Jensen L J, Sørensen J N, Larsen E H, Willumsen N J
Zoophysiological Laboratory, August Krogh Institute, University of Copenhagen, Denmark.
J Gen Physiol. 1997 Jan;109(1):73-91. doi: 10.1085/jgp.109.1.73.
We have hypothesized that a major role of the apical H(+)-pump in mitochondria-rich (MR) cells of amphibian skin is to energize active uptake of Cl- via an apical Cl-/HCO3(-)-exchanger. The activity of the H+ pump was studied by monitoring mucosal [H+]-profiles with a pH-sensitive microelectrode. With gluconate as mucosal anion, pH adjacent to the cornified cell layer was 0.98 +/- 0.07 (mean +/- SEM) pH-units below that of the lightly buffered bulk solution (pH = 7.40). The average distance at which the pH-gradient is dissipated was 382 +/- 18 microns, corresponding to an estimated "unstirred layer" thickness of 329 +/- 29 microns. Mucosal acidification was dependent on serosal pCO2, and abolished after depression of cellular energy metabolism, confirming that mucosal acidification results from active transport of H+. The [H+] was practically similar adjacent to all cells and independent of whether the microelectrode tip was positioned near an MR-cell or a principal cell. To evaluate [H+]-profiles created by a multitude of MR-cells, a mathematical model is proposed which assumes that the H+ distribution is governed by steady diffusion from a number of point sources defining a set of particular solutions to Laplace's equation. Model calculations predicted that with a physiological density of MR cells, the [H+] profile would be governed by so many sources that their individual contributions could not be experimentally resolved. The flux equation was integrated to provide a general mathematical expression for an external standing [H+]-gradient in the unstirred layer. This case was treated as free diffusion of protons and proton-loaded buffer molecules carrying away the protons extruded by the pump into the unstirred layer; the expression derived was used for estimating stationary proton-fluxes. The external [H+]-gradient depended on the mucosal anion such as to indicate that base (HCO3-) is excreted in exchange not only for Cl-, but also for Br- and I-, indicating that the active fluxes of these anions can be attributed to mitochondria-rich cells.
我们推测,两栖动物皮肤富含线粒体(MR)细胞顶端的H⁺泵的主要作用是通过顶端的Cl⁻/HCO₃⁻交换体为Cl⁻的主动摄取提供能量。通过用pH敏感微电极监测黏膜[H⁺]分布来研究H⁺泵的活性。以葡萄糖酸盐作为黏膜阴离子时,与角质化细胞层相邻处的pH比轻度缓冲的本体溶液(pH = 7.40)低0.98±0.07(平均值±标准误)个pH单位。pH梯度消散的平均距离为382±18微米,对应于估计的“未搅动层”厚度为329±29微米。黏膜酸化取决于浆膜pCO₂,并且在细胞能量代谢受抑制后消失,证实黏膜酸化是H⁺主动转运的结果。在所有细胞附近,[H⁺]实际上相似,并且与微电极尖端是位于MR细胞还是主细胞附近无关。为了评估由众多MR细胞产生的[H⁺]分布,提出了一个数学模型,该模型假设H⁺分布由来自多个点源的稳定扩散控制,这些点源定义了拉普拉斯方程的一组特定解。模型计算预测,在MR细胞的生理密度下,[H⁺]分布将由如此多的源控制,以至于它们各自的贡献无法通过实验分辨。通量方程被积分以提供未搅动层中外部稳定[H⁺]梯度的一般数学表达式。这种情况被视为质子和携带泵挤出到未搅动层中的质子的质子负载缓冲分子的自由扩散;导出的表达式用于估计稳定的质子通量。外部[H⁺]梯度取决于黏膜阴离子,这表明碱(HCO₃⁻)不仅与Cl⁻交换排泄,还与Br⁻和I⁻交换排泄,表明这些阴离子的主动通量可归因于富含线粒体的细胞。