AP Course

AP Calculus AB/BC

Study the complete College Board sequence for AP Calculus AB and BC, from limits through infinite series.

Choose an official unit and topic to open its lecture, concept check, or focused practice.

Lessons
1.1 Introducing Calculus: Can Change Occur at an Instant?1.2 Defining Limits and Using Limit Notation1.3 Estimating Limit Values from Graphs1.4 Estimating Limit Values from Tables1.5 Determining Limits Using Algebraic Properties of Limits1.6 Determining Limits Using Algebraic Manipulation1.7 Selecting Procedures for Determining Limits1.8 Determining Limits Using the Squeeze Theorem1.9 Connecting Multiple Representations of Limits1.10 Exploring Types of Discontinuities1.11 Defining Continuity at a Point1.12 Confirming Continuity over an Interval1.13 Removing Discontinuities1.14 Connecting Infinite Limits and Vertical Asymptotes1.15 Connecting Limits at Infinity and Horizontal Asymptotes1.16 Working with the Intermediate Value Theorem (IVT)2.1 Defining Average and Instantaneous Rates of Change at a Point2.2 Defining the Derivative of a Function and Using Derivative Notation2.3 Estimating Derivatives of a Function at a Point2.4 Connecting Differentiability and Continuity: Determining When Derivatives Do and Do Not Exist2.5 Applying the Power Rule2.6 Derivative Rules: Constant, Sum, Difference, and Constant Multiple2.7 Derivatives of cos x, sin x, e^x, and ln x2.8 The Product Rule2.9 The Quotient Rule2.10 Finding the Derivatives of Tangent, Cotangent, Secant, and/or Cosecant Functions3.1 The Chain Rule3.2 Implicit Differentiation3.3 Differentiating Inverse Functions3.4 Differentiating Inverse Trigonometric Functions3.5 Selecting Procedures for Calculating Derivatives3.6 Calculating Higher-Order Derivatives4.1 Interpreting the Meaning of the Derivative in Context4.2 Straight-Line Motion: Connecting Position, Velocity, and Acceleration4.3 Rates of Change in Applied Contexts Other Than Motion4.4 Introduction to Related Rates4.5 Solving Related Rates Problems4.6 Approximating Values of a Function Using Local Linearity and Linearization4.7 Using L’Hospital’s Rule for Determining Limits of Indeterminate Forms5.1 Using the Mean Value Theorem5.2 Extreme Value Theorem, Global Versus Local Extrema, and Critical Points5.3 Determining Intervals on Which a Function Is Increasing or Decreasing5.4 Using the First Derivative Test to Determine Relative (Local) Extrema5.5 Using the Candidates Test to Determine Absolute (Global) Extrema5.6 Determining Concavity of Functions over Their Domains5.7 Using the Second Derivative Test to Determine Extrema5.8 Sketching Graphs of Functions and Their Derivatives5.9 Connecting a Function, Its First Derivative, and Its Second Derivative5.10 Introduction to Optimization Problems5.11 Solving Optimization Problems5.12 Exploring Behaviors of Implicit Relations6.1 Exploring Accumulations of Change6.2 Approximating Areas with Riemann Sums6.3 Riemann Sums, Summation Notation, and Definite Integral Notation6.4 The Fundamental Theorem of Calculus and Accumulation Functions6.5 Interpreting the Behavior of Accumulation Functions Involving Area6.6 Applying Properties of Definite Integrals6.7 The Fundamental Theorem of Calculus and Definite Integrals6.8 Finding Antiderivatives and Indefinite Integrals: Basic Rules and Notation6.9 Integrating Using Substitution6.10 Integrating Functions Using Long Division and Completing the Square6.11 Integrating Using Integration by Parts6.12 Using Linear Partial Fractions6.13 Evaluating Improper Integrals6.14 Selecting Techniques for Antidifferentiation7.1 Modeling Situations with Differential Equations7.2 Verifying Solutions for Differential Equations7.3 Sketching Slope Fields7.4 Reasoning Using Slope Fields7.5 Approximating Solutions Using Euler’s Method7.6 Finding General Solutions Using Separation of Variables7.7 Finding Particular Solutions Using Initial Conditions and Separation of Variables7.8 Exponential Models with Differential Equations7.9 Logistic Models with Differential Equations8.1 Finding the Average Value of a Function on an Interval8.2 Connecting Position, Velocity, and Acceleration of Functions Using Integrals8.3 Using Accumulation Functions and Definite Integrals in Applied Contexts8.4 Finding the Area Between Curves Expressed as Functions of x8.5 Finding the Area Between Curves Expressed as Functions of y8.6 Finding the Area Between Curves That Intersect at More Than Two Points8.7 Volumes with Cross Sections: Squares and Rectangles8.8 Volumes with Cross Sections: Triangles and Semicircles8.9 Volume with Disc Method: Revolving Around the x- or y-Axis8.10 Volume with Disc Method: Revolving Around Other Axes8.11 Volume with Washer Method: Revolving Around the x- or y-Axis8.12 Volume with Washer Method: Revolving Around Other Axes8.13 The Arc Length of a Smooth, Planar Curve and Distance Traveled9.1 Defining and Differentiating Parametric Equations9.2 Second Derivatives of Parametric Equations9.3 Finding Arc Lengths of Curves Given by Parametric Equations9.4 Defining and Differentiating Vector-Valued Functions9.5 Integrating Vector-Valued Functions9.6 Solving Motion Problems Using Parametric and Vector-Valued Functions9.7 Defining Polar Coordinates and Differentiating in Polar Form9.8 Find the Area of a Polar Region or the Area Bounded by a Single Polar Curve9.9 Finding the Area of the Region Bounded by Two Polar Curves10.1 Defining Convergent and Divergent Infinite Series10.2 Working with Geometric Series10.3 The nth Term Test for Divergence10.4 Integral Test for Convergence10.5 Harmonic Series and p-Series10.6 Comparison Tests for Convergence10.7 Alternating Series Test for Convergence10.8 Ratio Test for Convergence10.9 Determining Absolute or Conditional Convergence10.10 Alternating Series Error Bound10.11 Finding Taylor Polynomial Approximations of Functions10.12 Lagrange Error Bound10.13 Radius and Interval of Convergence of Power Series10.14 Finding Taylor or Maclaurin Series for a Function10.15 Representing Functions as Power Series
Quizzes
Practice Problems AP formula notes, graph references, and practice sets will be added here.

