Beryllium has a nutrient-like vertical. Concentrations are depleted at the surface and increase with depth
Beryllium exists in seawater in the +II oxidation state as the BeOH+ and Be(OH)20 ions.
The residence time was estimated from the interocean fractionation of stable 9Be and radioactive 10Be (Measures et al., 1996).
Beryllium is determined by forming a volatile organic complex followed by gas chromatography with electron capture detection.