Stafford Walter F, Braswell Emory H
Analytical Ultracentrifugation Research Laboratory, Boston Biomedical Research Institute, 64 Grove Street, Watertown, MA 02472, USA.
Biophys Chem. 2004 Mar 1;108(1-3):273-9. doi: 10.1016/j.bpc.2003.10.027.
A method is described for the sedimentation velocity analysis of solutions composed of macromolecular solutes of widely disparate size. In sedimentation velocity experiments, usually a single rotor speed is chosen for the entire run, and consequently, the range of observable sedimentation coefficients can be severely limited. This limitation can be removed if the speed is varied during the run, starting with a relatively low speed so that the largest particles can be easily observed. The speed is increased during the run until full speed is attained and the run continued at full speed until the smallest species of interest have cleared the solution. The method, called wide distribution analysis, is based on the method developed originally by Yphantis and co-workers (Proc. Natl. Acad. Sci. USA 78 (1981) 1431) and on the time derivative method of Stafford (Anal. Biochem. 203 (1992) 295), essentially eliminating both the time-independent and radially-independent noise thereby improving the precision, especially for interference optics. An algorithm for analysis of data from both absorbance and interference optics and experimental protocols compatible with the Beckman XL-I Analytical Ultracentrifuge are presented. With these protocols an extremely wide range of sedimentation coefficients from approximately 1.0 to 250000 S can be accommodated in a single multi-speed run.
本文描述了一种用于分析由大小差异极大的大分子溶质组成的溶液沉降速度的方法。在沉降速度实验中,通常在整个实验过程中选择单一的转子速度,因此,可观测沉降系数的范围可能会受到严重限制。如果在实验过程中改变速度,从相对较低的速度开始,以便能够轻松观察到最大的颗粒,那么这种限制就可以消除。在实验过程中逐渐提高速度,直到达到全速,并以全速继续实验,直到感兴趣的最小物种沉降出溶液。这种方法称为宽分布分析,它基于Yphantis及其同事最初开发的方法(《美国国家科学院院刊》78 (1981) 1431)以及Stafford的时间导数方法(《分析生物化学》203 (1992) 295),基本上消除了与时间无关和与径向无关的噪声,从而提高了精度,特别是对于干涉光学。本文还介绍了一种用于分析来自吸光度和干涉光学数据的算法,以及与贝克曼XL-I分析型超速离心机兼容的实验方案。通过这些方案,在一次多速实验中可以涵盖从大约1.0到250000 S的极宽沉降系数范围。