AP Calculus AB/BC · Unit 7 · Topic 7.4

Reasoning Using Slope Fields

Match solution curves, equilibrium behavior, and increasing or concave regions to a slope field.

1. Topic Focus

Model rates with differential equations, read slope fields, approximate solutions, solve separable equations, and interpret exponential or logistic models.

This topic: Match solution curves, equilibrium behavior, and increasing or concave regions to a slope field.

2. Key Relationship

\(y'>0\Rightarrow y\uparrow\)

Read every symbol with its domain, direction, units, and hypotheses before applying the relationship.

3. Visual Connection

Slope field reasoningA solution remains tangent to the local segments while their signs and changes reveal direction and concavity.

4. Worked Example

A solution cannot cross an equilibrium line when uniqueness conditions hold.

Write the governing relationship first, carry out the algebra cleanly, and finish with a sentence that answers the mathematical question.

5. Concept Development

A slope field turns the local rule \(y'=F(x,y)\) into qualitative information about entire solution curves. A solution through \((x_0,y_0)\) must pass through that point smoothly and remain tangent to the nearby field segments as \(x\) moves both forward and backward.

A reasoning checklist

  1. Locate the initial point. It selects one curve from the family represented by the field.
  2. Read the sign of \(y'\). Positive segments mean the solution increases; negative segments mean it decreases.
  3. Track changing steepness. Slopes becoming more positive indicate concave up behavior; slopes becoming less positive or more negative indicate concave down behavior.
  4. Find zero-slope sets. Decide whether each is merely a nullcline or an equilibrium solution.
  5. Respect barriers and singularities. A solution cannot pass through a point where the equation is undefined, and equilibrium rows are barriers when standard uniqueness conditions hold.
  6. Describe long-term behavior cautiously. State what the visible field supports, such as approaching a level, moving away, or remaining bounded.

Increasing, decreasing, and horizontal tangents

Field along the solutionConclusion
\(F(x,y)>0\)the solution is increasing
\(F(x,y)<0\)the solution is decreasing
\(F(x,y)=0\)the solution has a horizontal tangent at that point
sign changes from \(+\) to \(-\)a local maximum is possible
sign changes from \(-\) to \(+\)a local minimum is possible

A solution may cross a curved nullcline. At the crossing it has a horizontal tangent, and the sign on the two sides determines whether the point is a local extremum. By contrast, a horizontal nullcline \(y=c\) is an equilibrium only if \(F(x,c)=0\) for every relevant \(x\).

