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Lecture Notes in Differential Equations - Bruce E. Shapiro

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392 LESSON 34. CRITICAL POINTS<br />

Figure 34.9: Phase portraits of s<strong>in</strong>gular l<strong>in</strong>ear system where all coefficients<br />

are nonzero for c/a > 0.<br />

is a critical po<strong>in</strong>t (when d ≠ 0), or on the l<strong>in</strong>e x = 0 (when d = 0). The<br />

directions of motion along the trajectories switch along the critical l<strong>in</strong>e. A<br />

good analogy is to th<strong>in</strong>k of the critical l<strong>in</strong>e as the top of a ridge (or the<br />

bottom of a valley), compared to a s<strong>in</strong>gle apex for a nons<strong>in</strong>gular system<br />

(Figure 34.9). We essentially have a whole l<strong>in</strong>e of sources or s<strong>in</strong>ks.<br />

By a similar argument, if c = d = 0 and a ≠ 0 and/or b ≠ 0, the system<br />

becomes<br />

}<br />

x ′ = ax + by<br />

y ′ (34.102)<br />

= 0<br />

The solutions are all horizontal l<strong>in</strong>es, and there is a ridge or valley of critical<br />

po<strong>in</strong>ts along the l<strong>in</strong>e y = ax/b (if b ≠ 0) or along the l<strong>in</strong>e x = 0 (if b = 0).<br />

If a = c = 0 with b ≠ 0 and d ≠ 0, the system is<br />

}<br />

x ′ = by<br />

y ′ = dy<br />

(34.103)<br />

The x-axis (the l<strong>in</strong>e y = 0) is a critical ridge (valley) and the trajectories<br />

are parallel l<strong>in</strong>es with slope d/b. Similarly, if b = d = 0 with a ≠ 0 and<br />

d ≠ 0 the system is<br />

}<br />

x ′ = ax<br />

y ′ (34.104)<br />

= ay<br />

so that the trajectories are parallel l<strong>in</strong>es with slope c/a and the y-axis is a

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