E. Bosatta et Gi. Agren, THE POWER AND REACTIVE CONTINUUM MODELS AS PARTICULAR CASES OF THE Q-THEORY OF ORGANIC-MATTER DYNAMICS, Geochimica et cosmochimica acta, 59(18), 1995, pp. 3833-3835
The reactive continuum model (Boudreau and Ruddick, 1991), the power m
odel (Janssen, 1984; Middelburg, 1989), and the a-theory (Bosatta and
Agren, 1991a) have been used to describe decomposition of organic matt
er; the reactive continuum model has also been used to model the kinet
ics of kerogen cracking, i.e., of oil and gas generation (Burnham et a
l., 1987). The reactive continuum model describes the organic matter a
s being composed of a continuous distribution of reactive types; the b
asic premise in the power model is that the reactivity of organic matt
er decreases with time. The q-theory is based on the idea that organic
matter is composed of an infinite spectrum of interacting (through mi
crobial and physicochemical processes) reactive types. We show here th
at the reactive continuum model and the power model can be deduced as
particular cases of the q-theory. The q-theory reduces to the reactive
continuum model if all interactions between the components of the spe
ctrum are neglected, whereas the power model is obtained under specifi
c assumptions about microbial properties. The q-theory is, therefore,
not only mathematically more general but has also a larger explanatory
power.