Equilibrium solutions and stability

For an autonomous equation \(y'=g(y)\), solve \(g(c)=0\) to find constant solutions \(y=c\). A sign chart or phase line classifies nearby motion:

Direction below \(c\)Direction above \(c\)Classification
up toward \(c\)down toward \(c\)stable: nearby solutions approach
down away from \(c\)up away from \(c\)unstable: nearby solutions separate
up or downthe same direction as belowsemistable: approaches from one side only

Concavity from the field

Concavity depends on how the slope changes along the chosen solution, not merely from left to right across a fixed row. If tangent slopes increase as the curve advances, then \(y''>0\); if they decrease, then \(y''<0\). When algebra is available, differentiating the differential equation confirms the visual reasoning:

\(y''=F_x(x,y)+F_y(x,y)y'.\)

For an autonomous equation \(y'=g(y)\), this becomes \(y''=g'(y)g(y)\). The formula is optional support; a clear slope-field argument can establish the same qualitative conclusion.

Can solution curves cross?

If \(F\) and the conditions ensuring local uniqueness are satisfied near a point, two distinct solutions cannot cross there: an intersection would give the same initial point two different solution curves. In typical AP examples with smooth right-hand sides, this means equilibrium curves and already-drawn solution curves act as barriers. Do not apply this claim across a singularity or when uniqueness is not guaranteed.

From one curve to a family

The field represents a family of solution curves. Different initial values select different members, but every valid member must follow the same local segments. Curves may share qualitative behavior, such as approaching one stable equilibrium, without being vertical translations of one another.

AP justification habit: Support each claim with a field feature: “the solution decreases because the segments are negative,” “it is concave up because slopes increase along the curve,” or “it approaches the equilibrium because segments on both sides point toward it.”

6. Detailed Worked Example and Error Check

Example 1: Cooling toward equilibrium

Consider \(y'=2-y\). The equilibrium is \(y=2\). Above it, slopes are negative; below it, slopes are positive.

  • If \(y(0)=5\), the solution decreases toward \(2\).
  • If \(y(0)=0\), the solution increases toward \(2\).
  • If \(y(0)=2\), the solution remains constant.

The upper solution is concave up because its negative slopes become less negative. The lower solution is concave down because its positive slopes become less positive. Algebra confirms this: \(y''=-y'\).

Example 2: Two equilibria with different stability

For \(y'=y(y-3)\), the equilibria are \(y=0\) and \(y=3\). A sign chart gives

\(\begin{array}{c|ccccc}y&(-\infty,0)&0&(0,3)&3&(3,\infty)\\ \hline y'&+&0&-&0&+\end{array}\)

Below \(0\), solutions rise; between \(0\) and \(3\), they fall; above \(3\), they rise. Therefore \(y=0\) attracts from both sides and is stable, while \(y=3\) repels from both sides and is unstable.

Example 3: A semistable equilibrium

For \(y'=(y-1)^2\), the only equilibrium is \(y=1\), and every non-equilibrium slope is positive. Solutions below \(1\) rise toward the equilibrium, while solutions above \(1\) rise away from it. The equilibrium is semistable.

Example 4: Crossing a non-equilibrium nullcline

For \(y'=x-y\), the nullcline is \(y=x\). It is not an equilibrium because it is not a horizontal constant solution. Above the line, \(x-y<0\), so solutions decrease; below it, they increase. A solution that crosses from above the line to below it has a horizontal tangent and changes from decreasing to increasing, producing a local minimum.

Example 5: Logistic behavior without solving

For

\(P'=P\left(1-\frac{P}{100}\right),\)

the equilibria are \(P=0\) and \(P=100\). For \(0<P<100\), the population increases and remains between the equilibrium barriers. Field segments become steepest near \(P=50\), so a positive solution is concave up below \(50\), concave down above \(50\), and approaches \(100\).

Example 6: Choosing a curve from a family

Suppose the field is generated by \(y'=-2y\) and a curve must pass through \((0,3)\). The correct curve begins above the equilibrium \(y=0\), decreases, remains above the axis, and flattens toward it. A curve that crosses the axis or initially rises contradicts the field.

