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Interactions of solvent with the heme region of methemoglobin and fluoro-methemoglobin.

机译:溶剂与高铁血红蛋白和氟-高铁血红蛋白的血红素区域的相互作用。

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摘要

It is now more than 20 years since Davidson and collaborators (1957, Biochim. Biophys, Acta. 26:370-373; J. Mol. Biol. 1:190-191) applied the theoretical ideas of Bloembergen et al. (1948. Phys. Rev. 73:679-712) on outer sphere magnetic relaxation of solvent protons to studies of solutions of methemoglobin. From then on, there has been debate regarding the relative contributions to paramagnetic solvent proton relaxation by inner sphere (ligand-exchange) effects and by outer sphere (diffusional) effects in methemoglobin solutions. Gupta and Mildvan (1975. J. Biol. Chem 250:146-253) extended the early measurements, attributed the relatively small paramagnetic effects to exchange with solvent of the water ligand of the heme-Fe3+ ion, and interpreted their data to indicate cooperativity and an alkaline Bohr effect in the presence of inositol hexaphosphate. They neglected the earlier discussions entirely, and made no reference to outer sphere effects. We have measured the relaxation rate of solvent protons as a function of magnetic field for solutions of methemoglobin, under a variety of conditions of pH and temperature, and have given careful consideration to the relatively large diamagnetic corrections that are necessary by making analogous measurements on oxyhemoglobin, carbonmonoxyhemoglobin, and cyano- and azide-methemoglobin. (The latter two, because of their short electronic relaxation times, behave as though diamagnetic). We show that the paramagnetic contribution to solvent relaxation can be dominated by outer sphere effects, a result implying that many conclusions, including those of Gupta and Mildvan, require reexamination. Finally, we present data for fluoro-methemoglobin, which relaxes solvent protons an order of magnitude better than does methemoglobin. Here one has a startling breakdown of the dogma that has been the basis for interpreting many ligand-replacement studies; in contrast to the prevailing view that replacement of a water ligand of a protein-bound paramagnetic ion by another ligand should decrease relaxation rates, replacement of H2O by F- increases the relaxation rate drastically. The data can all be reconciled, however, with what is anticipated from knowledge of ligand interactions in the heme region.
机译:戴维森及其合作者(1957,Biochim。Biophys,Acta。26:370-373; J. Mol。Biol。1:190-191)应用Bloembergen等人的理论思想至今已有20多年了。 (1948.Phys.Rev.73:679-712)关于溶剂质子的外球磁弛豫以研究高铁血红蛋白溶液。从那时起,关于高铁血红蛋白溶液中内球(配体交换)效应和外球(扩散)效应对顺磁溶剂质子弛豫的相对贡献一直存在争议。 Gupta和Mildvan(1975. J. Biol。Chem 250:146-253)扩展了早期的测量结果,将相对较小的顺磁效应归因于与血红素-Fe3 +离子水配体的溶剂交换,并解释了它们的数据以表明协同作用在肌醇六磷酸存在下具有碱性玻尔效应。他们完全忽略了前面的讨论,没有提及外层效应。我们已经测量了在各种pH和温度条件下高铁血红蛋白溶液的溶剂质子弛豫率与磁场的函数关系,并仔细考虑了通过对氧合血红蛋白进行类似测量而需要的相对较大的反磁性校正,一氧化碳血红蛋白和氰基-叠氮化物-高铁血红蛋白。 (由于后两者的电子弛豫时间短,它们的表现就好像是抗磁性的)。我们表明顺磁对溶剂弛豫的贡献可以由外球效应决定,结果暗示许多结论,包括Gupta和Mildvan的结论,都需要重新检验。最后,我们提供了氟-高铁血红蛋白的数据,它比高铁血红蛋白更好地使溶剂质子松弛了一个数量级。在这里,人们对教条有了惊人的分解,这已经成为解释许多配体置换研究的基础。与普遍的观点相反,普遍认为蛋白质结合的顺磁离子的水配体被另一种配体替代会降低弛豫率,而F-替代H2O则大大提高了弛豫率。然而,所有数据都可以与血红素区域中配体相互作用的知识相吻合。

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