Integration
Interactive curriculum lessons, worked examples, and geometric problem-solving techniques designed to help Kenyan students master CBC, KPSEA, KCSE, and IGCSE mathematics.
First Principles
Objective: Master polynomial integration as the reverse process of differentiation and use definite integrals to compute exact areas under curves.
(a) Concrete African Scenario
Consider a community water reservoir in Machakos harvesting runoff during rainy seasons. The rate of water inflow \(r(t)\) in cubic metres per hour varies continuously throughout the storm. To determine the total water volume accumulated in the dam, we slice the duration into short time intervals \(\Delta t\), compute volume slices \(r(t) \times \Delta t\), and add them up. As the intervals become infinitesimally small, this summation transforms into an integral.
(b) Geometric Insight
Integration provides the exact area bounded by a curve \(y=f(x)\), the \(x\)-axis, and vertical lines \(x=a\) and \(x=b\). In calculus, this limit of Riemann sums as \(n \to \infty\) (or strip width \(dx \to 0\)) is written as:
\[\lim_{n \to \infty} \sum_{i=1}^{n} f(x_i)\,\Delta x = \int_{a}^{b} f(x)\,dx\]
(c) The Fundamental Theorem & Antidifferentiation
Integration is the exact inverse operation of differentiation (anti-differentiation). If \(\frac{d}{dx}[F(x)] = f(x)\), then \(\int f(x)\,dx = F(x) + C\). When computing definite integrals between boundary limits, the arbitrary constant \(C\) subtracts away: \(\int_{a}^{b} f(x)\,dx = [F(x)]_a^b = F(b) - F(a)\).
Key Takeaway: Differentiation breaks down a function into its instantaneous rate of change (gradient), whereas integration accumulates rates of change back into the total net quantity (area).
Key Formulas
Power Rule: Increase the index/exponent by 1, divide the term by the new exponent, and include the constant of integration \(C\).
Constant Rule: Integrating a constant scalar \(k\) yields \(kx + C\) (since \(k = kx^0\)).
Linearity & Sum Rule: Integrate polynomials term by term, preserving coefficients.
Definite Integral: Evaluates the net signed area bounded by \(f(x)\) from \(x=a\) to \(x=b\).
Physical Area: When curves dip below the \(x\)-axis, separate the integral at the roots and take the absolute value of negative regions.
Worked Examples
- Step 1: Integrate each term independently using the power rule \(\int x^n\,dx = \frac{x^{n+1}}{n+1}\). \[\int 6x^2\,dx = 6\left(\frac{x^3}{3}\right) = 2x^3\]
- Step 2: Integrate the linear term: \[\int -4x\,dx = -4\left(\frac{x^2}{2}\right) = -2x^2\]
- Step 3: Integrate the constant term: \[\int 5\,dx = 5x\]
- Step 4: Combine all terms and append the constant of integration \(C\): \[2x^3 - 2x^2 + 5x + C\]
Final Answer: \(2x^3 - 2x^2 + 5x + C\)
- Step 1: Find the antiderivative \(F(x)\): \[F(x) = \frac{3x^3}{3} - \frac{2x^2}{2} + 4x = x^3 - x^2 + 4x\]
- Step 2: Evaluate at the upper limit \(x = 3\): \[F(3) = (3)^3 - (3)^2 + 4(3) = 27 - 9 + 12 = 30\]
- Step 3: Evaluate at the lower limit \(x = 1\): \[F(1) = (1)^3 - (1)^2 + 4(1) = 1 - 1 + 4 = 4\]
- Step 4: Apply the Fundamental Theorem \(F(3) - F(1)\): \[30 - 4 = 26\]
Final Answer: \(26\)
- Step 1: Identify where the curve intersects the \(x\)-axis to check for regions below the axis: \[3x^2 - 12x + 9 = 0 \implies 3(x-1)(x-3) = 0 \implies x = 1, x = 3\]
- Step 2: Determine sign of \(y\) across intervals:
- On \([0,1]\): \(y > 0\) (above \(x\)-axis)
- On \([1,3]\): \(y < 0\) (below \(x\)-axis)
- On \([3,4]\): \(y > 0\) (above \(x\)-axis)
- Step 3: Antiderivative \(F(x) = x^3 - 6x^2 + 9x\).
- Step 4: Compute each section:
- \(A_1 = \int_0^1 (3x^2 - 12x + 9)\,dx = [F(1) - F(0)] = (1 - 6 + 9) - 0 = 4\)
- \(A_2 = \int_1^3 (3x^2 - 12x + 9)\,dx = [F(3) - F(1)] = (27 - 54 + 27) - 4 = 0 - 4 = -4\) \(\implies |{-4}| = 4\)
- \(A_3 = \int_3^4 (3x^2 - 12x + 9)\,dx = [F(4) - F(3)] = (64 - 96 + 36) - 0 = 4 - 0 = 4\)
- Step 5: Sum absolute areas: \(\text{Total Area} = 4 + 4 + 4 = 12\) sq units.
Final Answer: \(12\) square units
Common Mistakes
Real World
1. KenGen Hydroelectric Inflow (Sondu Miriu Dam): Turbines generate power based on accumulated water volume. When rain gauges measure variable river discharge rate \(Q(t) = 4t - t^2\) m\(^3\)/s during a storm, engineers calculate total stored water over 4 hours by evaluating \(\int_0^4 (4t - t^2)\,dt\).
2. Matatu Kinematics on the Thika Superhighway: A GPS tracker logs a 14-seater matatu accelerating from a speed bump. Given acceleration \(a(t) = 3t\) m/s\(^2\), integrating acceleration gives velocity \(v(t) = \int a(t)\,dt\), and integrating velocity gives the exact distance travelled along the highway.
3. Irregular Agricultural Land Surveying in Mwea: Rice paddies bounded by natural winding river bends cannot be measured with simple \(L \times W\) formulas. Surveyors model river boundaries with polynomial functions \(y = f(x)\) and integrate over boundary coordinates to determine exact plot hectarage for land titles.
4. Industrial Coffee Processing in Kiambu: During peak harvest, coffee cherries are fed into a pulping machine at a variable rate \(R(t) = 12t - 3t^2\) tonnes/hour. Evaluating the integral over operating hours provides total tonnage processed for batch quality control.
Practice