A differential equation is a rule for the rate \(\dfrac{dy}{dx}\) written in terms of \(x\), \(y\), or both — a local instruction, not a finished formula for \(y\).
Verifying is not solving. Compute \(y'\) from the candidate, substitute it and \(y\) into the equation, and check both sides agree — never integrate.
Second derivative, concretely: if \(y'=x-y\) then \(y''=1-y'=1-(x-y)\). Differentiate the right side and substitute \(\dfrac{dy}{dx}\) back in — that sign tells you concavity.
A grid of tiny segments. At each point \((x,y)\) the segment's slope is just \(\dfrac{dy}{dx}\) evaluated there — no solving required.
Read the dependence: if \(\dfrac{dy}{dx}\) depends only on \(x\), every column looks identical; only on \(y\), every row looks identical; on both, the field changes everywhere.
When there's no formula for \(y\), march forward in steps of size \(h\), each step following the tangent line at the point you're standing on.
One line to remember: new \(y\) = old \(y\) + (slope at the old point)\(\,\times\,h\). The slope is \(\dfrac{dy}{dx}\) at where you are, not where you're going.
Accuracy: a smaller \(h\) (more steps) shrinks the error — roughly in proportion to \(h\). Get concavity from \(\dfrac{d^2y}{dx^2}\) (differentiate the equation).
The one technique for finding the actual function: get the \(y\)'s with \(dy\), the \(x\)'s with \(dx\), integrate both sides, then solve.
The \(+C\) goes in the moment you integrate — before you solve for \(y\) or exponentiate. Then use the initial condition to pin down \(C\).
Two named models worth recognizing on sight — one grows without bound, the other levels off at a ceiling.
A surprising share of questions never need the solution — they're answered straight from the equation.
Why it matters: "is the estimate an over- or under-estimate," "is the function concave up at this point," "what value does the solution approach" are all concavity-and-sign questions — fast points if you go to the equation instead of hunting for a formula.
Most modeling points are won or lost in the first line. Map the English phrase straight to a rate.
Then attach the data: an initial value gives \(y_0\) (or the constant \(C\)); a second data point or a known rate solves for \(k\). Units on the rate (people per year, °F per minute) confirm you differentiated the right quantity.
Every Unit 7 problem is one of four asks. Match the wording, then run the matching machinery.
The reliable move: read what the verb is asking before touching algebra. "Approximate," "sketch," "find," and "how large does it get" each point at a different one of the four — and choosing right is most of the credit.
Unit 7 is a single idea seen four ways: a differential equation is a local rule for change — and you can meet it as a picture (the slope field), a step-by-step march (Euler), the exact function (separation of variables), or a named model (exponential and logistic). The rule never changes; only how much detail the question demands. Read the verb, pick the view, and the calculus you already know finishes it.