Goldberg M, Pecht I
Biochemistry. 1976 Sep 21;15(19):4197-208. doi: 10.1021/bi00664a011.
The electron transfer reaction between the "blue" single copper protein azurin (from Pseudomonas aeruginosa) and the hexacyanoiron (II/III) couple has been studied. Equilibrium constants for the reduction of azurin were measured spectrophotometrically in the temperature range 5-33 degrees C (K = 1.1 X 10(-2) at 25 degrees C, deltaH degrees = 10.9 kcal/mol, 0.1 M potassium phosphate, pH 7.0, I = 0.22). The enthalpy change was also determined by microcalorimetry and from the analysis of chemical relaxation amplitudes. Following a temperature-jump perturbation of this equilibrium, only a single relaxation was observed. The reciprocal of the relaxation time increased linearly as oxidized azurin was reacted with increasing amounts of ferrocyanide, yet reached saturation when reduced azurin was titrated with ferricyanide. This behavior as well as the analysis of the relaxation amplitudes led to the following scheme for this system: see article. At 25 degrees C the rate constants for the electron transfer were k+3=6.4s-1 and k-3=45s-1, the association constants K1=54 M-1 and K2-1=610 M-1. The activation and overall thermodynamic parameters as well as the individual thermodynamic values for the different steps were combined to construct a self-consistent energy profile for the reaction.
对“蓝色”单铜蛋白天青蛋白(来自铜绿假单胞菌)与六氰合铁(II/III)电对之间的电子转移反应进行了研究。在5 - 33摄氏度的温度范围内,通过分光光度法测量了天青蛋白还原的平衡常数(25摄氏度时K = 1.1×10⁻²,ΔH° = 10.9千卡/摩尔,0.1 M磷酸钾,pH 7.0,I = 0.22)。焓变也通过微量量热法以及化学弛豫幅度分析来确定。对该平衡进行温度跃升扰动后,仅观察到单一弛豫。弛豫时间的倒数随着氧化型天青蛋白与越来越多的亚铁氰化物反应而线性增加,但在用铁氰化物滴定还原型天青蛋白时达到饱和。这种行为以及弛豫幅度分析导致了该系统的如下反应历程:见文章。在25摄氏度时,电子转移的速率常数为k₊₃ = 6.4 s⁻¹和k₋₃ = 45 s⁻¹,缔合常数K₁ = 54 M⁻¹和K₂⁻¹ = 610 M⁻¹。将活化和整体热力学参数以及不同步骤的各个热力学值结合起来,构建了该反应的自洽能量分布图。