A single class of first-order differential equation models a wide range of real phenomena: whenever a quantity's instantaneous rate of change depends on the quantity itself (and possibly time), the governing equation has the form dtdx=f(x,t).
Population growth (Malthusian law). If a population x(t) grows at a rate proportional to its current size, dtdx=kx with k>0. This is separable: xdx=kdt⇒lnx=kt+C⇒x=x0ekt, where x0 is the population at t=0. Doubling/tripling-time problems fix k from one data point and then answer a second question using the same k.
Radioactive decay. The same law with a negative rate constant, dtdA=−kA (k>0), models decay: A(t)=A0e−kt. The half-life is the time t1/2 at which A=2A0, found by solving 21=e−kt1/2.
Newton's law of cooling/warming. The rate at which a body's temperature T(t) changes is proportional to the difference between T and the constant ambient temperature Tm:
dtdT=k(T−Tm),k<0 for both cooling and warming towards Tm.
Separating and integrating gives T−Tm=Cekt; the constant C is fixed by the temperature at t=0, and k is fixed from one later reading, after which the model predicts the temperature (or the time to reach a target temperature) at any other instant.
Mixture (tank) problems. For a substance flowing into and out of a well-stirred tank, the amount x(t) present obeys
dtdx=IN−OUT, …