| Abstract: | Cysts of the crustacean Artemia are a useful model for studies on intracellular water because they are capable of essentially complete and reversible desiccation. We have used a variety of techniques on this system, the present work being an attempt to estimate the density of intracellular water (rho w). The density of individual cysts was evaluated from sedimentation velocity. Heptane displacement methods were used to determine the volume of a known mass of cysts, from which the density was calculated. The two methods produce comparable results. It was shown that the densities and water contents of large masses of cysts accurately reflect those of individual cysts. Cyst densities (rho c) were determined over the entire range of water content from 0 to 0.63 weight fraction of water (Wf), and temperature dependence was measured for 0.61 Wf over 2-41 degrees C. The following refer to 25 degrees C. No marked change was detected in rho c until the water content exceeded 0.15 Wf, at which rho c decreased as a linear function of Wf to maximum water content. However, the cyst does not behave ideally in the sense that the densities of the nonaqueous components and added water are not additive as a function of Wf. The partial specific volume of water in cysts at maximum hydration was estimated to be 3% larger than that of pure water. These observations are compared with density measurements on other systems, and with previous findings on the physical properties of water in this system. |
