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International Baccalaureate · DP 2: Applications and Interpretation HL

Revision: Functions and Modelling

⌚ ~35 min ▢ 4 blocks ✓ 16 exercises ➣ Prerequisites : Trigonometric Functions, Modelling
I Toolbox: Variation Models
Recappreviously studied — click to reread
Definition — Proportion with a Power
Let \(n\) be a positive whole number and \(k\) a nonzero number.
  • \(y\) is directly proportional to \(x^n\) when \(y = kx^n\) for every pair of matching values. We write \(y \propto x^n\). For \(n = 2\), \(y\) is proportional to the square of \(x\); for \(n = 3\), to the cube of \(x\).
  • \(y\) is inversely proportional to \(x^n\) when \(y = \dfrac{k}{x^n}\) for every pair of matching values, with \(x \neq 0\). We write \(y \propto \dfrac{1}{x^n}\). For \(n = 2\), this is the inverse-square law.
For \(n = 1\), these are direct proportion and inverse proportion.
Proposition — Asymptotic Behaviour
For \(k \neq 0\) and \(n\) a positive integer, the graph of the inverse variation model \(y = \dfrac{k}{x^n} = kx^{-n}\) (the form \(ax^m\) with \(m < 0\)) has the \(y\)-axis, \(x = 0\), as a vertical asymptote and the \(x\)-axis, \(y = 0\), as a horizontal asymptote.
Method — Recognising the Law from a Table
For each column of the table (with \(x \neq 0\)):
  1. compute \(\dfrac{y}{x}\) and \(xy\), then, if neither is constant, \(\dfrac{y}{x^2}\) and \(x^2y\), then \(\dfrac{y}{x^3}\) and \(x^3y\);
  2. keep the calculation that gives the same number in every column: if \(\dfrac{y}{x^n}\) is constant, \(y \propto x^n\); if \(x^ny\) is constant, \(y \propto \dfrac{1}{x^n}\); that number is the constant \(k\);
  3. if no calculation is constant, the table shows none of the laws tested here (\(n = 1\), \(2\) or \(3\)) — one column that breaks the pattern is enough.
Two columns in which \(x\) is doubled give a first guess (Remark “Telling the Laws Apart”), which the calculation then confirms.
Example
Each table comes from an experiment. Determine the variation model that each table follows.
  1. The air resistance \(R\), in newtons, on a cyclist riding at \(v\) metres per second.
    \(v\) \(2\) \(4\) \(6\) \(8\)
    \(R\) \(1.2\) \(4.8\) \(10.8\) \(19.2\)
    Then predict the air resistance at \(10\) metres per second.
  2. The time \(T\), in hours, that \(w\) workers need to paint a hall.
    \(w\) \(2\) \(3\) \(4\) \(6\)
    \(T\) \(18\) \(12\) \(9\) \(6\)

  1. \(R\) increases with \(v\), so we test direct variation with a power of \(v\): we compute \(\frac{R}{v}\), then \(\frac{R}{v^2}\), for every data point.
    \(v\) \(2\) \(4\) \(6\) \(8\)
    \(\frac{R}{v}\) \(0.6\) \(1.2\) \(1.8\) \(2.4\)
    \(\frac{R}{v^2}\) \(0.3\) \(0.3\) \(0.3\) \(0.3\)
    The ratio \(\frac{R}{v}\) is not constant, so \(R\) does not vary directly with \(v\). The ratio \(\frac{R}{v^2}\) is constant, equal to \(0.3\): \(R\) varies directly with the square of \(v\), \(R \propto v^2\), and \(R = 0.3v^2\). Check with doubling: from \(v = 2\) to \(v = 4\), \(R\) is multiplied by \(\frac{4.8}{1.2} = 4 = 2^2\), as a square law predicts. At \(v = 10\): $$R = 0.3 \times 10^2 = 30.$$ The model predicts an air resistance of \(30\) newtons.
  2. \(T\) decreases when \(w\) increases, so we test inverse variation: we compute the product \(wT\) for every data point: \(2 \times 18 = 36\), \(3 \times 12 = 36\), \(4 \times 9 = 36\), \(6 \times 6 = 36\). The product is constant, so \(T\) varies inversely with \(w\): \(T \propto \frac{1}{w}\) and \(T = \frac{36}{w}\). The constant \(36\) is the number of hours one worker alone would need, if the law held for one worker: \(w = 1\) lies outside the data, so this reading is an extrapolation.

