L. Goeyens et al., A ROOM-TEMPERATURE PROCEDURE FOR THE MANUAL DETERMINATION OF UREA IN SEAWATER, Estuarine, coastal and shelf science (Print), 47(4), 1998, pp. 415-418
Several earlier studies underpin the important role of dissolved organ
ic matter and more particularly urea in phytoplanktonic nitrogen uptak
e fluxes. Generally, the determination of urea concentrations relies o
n the formation of an imidazolone-thiosemicarbizide complex, a complex
ation which requires very accurate temperature control when carried ou
t at high temperature. It is also possible, however, to obtain reliabl
e results with a room temperature procedure. The measured abundances f
or both complexation at high temperature (85 degrees C, 20 min) and at
ambient temperature (22 degrees C, 72 h) are closely comparable. Lowe
r values are observed for temperatures <10 degrees C though. Moreover,
a comparison of both techniques reveals similar precision (coefficien
t of variation: 2%), sensitivity (slope of calibration line: 0.2) and
detection limit (0.14 mM). The room temperature alternative to the ear
lier described method is therefore a handy tool for urea analyses, whe
n a strict temperature control is difficult or impossible. (C) 1998 Ac
ademic Press.