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水转运蛋白。

Water-transporting proteins.

机构信息

Nordic Center for Water Imbalance Related Disorders, Institute of Cellular and Molecular Medicine, The Panum Institute, University of Copenhagen, Blegdamsvej 3C, 2200N, Copenhagen, Denmark.

出版信息

J Membr Biol. 2010 Apr;234(2):57-73. doi: 10.1007/s00232-009-9216-y. Epub 2009 Nov 30.

Abstract

Transport through lipids and aquaporins is osmotic and entirely driven by the difference in osmotic pressure. Water transport in cotransporters and uniporters is different: Water can be cotransported, energized by coupling to the substrate flux by a mechanism closely associated with protein. In the K(+)/Cl(-) and the Na(+)/K(+)/2Cl(-) cotransporters, water is entirely cotransported, while water transport in glucose uniporters and Na(+)-coupled transporters of nutrients and neurotransmitters takes place by both osmosis and cotransport. The molecular mechanism behind cotransport of water is not clear. It is associated with the substrate movements in aqueous pathways within the protein; a conventional unstirred layer mechanism can be ruled out, due to high rates of diffusion in the cytoplasm. The physiological roles of the various modes of water transport are reviewed in relation to epithelial transport. Epithelial water transport is energized by the movements of ions, but how the coupling takes place is uncertain. All epithelia can transport water uphill against an osmotic gradient, which is hard to explain by simple osmosis. Furthermore, genetic removal of aquaporins has not given support to osmosis as the exclusive mode of transport. Water cotransport can explain the coupling between ion and water transport, a major fraction of transepithelial water transport and uphill water transport. Aquaporins enhance water transport by utilizing osmotic gradients and cause the osmolarity of the transportate to approach isotonicity.

摘要

水通过脂质和水通道蛋白的运输是渗透驱动的,完全由渗透压差驱动。共转运体和单转运体中的水转运不同:水可以通过与底物通量偶联的机制共转运,这种机制与蛋白质密切相关。在 K(+) / Cl(-) 和 Na(+) / K(+) / 2Cl(-) 共转运体中,水完全共转运,而葡萄糖单转运体和 Na(+) 偶联的营养物和神经递质转运体中的水转运通过渗透和共转运发生。水共转运的分子机制尚不清楚。它与蛋白质内水通道中的底物运动有关;由于细胞质中扩散速率很高,传统的未搅动层机制可以排除在外。各种水转运模式的生理作用与上皮转运有关。上皮水转运由离子的运动提供能量,但耦合是如何发生的还不确定。所有上皮细胞都可以逆渗透压梯度向上转运水,这很难用简单的渗透作用来解释。此外,水通道蛋白的遗传缺失并没有支持渗透作用是唯一的运输方式。水共转运可以解释离子和水转运之间的偶联,这是跨上皮水转运和向上水转运的主要部分。水通道蛋白通过利用渗透梯度增强水转运,并使转运物的渗透压接近等渗。

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