Skills to practice
  • Finding a Variation Model with a Power
II Toolbox: Sinusoidal Models in Degrees
Recappreviously studied — click to reread
Common real-world examples of sinusoidal models include phenomena that oscillate (fluctuate periodically):
  • \(D(t)\) is the depth of water at a shore \(t\) hours after midnight
  • \(T(n)\) is the temperature of a city \(n\) days after January 1st
  • \(H(t)\) is the vertical height above ground of a person \(t\) seconds after entering a Ferris wheel
Method — Modelling Periodic Data in Degrees
A quantity that repeats itself every \(P\) units of time in a smooth wave, rising and falling symmetrically about a middle value, can be modelled by \(y = a\sin(bt) + d\) or \(y = a\cos(bt) + d\), where the angle \(bt\) is measured in degrees.
  1. Principal axis: \(d = \dfrac{\text{maximum} + \text{minimum}}{2}\).
  2. Amplitude: \(|a| = \dfrac{\text{maximum} - \text{minimum}}{2}\).
  3. Period: one period is one full turn of \(360^\circ\), so \(b = \dfrac{360}{P}\), in degrees per unit of time (\(b > 0\)).
  4. Form and sign, read on the start of the data, at \(t = 0\):
    • on the principal axis and rising: \(y = a\sin(bt) + d\) with \(a > 0\);
    • on the principal axis and falling: \(y = a\sin(bt) + d\) with \(a < 0\);
    • at a maximum: \(y = a\cos(bt) + d\) with \(a > 0\);
    • at a minimum: \(y = a\cos(bt) + d\) with \(a < 0\).
    The time origin is chosen so that the data start at one of these four positions; data that start anywhere else need a horizontal translation of the curve.
  5. Check the model on a data point, and set the calculator to degree mode before using it.
Figure
Example
In a city of the southern hemisphere, the mean monthly temperature is highest in January, \(26^\circ\)C, and lowest in July, \(10^\circ\)C, and the pattern repeats every year. Let \(t\) be the time in months, with \(t = 0\) in January and \(t = 6\) in July.
  1. Find a model \(T(t) = a\cos(bt) + d\) for the mean monthly temperature, the angle \(bt\) being in degrees.
  2. Use the model to estimate the mean temperature in April (\(t = 3\)) and in May (\(t = 4\)).

  1. Following the Method:
    • principal axis: \(d = \dfrac{26 + 10}{2} = 18\);
    • amplitude: \(|a| = \dfrac{26 - 10}{2} = 8\);
    • the period is \(12\) months, so \(b = \dfrac{360}{12} = 30\) (degrees per month);
    • at \(t = 0\) the temperature is at its maximum: the form \(a\cos(bt) + d\) with \(a > 0\), so \(a = 8\).
    The model is \(T(t) = 8\cos(30t) + 18\). Check in July: \(T(6) = 8\cos 180^\circ + 18 = -8 + 18 = 10\), the minimum of the data.
  2. $$\begin{aligned}[t] T(3) &= 8\cos 90^\circ + 18 = 8 \times 0 + 18 = 18,\\ T(4) &= 8\cos 120^\circ + 18 = 8 \times \left(-\frac{1}{2}\right) + 18 = 14. \end{aligned}$$ The model estimates about \(18^\circ\)C in April and \(14^\circ\)C in May.
Figure

Skills to practice
  • Finding a Sinusoidal Model in Degrees
III Exam-Style Questions
Skills to practice
  • Working with Technology: Functions and Modelling
  • Working with Technology: Further Functions and Modelling