I'm trying to solve this equation (Windkessel equation) numerically as:
$$C \frac{d P}{d t} + \frac{P}{R} = Q(t)$$
Where $C$ is compliance, $R$ is resistance, $P$ is pressure, and $Q(t)$ is a known input signal (i.e. volumetric flux). I tried explicit (i.e. Forward Euler Method) as well as semi-implicit (i.e. Backward Euler Method) and trapezoidal time integration techniques. But, all of these three well-known methods fail at some values for $C$ and $R$.
First, I wanted to know how can I map the stability region of this ODE based on $R$ and $C$ values? Also, what's your suggestion in terms of the time integration method? For example, will the 4th order Runge-Kutta method help me to reach a broader stability zone or not? Any comment or idea is appreciated.