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Multivariable Calculus
Vectors and Dot Products
01Vectors, Components, and Length in Space02Scaling and Adding Vectors: The Parallelogram Rule03The Dot Product and the Law of Cosines04Finding Angles in Space With the Dot Product05The Perpendicularity Test and the Normal Vector to a PlaneProblem set0/10Problem set 20/10MIT problem set0/2
Determinants and the Cross Product
01The Component of a Vector Along Any Unit Direction02The 2x2 Determinant and the Area of a Parallelogram03The 3x3 Determinant and the Volume of a Box04The Cross Product and the Right-Hand Rule05The Triple Product and the Volume of a ParallelepipedProblem set0/10Problem set 20/10MIT problem set0/2
Matrices and Inverse Matrices
01Why Swapping a Cross Product Flips Its Sign02The Equation of a Plane Through Three Points03Matrix Multiplication: Rows Dotted With Columns04Matrices as Transformations: Identity and Rotation05The Inverse Matrix and Solving AX = B06Computing a 3x3 Inverse: Minors, Cofactors, AdjointProblem set0/10Problem set 20/10MIT problem set0/2
Planes and Square Systems
01Planes From a Point and a Normal Vector02Reading the Normal Vector Off a Plane Equation03Three Planes, One Point: Solving a 3x3 System04Invertibility, det A, and the Homogeneous System05When det A = 0: Coplanar Normals and a Line of SolutionsProblem set0/10Problem set 20/10
Parametric Lines and Curves
01Parametric Equations of a Line Through Two Points02Where a Line Meets a Plane, and When It Never Does03The Cycloid: Choosing a Parameter That Is Not Time04Deriving the Cycloid's Equations From Three Vectors05Is the Cycloid's Bottom a Corner? Taylor Expansion Finds a CuspProblem set0/10Problem set 20/10MIT problem set0/2
Velocity and Kepler's Law
01Velocity and Speed on the Cycloid: Why the Point Stops Dead02Acceleration Is a Vector: Turning at Constant Speed Still Counts03Arc Length and the Unit Tangent: v = T̂ ds/dt04Equal Areas in Equal Times: Kepler's Second Law and |r × v|05Kepler's Second Law Means the Force Is CentralProblem set0/10Problem set 20/10MIT problem set0/1
Functions of Several Variables
01Functions of Two Variables: Graphs as Surfaces, Built from Slices02Level Curves and Contour Plots: A Surface Drawn as a Flat Map03Reading Contour Plots: Domes, Bowls, Saddles and Mountain Passes04Partial Derivatives: Change One Variable, Hold the Other FixedProblem set0/10Problem set 20/10MIT problem set0/2
Optimization and Least Squares
01Approximation Formula: Changes in x and y Add, via the Tangent Plane02Critical Points: Where Both Partial Derivatives Are Zero03Minimum, Maximum or Saddle Point? Classifying by Completing the Square04Least Squares: The Best-Fit Line as a Minimization in a and b05Solving Least Squares: Best-Fit Lines, Exponentials and ParabolasProblem set0/10Problem set 20/10MIT problem set0/3
The Second Derivative Test
01Quadratic Critical Points: The Sign of 4ac − b² Decides02The Second Derivative Test: Classifying by the Sign of AC − B²03Global Min and Max of x + y + 1/(xy): Boundary and InfinityProblem set0/10Problem set 20/10MIT problem set0/1
Differentials and the Chain Rule
01The Total Differential: Why df Is Not Δf, and Its Three Uses02The Chain Rule: Why It Holds, a Worked Check, and the Product Rule03Chain Rule for a Change of Variables: Partials in Polar CoordinatesProblem set0/10Problem set 20/10MIT problem set0/1
Gradients and Constraints
01The Gradient Vector: Why It Is Perpendicular to Level Sets02Tangent Plane to a Surface From the Gradient: The Hyperboloid03Directional Derivatives and the Direction of Steepest AscentProblem set0/10Problem set 20/10MIT problem set0/2
01Lagrange Multipliers: Tangent Level Curves and ∇f = λ∇g02Solving the Lagrange Equations, and Why the Method Works03The Least-Area Gold Pyramid: Its Top Sits Over the IncenterProblem set0/10Problem set 20/10MIT problem set0/1
01Implicit Partial Derivatives: Differentiate the Constraint02Which Variable Is Held Constant? Subscript Notation03A Constrained Rate Three Ways: Differentials vs Chain RuleProblem set0/10Problem set 20/10MIT problem set0/3
Multiple Integrals
01The Heat Equation: A First Partial Differential Equation02Double Integrals: Volume Under a Surface by Slicing03Iterated Integrals Over a Square and a Quarter Disk04Exchanging the Order of Integration: Redraw the RegionProblem set0/10Problem set 20/10MIT problem set0/1
01Double Integrals in Polar Coordinates: Why dA = r dr dθ02Area, Mass, Averages and Center of Mass by Double Integrals03Moment of Inertia: Spinning a Disk About Its Center and Its RimProblem set0/10Problem set 20/10MIT problem set0/3
01Change of Variables: How a Substitution Rescales Area02The Jacobian: Why Every Polar Integral Carries an r03Change of Variables Start to Finish: x²y with u = x, v = xyProblem set0/10Problem set 20/10MIT problem set0/1
Vector Fields and Line Integrals
01Vector Fields: Sketching Constant, Radial and Rotating Fields02Work as a Line Integral: Computing ∫ F · dr Along a Path03Evaluating ∫ M dx + N dy: One Parameter Along the Curve04Line Integrals by Geometry: Work Around a Circle with F · T dsProblem set0/10Problem set 20/10MIT problem set0/1
01Work Around a Closed Curve: Integrating Piece by Piece02The Fundamental Theorem for Line Integrals: ∫ ∇f · dr03Path Independence and Why the Rotation Field Fails It04Conservative Fields: Four Equivalent PropertiesProblem set0/10Problem set 20/10MIT problem set0/1
01The Gradient Field Test: My = Nx, and Where It Breaks02Finding a Potential Function by Line Integrals03Finding a Potential Function by Partial Antiderivatives04Curl in the Plane: Measuring How a Field RotatesProblem set0/10Problem set 20/10MIT problem set0/2

Finding a Potential Function by Line Integrals

How does reading the fundamental theorem backwards turn a line integral along two straight pieces into the potential itself?


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Your summary note

    1. 1

      The fundamental theorem read backwards

      Write (x_1, y_1) = \int_C \vec F \cdot d\vec r + f(0,0)forapathfromtheorigin,validoncethetestpasses,andstatethat(0,0) for a path from the origin, valid once the test passes, and state that (0,0)forapathfromtheorigin,validoncethetestpasses,andstatethat(0,0) is a free constant.

    2. 2

      The two-piece path

      Record that on the hmBcaxis = 0and=0 and = 0and=0, and on the vertical piece = x_1and=0 and = 0and=0, and which integrand survives on each.

    3. 3

      The worked example ⟨4x2+8xy, 3y2+4x2⟩\langle 4x^2 + 8xy,\ 3y^2 + 4x^2\rangle⟨4x2+8xy, 3y2+4x2⟩

      Evaluate both pieces to reach = \tfrac43 x^3 + y^3 + 4x^2 y + c$, then check by taking the gradient.

    4. 4

      Other choices of path

      Redo the example with the hmBcaxis first to get the same potential, and note when the radial path is the better choice.

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