SUMMARYIncreases in turbidity of Escherichia coZi strain ~1 2 due to added non-permeant salts (NaCl and MgC1,) and sucrose are strictly dependent on medium osmotic pressure, when correction is made for changes in medium refractive index. The volume of the whole cell and the fraction of the intact cell bounded by the cytoplasmic membrane have been measured by dextran and [14C]sucrose exclusion spaces. Increases in medium osmotic pressure due to non-penetrant medium solutes cause outflow of water across the cytoplasmic membrane and contraction away from the cell wall (plasmolysis), corresponding to the increases in turbidity. In addition salts (NaCl and MgCl,) cause appreciable contraction in volume of the whole cell, presumably due to ionic interaction with the wall; sucrose causes only marginal decreases in whole cell volume. Electron micrographs of cells plasmolysed by NaCl or MgCl,, but not by sucrose, show numerous adhesion points between the wall and the cytoplasmic membrane.Glycerol penetrates the cell to the same extent as water, but because of its slower rate of penetration, transient decreases in volume occur which can be measured in a stopped-flow spectrophotometer due to concomitant increases in turbidity. In cells grown on glucose-containing medium the rate of glycerol penetration is non-saturating. In cells grown on glycerol an additional saturatingfacilitated diffusion system is induced. Mutants deleted in the facilitator (F-) are available and do not show facilitated diffusion when grown on glycerol. Water exit and glycerol penetration in glucose-grown cells show transition points in Arrhenius plots corresponding to phase changes of the membrane lipids.
I N T R O D U C T I O NCells are permeable to water, but selectively permeable to extra-and intra-cellular solutes. The cell permits entry and exit of only those solutes necessary to maintain its metabolism. Facilitated diffusion and active transport systems are formed to allow solute transport across the plasma membrane (Kaback, 1972). A few solutes, for example urea and glycerol, appear to be capable of entry by simple diffusion (Mitchell & Moyle, 1956).Cells thus act as osmometers: changes in medium osmotic pressure cause movements of water into or out of the cell (and hence cause volume changes of the cell) in order to regain osmotic equilibrium between the cell and its environment. A convenient, simple and rapid method of measuring osmotically-induced volume changes is to measure light scattering or turbidity changes. This technique is a powerful method of assaying substrate entry into cells. The medium osmotic pressure is raised, causing water exit and a decrease in volume (increase in turbidity). The subsequent entry of substrate causes re-swelling (decrease in turbidity) and the rate of re-swelling can be used to determine the properties of the substrate permea-