Video summary
All of Straight Line Graphs in 20 Minutes! | Chapter 5 | A-Level Pure Maths Revision
Main summary
Key takeaways
Main ideas / lessons covered (Chapter 5: Straight Line Graphs)
1) Equation of a line (using gradient)
Given two coordinate points, ((x_1, y_1)) and ((x_2, y_2)), first find the gradient (m):
[ m=\frac{y_2-y_1}{x_2-x_1} ]
This is interpreted as change in (y) over change in (x).
Then use the point-slope form:
[ y-y_1=m(x-x_1) ]
If needed, substitute and simplify to write in slope-intercept form:
[ y=mx+c ]
Worked example (key steps): Find the line through ((5,7)) and ((3,-1)).
-
Gradient: [ m=4 ]
-
Substitute into (y-y_1=m(x-x_1)) to obtain: [ y=4x-13 ]
2) Perpendicular lines (finding the perpendicular gradient)
If a line has gradient (m), then a line perpendicular to it has gradient:
[ m_\perp=-\frac{1}{m} ]
Then use the perpendicular gradient to form the equation of the line through a given point.
Worked example (key steps): Perpendicular to (y=2-3x) through ((6,5)).
- Original line gradient: (-3)
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Perpendicular gradient: [ m_\perp=\frac{1}{3} ]
-
Use (y=\frac{1}{3}x+c)
- Substitute ((6,5)) to solve:
- (c=3)
Result:
[ y=\frac{1}{3}x+3 ]
3) Intersection of two lines + triangle area using coordinate geometry
To find the intersection and the area of a triangle formed:
- Rearrange each line into a usable form (commonly (y=mx+c)).
- Find the intersection point (A) by solving the two equations simultaneously.
- Find point (B) where one line meets the (x)-axis:
- set (y=0) and solve for (x).
-
Use triangle area: [ \text{Area}=\frac{1}{2}\times(\text{base})\times(\text{height}) ]
- Height is the (y)-coordinate of (A)
- Base is the horizontal distance along the (x)-axis from the origin to (B)
Worked example (key steps): Lines:
- (l_1: 4x-y=0 \Rightarrow y=4x)
- (l_2: 2x+3y-21=0 \Rightarrow y=-\frac{2}{3}x+7)
Intersection (A):
- Substitute (y=4x) into (2x+3y-21=0): [ x=\frac{3}{2},\quad y=6 ]
Point (B) (where (l_2) meets the (x)-axis):
- Set (y=0): [ 2x-21=0 \Rightarrow x=\frac{21}{2}=10.5 ]
Triangle area: [ \frac{1}{2}\times 10.5 \times 6=\frac{63}{2} ]
4) Modelling with straight lines (linear relationship in context)
A common model is:
[ d=at+b ]
where:
- (d) = depth
- (t) = time
- (a) = gradient (rate of change of depth per second)
- (b) = intercept (depth at (t=0))
Worked example (container leaking):
Given:
- Start: (t=0), (d=19.1)
- After 100 seconds: (d=6.1)
Find the gradient:
[ a=\frac{6.1-19.1}{100-0}=\frac{-13}{100}=-0.13 ]
Model (using (b=19.1)):
[ d=-0.13t+19.1 ]
Interpretation:
- (a=-0.13): depth decreases by (0.13) units per second
- (b=19.1): initial depth
Find when the container is empty ((d=0)):
[ 0=-0.13t+19.1 ] [ t=146.9\text{ seconds} ]
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