The "independence principle" in the processes of water transport

A General Channel Model Accounts for Channel, Carrier, Countertransport and Cotransport Kinetics

In this work we propose a unifying model of mediated membrane transport, based upon the idea that the integral membrane proteins involved in these processes operate via complex channel mechanisms. In the first part, we briefly review literature about the structural aspects of membrane transporters. We conclude that there is a substantial amount of evidence suggesting that most membrane proteins performing transport are embodied with channel-like structures that may constitute the translocation paths. This includes cases where the phenomenological transport kinetics do not correspond to the classical channel behavior. In the second part of this article we introduce the general channel model of mediated transport and employ it to derive specific examples, like simple one- or two-ligand channels, water-ligand channels, simple carriers, co- and counter-transport systems and more complex water-ligand carriers. We show that, for the most part, these particular cases can be obtained by the application of the techniques of diagram reduction to the full model. The necessary conditions for diagram reduction reflect physical properties of the protein and its surroundings.

Water transport across mammalian cell membranes

This review summarizes recent progress in water-transporting mechanisms across cell membranes. Modern biophysical concepts of water transport and new measurement strategies are evaluated. A family of water-transporting proteins (water channels, aquaporins) has been identified, consisting of small hydrophobic proteins expressed widely in epithelial and nonepithelial tissues. The functional properties, genetics, and cellular distributions of these proteins are summarized. The majority of molecular-level information about water-transporting mechanisms comes from studies on CHIP28, a 28-kDa glycoprotein that forms tetramers in membranes; each monomer contains six putative helical domains surrounding a central aqueous pathway and functions independently as a water-selective channel. Only mutations in the vasopressin-sensitive water channel have been shown to cause human disease (non-X-linked congenital nephrogenic diabetes insipidus); the physiological significance of other water channels remains unproven. One mercurial-insensitive water channel has been identified, which has the unique feature of multiple overlapping transcriptional units. Systems for expression of water channel proteins are described, including Xenopus oocytes, mammalian and insect cells, and bacteria. Further work should be directed at elucidation of the role of water channels in normal physiology and disease, molecular analysis of regulatory mechanisms, and water channel structure determination at atomic resolution.

Osmotic permeability in a molecular dynamics simulation of water transport through a single-occupancy pore

The aim of this work is to determine plausible values for the rate constants of kinetic models representing water transport through narrow pores. We present here the results of molecular dynamics simulations of the movement of water molecules through a single-site hydrophilic pore. The system consists of a rectangular box of water molecules, some of which are positionally restrained so as to act as a membrane. This membrane separates two compartments where water molecules move freely; one of the positions in the membrane is initially vacant (the 'single-site pore'), but can be occupied by mobile molecules. To analyze the results, we represented the pore by a two-state kinetic diagram in which the vacant and occupied states are linked by transitions corresponding to the binding and release of water molecules. The mean occupancy and vacancy times directly yield the rate constants of binding and release, which in turn yield the osmotic water permeability coefficient per pore pf. We also compute the apparent activation energies delta E* for the rate constants and for pf. The pf value was (1.56 +/- 0.04).10(-11) cm3/s (at 307 K), which is much larger than those determined for CHIP28 and for gramicidin A (of about 10(-13) and 10(-14) cm3/s, respectively). These values were compared with those arising from a model of a symmetric single-file pore through which one-vacancy-mediated water transport takes place. The model yields an expression for pf as a function of the rate constants and of the number of molecular positions (n) in the file. When n = 1, this expression becomes the one corresponding to the single-site pore studied in our current simulation. Using the rate constants of binding and release derived from our simulation, the pf values are consistent with an occupancy value of 5-6 found for gramicidin A, and with occupancies of 4-7 that can be estimated for the single-file pore of a recently proposed model for CHIP28. delta E* for pf is 3.0 kcal/mol, a value similar to that determined for CHIP28. Hence, the system simulated here appears plausible and can be used to mimic some physical properties of water transport through biological pores.