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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

The Bernoulli Equation and the Substitution v = y^(1-n)

How does the substitution $v = y^{1-n}$ turn a Bernoulli equation, nonlinear in $y$, into a linear equation you already know how to solve?


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Your summary note

    1. 1

      Direct versus inverse substitution

      Define each by whether a new or an old variable stands alone on the left, and record u=1−x2u = 1 - x^2u=1−x2 for ∫x1−x2 dx\int x\sqrt{1-x^2}\,dx∫x1−x2​dx and x=sin⁡ux = \sin ux=sinu for ∫1−x2 dx\int \sqrt{1-x^2}\,dx∫1−x2​dx.

    2. 2

      The form y′=p(x)y+q(x)yny' = p(x)y + q(x)y^ny′=p(x)y+q(x)yn and its restrictions

      Record that every term on the right must carry yyy or a power of yyy, with no pure xxx or constant term, and that n=0n = 0n=0 is linear and n=1n = 1n=1 separable.

    3. 3

      Dividing by yny^nyn to reach a linear equation in vvv

      Divide through by yny^nyn, set v=y1−nv = y^{1-n}v=y1−n, compute v′=(1−n)y−ny′v' = (1-n)y^{-n}y'v′=(1−n)y−ny′ by the chain rule, reach v′1−n=p(x)v+q(x)\frac{v'}{1-n} = p(x)v + q(x)1−nv′​=p(x)v+q(x), and note the final conversion back to yyy.

    Attempt 1 of 2