A method for the detection of the nitric oxide radical (NO) in oxygen-containing aqueous solution by means of electron paramagnetic resonance spectroscopy (EPR) is described. NO evolving from the spontaneous decomposition of 3-morpholinosydnonimine (SIN-1) was trapped by Fe(2+)-diethyldithiocarbamate (DETC) complex dissolved in yeast cell membranes. The resulting mononitrosyl-Fe(2+)-(DETC)2 complex was stable and exhibited a characteristic EPR signal at g perpendicular = 2.04 and g parallel = 2.02 with an unresolved triplet hyperfine structure at g perpendicular in frozen solution and an isotropic triplet signal at gav = 2.03 at 37 degrees C. The amount of NO trapped was calculated from the amplitude of one of the triplet lines calibrated by means of a dinitrosyl-Fe(2+)-thiosulfate standard. The lower detection limit of NO was 0.5 nmol/(ml x h) due to a low background NO signal. The upper detection limit was about 10 nmol NO/40 mg traps (DETC-loaded yeast cells), because of saturation of traps. The trapping efficiency approached 60% under anaerobic conditions and with low concentrations of SIN-1, but decreased progressively with higher concentrations and in the presence of oxygen. Nitrite (up to 0.1 mM) did not increase the background NO level. The sensitivity was sufficient to follow the rate of NO release from SIN-1 on-line at 37 degrees C in a flat quartz cuvette. The time course of NO release detected by EPR spectrometry correlated with the time course of nitrite accumulation measured by diazotation. In conclusion, this method will permit the on-line detection of NO formation from endogenous and pharmacological sources in oxygen-containing aqueous media.