s)中对扩散进行去卷积,有助于识别不参与缔合的物种。由于在c(s)方法中可分析大量扫描数据,其s(w)值非常精确,能将等温线扩展到极低浓度。对于所有微分沉降系数,都推导出了因径向稀释导致沉降边界减慢的校正值。作为解释重均s值等温线的替代方法,研究了用Lamm方程解对多个沉降实验进行直接全局建模。为此,引入了新软件SEDPHAT,可对多个沉降速度和平衡实验进行全局分析。在这种方法中,利用了沉降曲线形状的信息,这有助于识别缔合方案,且精确表征缔合所需的实验更少。此外,在合适条件下,可检测到不属于可逆平衡一部分的无活性物质的比例。

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