Simulation of hyporheic self-purification in rivers: the assimilative capacity of proteins

Abstract

For the biochemical study of assimilation capacity (AC), two hypotheses were put forward (three levels of response, the hyporheon being the main site of self-purification). A physical model was designed, simulating the hyporheon and its response to increasing inputs of proteins was studied. The analyses evidence a low accumulation of proteins in the hyporheic biofilms for daily flows ranging from 0.1 to 20 mg/day. The percolation of proteins stimulates the proteolytic activity (increase in Vm) whereas the Km shows no significant change ; the assimilation capacities thus stimulated are vastly superior to the daily loads introduced into the system and explain the low accumulation of proteins. This stimulation concerns only a shallow active zone < 2 cm. For the future, a method of localising zones of hyporheic infiltrations (micro-piezometry, tracing, etc.) should be developed to monitor in situ the action of inputs of organic matter (OM) to estimate the AC of the river.