Summary. The reversible dependence of skin osmotic water permeability (Lpo) upon the ionic concentration of the outer bathing solution -which we have called "hydrosmotic salt effect" (HSE) -was studied in the isolated skin of the toad Bufo marinus ictericus. The skin osmotic water flow (Jr) was measured as a function of outer bathing solution osmolality (Oe). Lp~), calculated as (Jv/A ~)ap_ o (where A ~ and AP are the osmotic and hydrostatic pressure differences across the skin, respectively) was constant when O e was altered with sucrose, a nonelectrolyte. In contrast, LpD increased continuously in the hypotonic range as O e was raised from zero (distilled water) with NaC1 or KCI. The HSE could also be evoked in the condition of reversed osmotic volume flow. with the outer bathing medium made hypertonic with sucrose.Diffusional t4C-sucrose permeability, measured in the Jr=0 condition to prevent solvent drag of sucrose in the paracellular pathways, indicate that the hydrosmotic salt effect cannot be explained by assuming a paracellular permeability increase, due to tight junction opening, but might be interpreted as due to changes in the osmotic water permeability of the apical membranes of the most superficial cells of the epithelium.The hydrosmotic salt effect can be elicited in control skins and in vasopressin-stimulated skins, on top of the hormonal response.The time course of the hydrosmotic salt effect is substantially different from that of the hydrosmotic response to vasopressin. Its half-time is 4 to 5 times faster than that of vasopressin action, with individual values as short as 1.5 min.The time courses of the hydrosmotic salt-effect onset and reversibility are exponential, clearly contrasting with the typical sigmoidal shape of vasopressin onset and washout time courses.Based on time course data and on speed of response we postulate that the mechanism underlying the hydrosmotic salt effect is due to modifications of existing water pathways in the apical membrane, rather than to incorporation and removal of water permeability units in this structure.