Method
Flows on the line
Adapted
Shows how to read the long-time behaviour of an autonomous equation off the graph of — fixed points, the sign of at each one as a decay or growth rate, and the theorem that every solution is monotone, so that nothing on the line can oscillate.
Prerequisites: Existence and uniqueness of solutions, Taylor's theorem, Limits of sequences and completeness
An autonomous equation in one unknown,
is the smallest nonlinear problem there is, and almost none of them can be solved in closed form. They do not need to be. The whole qualitative story — which states the system settles into, from which starting values, how fast, and which solutions run away to infinity — can be read off the graph of without integrating anything, and this unit says how.
The reason the reading is so complete is a restriction that will not survive into two dimensions: a solution of is a monotone function of . It cannot overshoot, it cannot ring, and it cannot repeat. Everything either approaches a zero of or leaves every bounded set. Oscillation needs either a second dimension, which is the subject of Classification of linear planar systems and what follows it, or a phase space that closes on itself, which is Flows on the circle.
Let be an open interval and let be continuously differentiable. The equation
is called a one-dimensional or first-order system. It is autonomous: the right-hand side does not contain , so the rule of motion at a point of is the same at every instant. By Existence and uniqueness of solutions the initial-value problem has exactly one solution on some time interval around , and we write for it and for the largest interval on which it is defined.
The geometric reading is to regard not as an axis along which graphs of solutions are drawn, but as the space in which the motion happens — the phase line. A number is a state; is the velocity assigned to that state; the assignment is a vector field on the line. A solution is then the position at time of a point carried by that field, and its image in is its trajectory. The picture of with the trajectories marked, arrows pointing right where and left where , is the phase portrait. Strogatz's way of holding the picture in mind is to imagine a fluid filling the line and moving with local velocity , a solution being a speck carried along by it.
A fixed point (equivalently, an equilibrium point) is a zero of : a number with . The constant function is then a solution, and in the fluid picture is a place where the fluid is at rest. We adopt Hirsch, Smale and Devaney's definitions of what it means for such a point to be stable. The fixed point is
- stable if every neighbourhood of contains a neighbourhood of such that every solution starting in is defined for all and stays in for all ;
- asymptotically stable (a sink, or an attractor) if in addition can be chosen so that every solution starting in it satisfies as ;
- unstable (a source, or a repeller, when the flow leaves on both sides) if it is not stable.
In phase portraits a sink is drawn as a filled circle and a source as an open one; a fixed point attracting on one side and repelling on the other is drawn half filled and called half-stable.
Let be continuously differentiable on an open interval and let for some . Write .
- If , then is asymptotically stable. Quantitatively: for every there is a such that every solution with exists for all and obeys
- If , then is unstable. Quantitatively: for every there is a such that any solution starting with obeys for as long as it stays within of , and therefore leaves that neighbourhood in finite time.
- If , no conclusion follows. All four possibilities occur: is asymptotically stable for , unstable for , half-stable for , and stable but not asymptotically stable for .
The number is a rate and its reciprocal is the characteristic time of the fixed point: the time in which a small deviation from changes by a factor .
Strogatz states the criterion in the form that the perturbation obeys and so grows or decays exponentially at rate , and identifies as the time scale, without the that parts 1 and 2 carry here (pp. 24-25); the is the price of turning the approximation into an inequality valid for the nonlinear equation, and the proof below pays it. Part 1 is also the one-dimensional case of Hirsch, Smale and Devaney's theorem that an equilibrium whose linearisation has every eigenvalue of negative real part is asymptotically stable (p. 175), the single eigenvalue here being .
Near the graph of is a line of slope through the zero, bent by an amount that is small compared with the deviation itself. A line of negative slope through points towards on both sides, and a line of positive slope points away. The only work is to show that the bending cannot overturn the verdict, and the trick is not to track the position but its square: is times a coefficient that the mean value theorem exhibits as an average of over the segment from to , and continuity of pins that average within of . The differential inequality then integrates to the stated exponential bound, with no linearisation and no neglected terms.
Write , so and .
Step 1: an exact factorisation of the right-hand side. Since is continuously differentiable and , the fundamental theorem of calculus applied to on gives
valid for every with . This is exact, not an approximation; is continuous and . (It is the integral form of the first-order Taylor expansion of Taylor's theorem, arranged so that the remainder is absorbed into the coefficient rather than left over.)
Step 2: choosing the neighbourhood. Let . Because is continuous at , there is with and
If then every point with also lies within of , so averaging the displayed bound over gives
Step 3: the differential inequality. Put . Wherever the solution satisfies ,
so by , . Multiplying the right-hand inequality by the positive factor turns it into , so is non-increasing and
The same manipulation with the left-hand inequality gives .
