We present a one-dimensional physicochemical model of the processes le
ading to methane emission from peatland. The model simulates short-ter
m responses of the methane-emitting system. Biological transformations
(respiration, methanogenesis and oxidation of methane) follow modifie
d Michaelis-Menten kinetics, with reaction potentials based on simplif
ied representations of measured data. Root transport properties are si
milarly schematised. The model simulates measured responses to tempera
ture, water table and inhibitor deposition (acid rain) quite well. Met
hane emission occurs overwhelmingly through the plant-introducing root
transport into the model system typically converts a net sink into a
source. Simulations performed using the model highlight the need for c
aution when extrapolating apparent activation energies or Q(10) factor
s based on short-term laboratory-based incubations to larger areas and
longer time scales. They suggest that short-term temperature response
is proportional to baseline activity and, other things being equal, t
hat increasing total root transport capacity above a very low minimum
is likely to result in a net decrease in methane flux. (C) 1998 Elsevi
er Science Ltd. All rights reserved.