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通过色散X射线吸收光谱法测定巯基乙酸对马脾铁蛋白中铁的快速还原作用。

Rapid reduction of iron in horse spleen ferritin by thioglycolic acid measured by dispersive X-ray absorption spectroscopy.

作者信息

Joo M S, Tourillon G, Sayers D E, Theil E C

机构信息

Department of Physics, North Carolina University, Raleigh 27695-7622.

出版信息

Biol Met. 1990;3(3-4):171-5. doi: 10.1007/BF01140575.

Abstract

The release of iron from ferritin is important in the formation of iron proteins and for the management of diseases in both animals and plants associated with abnormal accumulations of ferritin iron. Much more iron can be released experimentally by reduction of the ferric hydrous oxide core than by chelation of Fe3+ which has led to the notion that reduction is also the major aspect of iron release in vivo. Variations in the kinetics of reduction of the mineral core of ferritin have been attributed to the redox potential of the reductant, redox properties of the iron core, the structure of the protein coat, the analytical method used to detect Fe2+ and reactions at the surface of the mineral. Direct measurements of the oxidation state of the iron during reduction has never been used to analyze the kinetics of reduction, although Mössbauer spectroscopy has been used to confirm the extent of reduction after electrochemical reduction using dispersive X-ray absorption spectroscopy (DXAS). We show that the near edge of X-ray absorption spectra (XANES) can be used to quantify the relative amounts of Fe2+ and Fe3+ in mixtures of the hydrated ions. Since the nearest neighbors of iron in the ferritin iron core do not change during reduction, XANES can be used to monitor directly the reduction of the ferritin iron core. Previous studies of iron core reduction which measured by Fe2+.bipyridyl formation, or coulometric reduction with different mediators, suggested that rates depended mainly on the redox potential of the electron donor.(ABSTRACT TRUNCATED AT 250 WORDS)

摘要

铁蛋白中铁的释放对于铁蛋白的形成以及动植物中与铁蛋白铁异常积累相关疾病的管理都很重要。通过还原氢氧化铁核心实验释放的铁比通过螯合Fe3+释放的铁多得多,这导致了还原也是体内铁释放主要方面的观点。铁蛋白矿物核心还原动力学的变化归因于还原剂的氧化还原电位、铁核心的氧化还原性质、蛋白质外壳的结构、用于检测Fe2+的分析方法以及矿物表面的反应。尽管穆斯堡尔光谱已被用于通过色散X射线吸收光谱法(DXAS)确认电化学还原后的还原程度,但在还原过程中铁的氧化态的直接测量从未被用于分析还原动力学。我们表明,X射线吸收光谱(XANES)的近边可用于量化水合离子混合物中Fe2+和Fe3+的相对含量。由于铁蛋白铁核心中铁的最近邻在还原过程中不会改变,XANES可用于直接监测铁蛋白铁核心的还原。以前通过Fe2+ -联吡啶形成或用不同介质进行库仑还原测量铁核心还原的研究表明,速率主要取决于电子供体的氧化还原电位。(摘要截短于250字)

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