All animal cells undergo volume expansion or shrinkage because of water flux driven by transmembrane osmotic gradients. The osmotically obliged water moves into and out of the cells primarily by diffusion through the membrane lipid bilayers [1,2]. Because water movement is constrained by membrane fluidity and lipid organization, the diffusional water transport is small in magnitude (Ͻ50 m · s
Ϫ1) and characterized by a high (Ͼ10 kcal · mol Ϫ1 ) Arrhenius activation energy (E a ), a measure of the energy barrier to water flux [1][2][3]. In specialized tissues, such as renal tubules, eye lens, inner ear, and choroid plexus, membrane water permeability is greatly enhanced by the expression of the channel-forming protein aquaporin [3][4][5]. The expression of water channels is not localized in region where high water permeability is required; it is now established that aquaporin molecules are abundant throughout animal tissues [6,7]. Recently, diffuse distributions of aquaporin molecules have been identified in several cardiac preparations by immunohistochemical approaches [6][7][8][9]. However, the functional significance of their presence in tissues serving a non-water-transporting role is still unclear.The purpose of this study was to evaluate osmotically induced volume change and sarcolemmal water flux of guinea pig ventricular myocytes. Cell surface dimensions were measured by digital videomicroscopy, and the osmotic water permeability coeffi- Japanese Journal of Physiology, 52, 333-342, 2002 Key words: cell volume, membrane water permeability, water channel, cardiac myocyte, osmolality.
Abstract:To elucidate the mechanism of water flux across heart cell membranes, osmotically induced volume changes and sarcolemmal water permeability were evaluated in isolated guinea pig ventricular myocytes by videomicroscopic measurements of cell surface dimensions. Superfusion with anisosmotic solution (0.5-4 times normal osmolality) caused a rapid (Ͻ3 min to new steady state) and reversible cell swelling or shrinkage mainly because of proportional changes in cell width and thickness. The van't Hoff relationship between relative cell volume and the reciprocal of relative osmolality was linear and predicted an apparent osmotically dead space of ϳ35% cell volume. The osmotic water permeability coefficient (P f ) measured from the time course of cell swelling/shrinkage was ϳ22 m · s Ϫ1 at 35°C. Arrhenius activation energy (E a ), a measure of the energy barrier to water flux, was ϳ3.8 kcal · mol Ϫ1 between 11 and 35°C; this value is equivalent to E a for free-water diffusion in bulk solution (ϳ4 kcal · mol ). Although the observed P f is small in magnitude, both the low E a and the sulfhydryl-related modifications of P f are characteristic of channel-mediated water transport. These data suggest that water channels form a major conduit for water crossing the sarcolemma of guinea-pig heart cells.