This paper examines the Rothamsted soil-carbon turnover model. This mo
del and other soil carbon turnover models are increasingly being used
in climate change and land use studies. The formulation of this model
is as a discrete sums-of-exponentials. This discrete form may be conve
rted to a continuous form which can be shown to be an asymptotic appro
ximation of a simple linear first-order system of differential equatio
ns where the exponential decay rate constants in the sums-of-exponenti
als form approximate the first-order rate transfer coefficients in the
differential equation form. There are many standard analytical result
s that can be obtained from this linear system of differential equatio
ns that could prove to be very useful in modelling soil-carbon turnove
r.