Example 7: Analytic confirmation of concavity

For \(y'=x+y\), differentiate along a solution:

\(y''=1+y'=1+x+y.\)

At \((0,0)\), the solution has \(y'=0\) and \(y''=1>0\). Thus it has a horizontal tangent and is locally concave up, consistent with a local minimum.

Example 8: Bounds from equilibrium barriers

For \(y'=y(4-y)\), solutions with \(0<y(0)<4\) have positive slope. They cannot cross \(y=0\) or \(y=4\) in a smooth uniqueness setting because both are equilibrium solutions. Therefore the solution remains bounded between \(0\) and \(4\) while increasing toward \(4\).

Common reasoning errors

  • Drawing a curve that passes through the initial point but is not tangent to nearby segments.
  • Calling every zero-slope curve an equilibrium solution.
  • Inferring concavity from the sign of \(y'\); increasing does not automatically mean concave up.
  • Allowing a solution to cross a smooth equilibrium barrier.
  • Classifying stability from only one side of an equilibrium.
  • Claiming a precise limiting value beyond what the visible field or equation supports.

7. AP Reasoning Routine

Translate the context into a rate equation, verify candidate solutions by substitution, carry constants through integration, and apply initial conditions last.

  • Identify the representation and requested quantity.
  • State the rule or theorem and verify its conditions.
  • Keep exact values until the final requested approximation.
  • Interpret sign, units, interval, and context.
AP Checkpoint

Use slope-field or sign reasoning; do not solve the differential equations explicitly.
(a) For \(y'=-3y\) with \(y(0)=4\), describe monotonicity, concavity, bounds, and long-term behavior.
(b) For \(y'=y(y-2)\), identify and classify all equilibria.
(c) Classify the equilibrium of \(y'=(y+1)^2\) and describe motion on each side.
(d) For \(y'=x-y\), identify the nullcline, state the sign above and below it, and explain why the nullcline is not an equilibrium solution.
(e) For \(y'=1-y^2\), identify each equilibrium and classify its stability.
(f) For \(P'=0.2P(1-P/600)\) with \(0<P(0)<600\), describe monotonicity, the concavity change, and the limiting level suggested by the field.
(g) A field has horizontal segments on \(y=4\), positive slopes below, and negative slopes above. Classify \(y=4\) and describe a solution through \((0,7)\).
(h) Could a solution of \(y'=y(2-y)\) starting at \(y(0)=1\) cross the equilibrium \(y=2\) in a region where uniqueness holds? Explain.
(i) Along a solution curve, tangent slopes change from \(-3\) to \(-1\) to \(0\) as \(x\) increases. State monotonicity and concavity on that portion.
(j) For \(y'=x+y\), determine \(y'\) and \(y''\) at \((0,0)\), then classify the local shape.

Check the solution

(a) Above \(y=0\), slopes are negative, so the solution decreases. Since \(y''=-3y'=9y>0\), it is concave up. It remains between \(0\) and \(4\) and approaches the stable equilibrium \(0\).
(b) Equilibria are \(y=0\) and \(y=2\). Slopes are positive below \(0\), negative between \(0\) and \(2\), and positive above \(2\). Thus \(y=0\) is stable and \(y=2\) is unstable.
(c) \(y=-1\) is semistable. Slopes are positive on both sides: solutions below rise toward \(-1\), while solutions above rise away.
(d) The nullcline is \(y=x\). Slopes are negative above it and positive below it. The line is not an equilibrium because an equilibrium must be a constant horizontal solution \(y=c\).
(e) Equilibria are \(y=-1\) and \(y=1\). Slopes are negative below \(-1\), positive between them, and negative above \(1\). Thus \(y=-1\) is unstable and \(y=1\) is stable.
(f) The population increases while it lies between \(0\) and \(600\). It is concave up below \(300\), concave down above \(300\), and approaches \(600\).
(g) Segments on both sides point toward \(y=4\), so it is stable. The solution through \((0,7)\) decreases, remains above \(4\), and flattens as it approaches \(4\).
(h) No. The line \(y=2\) is an equilibrium solution and acts as a barrier under uniqueness; the solution from \(y=1\) increases toward it without crossing.
(i) The slopes remain negative, so the solution is decreasing. They increase from \(-3\) toward \(0\), so the curve is concave up.
(j) At \((0,0)\), \(y'=0\). Differentiating gives \(y''=1+y'=1\), so the solution has a horizontal tangent and is locally concave up, indicating a local minimum.