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Differential Equations
The Geometric View of ODEs
01Direction Fields and the Geometric View of ODEs02Integral Curves and the Isocline Method03Perpendicular Isoclines: The Circles of y' = -x/y04Isocline Corridors and a Trap for Solutions05Existence and Uniqueness: One Curve Through a Point06Where Existence and Uniqueness FailProblem set0/10Problem set 20/10MIT problem set0/3
Numerical Methods
01Euler's Method and Its Three Equations02Euler's Method by Hand: Building the Table03Convexity and the Sign of Euler's Error04First Order Error: Halve the Step, Halve the Error05Improved Euler (RK2): Averaging Two Slopes06Runge-Kutta 4 and the Price of Accuracy07Singular Points: Where Every Method FailsProblem set0/10Problem set 20/10MIT problem set0/1
First-Order Linear Equations
01First Order Linear: Standard Form and the Sign of p02The Conduction-Diffusion Model: Newton's Law of Cooling03The Integrating Factor and the Four-Step Method04Integrating Factors: Two Mistakes and a Trick Question05Constant Coefficients: Steady State and TransientProblem set0/10Problem set 20/10MIT problem set0/1
Substitution Methods
01Scaling a First Order ODE: The Fourth-Power Cooling Law02The Bernoulli Equation and the Substitution v = y^(1-n)03A Worked Bernoulli Example: The Substitution v = 1/y04Homogeneous Equations: The Zoom Test and y = zx05Modelling the Lighthouse Chase: A 45-Degree Heading06The Boat's Path: A Logarithmic Spiral in Polar CoordinatesProblem set0/10Problem set 20/10
Autonomous Equations
01Autonomous Equations and Time-Translation Invariance02Critical Points: Constant Solutions as Barriers03The Embezzler Model dy/dt = ry - w: One Unstable Balance04The Logistic Equation: Carrying Capacity Without Solving05Stable, Unstable and Semi-Stable Critical Points06Maximum Sustainable Harvest: Why h = a^2/4bProblem set0/10Problem set 20/10MIT problem set0/3
Complex Numbers
01Complex Division, Polar Form and the Definition of e^(iθ)02Why e^(iθ) Earns Its Name: Multiply Moduli, Add Angles03Integrating e^(-x) cos x by Complexifying04The nth Roots of Unity: Zeta on the Unit CircleProblem set0/10Problem set 20/10MIT problem set0/4
Input and Response
01Steady-State and Transient Solutions of y' + ky = q(t)02Input, Response and the Superposition Principle03Solving y' + ky = k cos ωt by Complexification04Amplitude and Phase Lag of a Sinusoidal ResponseProblem set0/10Problem set 20/10MIT problem set0/2
01Cartesian Method: Rationalise, Then Take the Real Part02The Sinusoidal Identity and Its Right Triangle03Three Proofs of the Sinusoidal Identity04The Mixing Tank: Salt Balance and k = r/V05RC Circuits, Decay Chains and Negative kProblem set0/10Problem set 20/10MIT problem set0/2
Second-Order Linear Equations
01Second-Order Linear ODEs and the Spring–Mass–Dashpot02The Characteristic Equation and Overdamped Motion03Complex Roots a ± bi and Underdamped Oscillation04Critical Damping and Reduction of Order: t e^(−at)Problem set0/10Problem set 20/10MIT problem set0/2

A Worked Bernoulli Example: The Substitution v = 1/y

Why does $v = 1/y$ make $y' = y/x - y^2$ linear, and why must $v$ become one fraction before you turn it back into $y$?


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Your summary note

    1. 1

      Recognizing n=2n = 2n=2 and reducing to a linear equation

      Record the concealed form xy′−y=−xy2xy' - y = -xy^2xy′−y=−xy2, divide by y2y^2y2, and use v=1/yv = 1/yv=1/y with v′=−y′/y2v' = -y'/y^2v′=−y′/y2 from the chain rule to reach v′+vx=1v' + \frac{v}{x} = 1v′+xv​=1.

    2. 2

      The integrating factor xxx for v′+v/x=1v' + v/x = 1v′+v/x=1

      Compute e∫dx/x=xe^{\int dx/x} = xe∫dx/x=x, multiply through to xv′+v=xxv' + v = xxv′+v=x, check that the left side is (xv)′(xv)'(xv)′, and integrate to v=x2+cxv = \frac{x}{2} + \frac{c}{x}v=2x​+xc​.

    3. 3

      Converting back to y=2xx2+C1y = \frac{2x}{x^2 + C_1}y=x2+C1​2x​

      Combine vvv into the single fraction x2+2c2x\frac{x^2 + 2c}{2x}2xx2+2c​ before inverting, rename 2c2c2c as C1C_1C1​, and record that the constant is not additive, so an initial condition is fitted from this final form.

    Attempt 1 of 2