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Structural studies of adsorbed protein (betalactoglobulin) on natural clay (montmorillonite)

机译:天然粘土(蒙脱土)上吸附蛋白(β-乳球蛋白)的结构研究

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In this work, the adsorption of a small globular protein (betalactoglobulin, BLG), on a natural montmorillonite clay (Mt) was investigated in acidic buffer (pH = 3). The combination of different characterization techniques such as zetametry, X-ray diffraction, transmission electronic microscopy, fluorescence and solid state nuclear magnetic resonance spectroscopies shed light on the interaction mechanism between the clay mineral and the proteins. For low BLG concentration, a slight increase of the interlayer spacing of the clay mineral was noticed as well as structural changes of the protein. In contrast, as the concentration of BLG increased, the adsorption led to a partial exfoliation of the clay mineral, accompanied with significant secondary structural changes of the protein characterized by a loss of beta-sheet organization. Altogether, our results revealed an unexpected adsorption scheme where the increase of the BLG/Mt weight ratio of the hybrid material leads to a partial exfoliation of the Mt, but at the expense of the protein native structure.
机译:在这项工作中,在酸性缓冲液(pH = 3)中研究了一种小球蛋白(β-乳球蛋白,BLG)在天然蒙脱土(Mt)上的吸附。 Zetametry,X射线衍射,透射电子显微镜,荧光和固态核磁共振光谱等不同表征技术的结合为粘土矿物与蛋白质之间的相互作用机理提供了线索。对于低BLG浓度,可以看到粘土矿物的层间间距略有增加,以及蛋白质的结构变化。相反,随着BLG浓度的增加,吸附会导致粘土矿物部分剥落,并伴随着蛋白质的明显二级结构变化,其特征在于β-折叠结构的丧失。总而言之,我们的结果揭示了一种意想不到的吸附方案,其中杂化材料的BLG / Mt重量比的增加导致Mt的部分剥落,但以蛋白质天然结构为代价。

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