Step 4: part 1. Suppose and let , so ; take from step 2 and . As long as the solution stays in , bound holds and gives , so the solution cannot reach the boundary of that interval; since it also stays in a compact subset of , it does not blow up and is defined for all . Hence holds for all , and as it forces . Both parts of the definition of asymptotic stability are met, with serving for any given once is shrunk to fit inside .
Step 5: part 2. Suppose and let , so ; take from step 2 and . While the solution remains in we have , whose right-hand side exceeds once . So the solution leaves the interval by that time. Since this happens for starting values arbitrarily close to , no neighbourhood of the kind required for stability exists when .
Step 6: part 3. Each of the four equations has . For separation of variables gives for , so : asymptotically stable, but decaying like rather than exponentially. For the same computation gives , so as : unstable, indeed blowing up in finite time. For the field points right on both sides, so the origin attracts from the left and repels on the right: half-stable, hence not stable. For every point is a fixed point, so solutions neither approach nor leave: stable, not asymptotically stable.
Let be continuously differentiable on an open interval and let solve on its maximal interval .
- No crossing. If for some and some fixed point , then . Equivalently, a non-constant solution never attains the value of a fixed point, at any finite time.
- Monotonicity. is either strictly increasing on all of , or strictly decreasing on all of it, or constant, according to the sign of .
- No periodic solutions. The only periodic solutions of are the constant ones. In particular there are no oscillations: no overshoot, no ringing, no sustained cycle.
- The only two fates. As , either tends to a fixed point of , or it leaves every compact subinterval of . If and is bounded above (for increasing ) or below (for decreasing ), then and converges to a fixed point.
Strogatz states 2, 3 and (for ) 4 and attributes them to the topology of the line: a point moving monotonically along a line never returns to where it started (pp. 28-29).
To turn around, a solution must pass through an instant at which its velocity is zero — and its velocity is evaluated at its own position, so at that instant it is sitting on a fixed point. But a fixed point already carries a solution, the constant one, and uniqueness allows only one solution through a given state. So a solution that touches a fixed point is that constant solution and never moved at all. A moving solution therefore never changes the sign of its velocity: it is monotone, and a monotone function that is not constant cannot return to an earlier value.
The last part is the monotone convergence theorem plus one observation: a monotone solution that converges must be slowing to a stop, and the only places where the velocity vanishes are the fixed points.
Part 1. Suppose and . The constant function solves with . Since is continuously differentiable it is locally Lipschitz, so by Existence and uniqueness of solutions the initial-value problem posed at time with value has only one solution, and two solutions that agree at one time agree on their whole common interval. Hence .
Part 2. Set , a continuous function of . Suppose took both a strictly positive and a strictly negative value, say with . By the intermediate value theorem there is with , that is, , so is a fixed point. By part 1, is then constant and , contradicting . So does not change sign.
If is nowhere zero it has one strict sign throughout, and is strictly monotone. If for some , part 1 makes constant. In either case the sign is that of .
Part 3. Let be periodic with period , so for all . Then is defined for all and , which is incompatible with strict monotonicity. By part 2, is constant.
Part 4. Suppose is increasing (the decreasing case is the same with the inequalities reversed, or follows by applying this one to , which solves ). Let be a compact subinterval, and suppose for all . Then is increasing and bounded above by , so by the monotone convergence theorem exists and lies in . If were finite the solution would extend past from the state , contradicting maximality; so .
It remains to show . Suppose instead . Since increases to we have , for if then on a neighbourhood of by continuity, and entering that neighbourhood would have to decrease. So . By continuity of there is with for , and there is with for . Then for all , so , contradicting . Hence and , a fixed point.
If no compact subinterval contains the trajectory for all time, then by definition leaves every compact subinterval of ; when and is increasing this means (possibly in finite time, as for ).
- Autonomy — that does not depend on — is used everywhere, and is the whole reason a one-dimensional phase space is available. It is needed in part 1 of the monotonicity proof (a constant function is a solution only because holds at all times), and it is what makes the velocity a function of position alone, so that the graph of is a complete description. The non-autonomous equation has the oscillating solutions , so part 3 fails at once without it.
- Uniqueness, which continuous differentiability of supplies, is used exactly once, in part 1 of the monotonicity proof, and everything after it rests on that. Dropping it costs the no-crossing statement: for , which has a continuous but non-Lipschitz right-hand side at the origin, the function equal to for and to for is a solution that sits on the fixed point for all negative time and then leaves it. (Monotonicity happens to survive in that particular example because there, but the argument above no longer delivers it.) The related non-uniqueness example is in Existence and uniqueness of solutions.
- in the stability theorem is what makes the factorisation of step 1 possible; without it the right-hand side has a non-zero constant term and there is no fixed point to be stable.
