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Sedimentation Velocity Analysis of Heterogeneous Protein-Protein Interactions: Lamm Equation Modeling and Sedimentation Coefficient Distributions c(s)

机译:异质蛋白相互作用的沉降速度分析:Lamm方程模型和沉降系数分布c(s)

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摘要

We describe algorithms for solving the Lamm equations for the reaction-diffusion-sedimentation process in analytical ultracentrifugation, and examine the potential and limitations for fitting experimental data. The theoretical limiting case of a small, uniformly distributed ligand rapidly reacting with a larger protein in a “constant bath” of the ligand is recapitulated, which predicts the reaction boundary to sediment with a single sedimentation and diffusion coefficient. As a consequence, it is possible to express the sedimentation profiles of reacting systems as c(s) distribution of noninteracting Lamm equation solutions, deconvoluting the effects of diffusion. For rapid reactions, the results are quantitatively consistent with the “constant bath” approximation, showing c(s) peaks at concentration-dependent positions. For slower reactions, the deconvolution of diffusion is still partially successful, with c(s) resolving peaks that reflect the populations of sedimenting species. The transition between c(s) peaks describing reaction boundaries of moderately strong interactions (KD ∼ 10−6 M) or resolving sedimenting species was found to occur in a narrow range of dissociation rate constant between 10−3 and 10−4 s−1. The integration of the c(s) peaks can lead to isotherms of species populations or s-value of the reaction boundary, respectively, which can be used for the determination of the equilibrium binding constant.
机译:我们描述了用于解决分析超离心反应扩散沉淀过程中的Lamm方程的算法,并研究了拟合实验数据的潜力和局限性。概括了理论上的局限性,即一个小的,均匀分布的配体会在配体的“恒定浴”中与较大的蛋白质快速反应,从而预测了具有单一沉降和扩散系数的沉积物的反应边界。因此,可以将反应体系的沉降曲线表示为非相互作用Lamm方程解的c(s)分布,从而消除扩散的影响。对于快速反应,结果在定量上与“恒定浴”近似一致,显示出浓度依赖性位置的c(s)峰。对于较慢的反应,扩散的解卷积仍然部分成功,其中c(s)个分辨峰反映了沉积物的种群。发现在描述中等强相互作用(KD〜10 -6 M)或解析沉积物的反应边界的c(s)个峰之间的跃迁发生在10 −3 和10 −4 s -1 。 c(s)个峰的积分可能分别导致物种种群的等温线或反应边界的s值,这些等温线可用于确定平衡结合常数。

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