Abstract
This paper is concerned with the linear ODE in the form , which represents a simplified storage model of the carbon in the soil. In the first part, we show that, for a periodic function , a linear drift in the coefficient involves a linear drift for the solution of this ODE. In the second part, we extend the previous results to a classical heat non-homogeneous equation. The connection with an analytic semi-group associated to the ODE equation is considered in the third part. Numerical examples are given.
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