- continuous at , not merely the existence of , is used in step 2 to make hold on a whole interval rather than at the single point . The exponential bound is a statement about an interval and needs an interval's worth of control.
- is essential and not a technicality: part 3 of the statement exhibits four equations with the same linearisation and four different answers. When , fall back on the sign of on each side of , which always settles the question; the four equations listed there realise the four possible sign patterns, namely for , for , for , and vanishing identically. The degenerate case is not a curiosity: it is precisely where bifurcations happen, which is the subject of Bifurcations in one dimension.
- Boundedness in part 4 cannot be dropped. with has the solution , which reaches infinity at : the solution is monotone and has no fixed point to converge to, and is finite.
Given with continuously differentiable on an interval :
- Find the fixed points. Solve on . If the equation cannot be solved in closed form, split into two pieces whose graphs you know, , and locate the intersections of and instead; the fixed points are the -coordinates of the intersections.
- Mark the sign of on each interval between consecutive fixed points. One test value per interval is enough, because is continuous and vanishes only at the fixed points. Draw a rightward arrow where and a leftward arrow where . This is the phase portrait, and it already determines the fate of every initial condition: the flow carries towards the first fixed point in the direction of its arrow, or out of if there is none.
- Classify each fixed point by the arrows on its two sides: in-in is a sink, out-out a source, and in-out or out-in is half-stable.
- Get the rates. Compute at each fixed point. Negative confirms a sink, positive a source, and the magnitude gives the characteristic time . If the arrows of step 2 still give the classification; only the rate is lost, and the approach is then slower than any exponential.
- Sketch against if required. The curve is monotone, with slope ; it is concave up where the phase point is speeding up (that is, where ) and concave down where it is slowing down, and it approaches a horizontal asymptote at each sink.
- Get exact times when you need them. Because the equation is separable, the time to travel from to with no fixed point in between is which is finite precisely when does not vanish on the closed interval between the two. Its divergence at a fixed point is the analytic form of part 1 of the theorem above.
Take
Step 1: fixed points. at and .
Step 2: signs. , , . So the flow is leftward on , rightward on and leftward on .
Step 3: classification. The arrows point away from on both sides and towards on both sides: is a source, is a sink.
Step 4: rates. , so
confirming step 3 and giving both characteristic times as . Every solution starting with converges to ; every solution with decreases, and since and grows quadratically there, it reaches in finite time. The solution from is the constant .
Step 5: an exact transit time. Start at and ask how long the phase point takes to reach . There is no fixed point in , so step 6 of the method applies. Partial fractions give
because . Hence
At the bracket is ; at it is . So
Step 6: check it two ways. Numerically integrating from with an adaptive solver gives , agreeing to twelve figures. And the linear estimate near the sink predicts a deviation decaying as , so shrinking the deviation from (at ) to (at ) should take about . The true time is longer, because the deviation starts at , which is not small compared with the distance between the fixed points, and the flow there is slower than the linearisation at suggests. The linear rate is a statement about the final approach, not about the whole journey.
The physical setting in which one-dimensional flows arise exactly, rather than as a caricature, is overdamped motion: a particle of mass in a force field , moving through a medium that exerts a drag , obeys
When the drag dominates the inertia the term may be dropped and what is left is first order,
Strogatz's picture is a bead in a vat of honey. (The neglect is not uniformly valid: it fails during a brief initial transient in which the inertial and damping terms are comparable, and only after that does the first-order description take over — a singular limit, treated in Boundary layers and matched asymptotics.)
In this reading, part 3 of the monotonicity theorem is a physical statement with no mystery in it: a mass whose inertia has been thrown away cannot overshoot, so it cannot oscillate. Damped oscillation needs the inertia, and undamped oscillation needs the inertia and no damping; both live in the two-dimensional phase plane of The damped and driven harmonic oscillator, not on a line.
The same content is packaged as a potential. Define by
up to an additive constant; every one-dimensional flow has one, because every continuous function has an antiderivative. Along any solution the chain rule gives
with equality exactly at the fixed points. So never increases along a trajectory: the system always runs downhill, and the fixed points are the critical points of , with local minima the sinks and local maxima the sources. This is the statement that every flow on the line is a gradient flow, and it gives a second reason why nothing can cycle — a cycle would have to return to its starting value, which a strictly decreasing quantity forbids. It is also the point of contact with equilibrium thermodynamics and Landau theory, where is a free energy and the stable states of the system are its minima; the bifurcations of Bifurcations in one dimension are then the changes in the shape of that free-energy landscape as a control parameter is turned. For the quadratic example above, , with a local maximum at (value ) and a local minimum at (value ), exactly matching the source and the sink found there.
The defining relation no longer has a single-valued solution once the phase space is a circle and has no zeros, which is how Flows on the circle escapes this unit's conclusions and manages to oscillate.