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A Mathematical Model of Solute Coupled Water Transport in Toad Intestine Incorporating Recirculation of the Actively Transported Solute

机译:蟾蜍肠道中溶质耦合水迁移的数学模型结合了主动迁移溶质的再循环

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摘要

A mathematical model of an absorbing leaky epithelium is developed for analysis of solute coupled water transport. The non-charged driving solute diffuses into cells and is pumped from cells into the lateral intercellular space (lis). All membranes contain water channels with the solute passing those of tight junction and interspace basement membrane by convection-diffusion. With solute permeability of paracellular pathway large relative to paracellular water flow, the paracellular flux ratio of the solute (influx/outflux) is small (2–4) in agreement with experiments. The virtual solute concentration of fluid emerging from lis is then significantly larger than the concentration in lis. Thus, in absence of external driving forces the model generates isotonic transport provided a component of the solute flux emerging downstream lis is taken up by cells through the serosal membrane and pumped back into lis, i.e., the solute would have to be recirculated. With input variables from toad intestine (Nedergaard, S., E.H. Larsen, and H.H. Ussing, J. Membr. Biol. 168:241–251), computations predict that 60–80% of the pumped flux stems from serosal bath in agreement with the experimental estimate of the recirculation flux. Robust solutions are obtained with realistic concentrations and pressures of lis, and with the following features. Rate of fluid absorption is governed by the solute permeability of mucosal membrane. Maximum fluid flow is governed by density of pumps on lis-membranes. Energetic efficiency increases with hydraulic conductance of the pathway carrying water from mucosal solution into lis. Uphill water transport is accomplished, but with high hydraulic conductance of cell membranes strength of transport is obscured by water flow through cells. Anomalous solvent drag occurs when back flux of water through cells exceeds inward water flux between cells. Molecules moving along the paracellular pathway are driven by a translateral flow of water, i.e., the model generates pseudo-solvent drag. The associated flux-ratio equation is derived.
机译:建立了吸收性泄漏上皮的数学模型,用于分析溶质耦合水的传输。不带电的驱动溶质扩散到细胞中,并从细胞中泵入侧向细胞间空间(lis)。所有膜都包含水通道,溶质通过对流扩散通过紧密连接的膜和间隙基底膜。与细胞旁水流相比,细胞旁途径的溶质渗透率大,因此溶质的细胞旁通量比(流入/流出)较小(2-4),与实验一致。然后,从lis流出的流体的虚拟溶质浓度显着大于lis中的浓度。因此,在没有外部驱动力的情况下,如果细胞通过浆膜吸收并吸收回lis的溶质通量的一部分,则该模型会产生等渗运输,也就是说,必须将溶质再循环。使用蟾蜍肠的输入变量(Nedergaard,S.,EH Larsen和HH Ussing,J. Membr。Biol。168:241-251),计算预测出60-80%的泵送通量来自浆膜浴,与回流通量的实验估计。在lis的实际浓度和压力下,具有以下特征,可以获得鲁棒的溶液。液体吸收的速率由粘膜的溶质渗透性决定。最大流体流量取决于lis膜上泵的密度。随着将水从粘膜溶液输送到lis的路径的水力传导,能量效率会提高。可以完成向上的水输送,但是由于细胞膜具有较高的水力传导性,因此流过细胞的水会掩盖输送强度。当通过细胞的反水通量超过细胞之间的向内水通量时,就会发生反常的溶剂阻力。沿旁细胞途径移动的分子是由水的横向流动驱动的,即该模型产生了伪溶剂阻力。导出相关的磁通比方程。

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