Figure 21.

Balance between production of nutrients by microorganisms and uptake by assimilation or precipitation as a function of concentration (proportional to diffusion scale). Reaction is normalized to the maximum production rate and concentration is normalized to half saturation (Km) (modified from Aller and Aller[23]).

Kristensen Geochemical Transactions 2001 2:92   doi:10.1186/1467-4866-2-92