The principle of constant gradient ensures that the rate of change between the x and y variables is identical for both lines. This geometric property prevents the lines from ever converging or diverging.
If two lines have equations and , they are parallel if and only if . If as well, the lines are considered coincident (the same line).
Parallelism is a transitive property: if Line A is parallel to Line B, and Line B is parallel to Line C, then Line A is also parallel to Line C.
Step 1: Identify the Gradient: Determine the gradient () of the given line. If the equation is not in form, rearrange it first.
Step 2: Set up the New Equation: Use the same gradient for the new line, writing it as , where is the unknown y-intercept.
Step 3: Substitute Coordinates: Plug the coordinates of the point the new line passes through into the equation to solve for .
Step 4: Finalize: Write the complete equation using the original gradient and the newly calculated y-intercept.
| Relationship | Gradient Condition | Intersection |
|---|---|---|
| Parallel | Never | |
| Perpendicular | Exactly once at | |
| Intersecting | Exactly once | |
| Coincident | AND | Infinitely many points |
Check the Form: Always ensure the equation is in the form before identifying the gradient. A common trap is an equation like , where the gradient is , not .
Verify the Gradient: In multiple-choice questions, immediately eliminate any options that do not have the exact same gradient as the reference line.
Substitution Check: After finding the new equation, substitute the given point back into it. If the equation does not balance, a calculation error occurred during the solving for .
Watch for Vertical Lines: Lines in the form are parallel to each other. They have an undefined gradient, so the standard method does not apply.
The Intercept Trap: Students often mistakenly think parallel lines must have the same y-intercept. If they have the same intercept and gradient, they are the same line, not distinct parallel lines.
Sign Errors: When rearranging equations (e.g., from ), failing to account for negative signs often leads to the wrong gradient, resulting in a line that is not parallel.
Reciprocal Confusion: Confusing parallel gradients (which are equal) with perpendicular gradients (which are negative reciprocals) is a frequent source of error.