Concept understanding — Straight Lines — Forms of the Equation
The general (linear) equation of a straight line is ax+by+c=0, where a,b are not both zero; the set of solutions of any such equation is a straight line in the plane. Because dividing through by b (or a) removes one constant, every line's equation genuinely contains only two independent arbitrary constants — so exactly two independent pieces of information (two points, or a point and a slope, or two intercepts, etc.) are enough to pin a line down uniquely.
Slope. The angle of inclinationθ of a line is the angle it makes with the x-axis, measured counter-clockwise; the slopem=tanθ (undefined when θ=π/2, i.e. for a vertical line). Equivalently, through two points (x1,y1),(x2,y2) with x1=x2, m=x2−x1y2−y1; from the general form, m=−a/b (b=0). Three points are collinear exactly when the slope of any one pair equals the slope of another pair sharing a point.
Intercepts. The x-intercept is where a line meets the x-axis (y=0); the y-intercept is where it meets the y-axis (x=0). (x=0 is itself the equation of the y-axis; y=0 is the equation of the x-axis.)
The six forms (two conditions each, all interconvertible by algebra):
Normal length p, angle α of the normal with the x-axis
xcosα+ysinα=p
Parametric, through (x1,y1) at inclination θ, parameter r = signed distance from (x1,y1)
cosθx−x1=sinθy−y1=r
Special cases of slope-intercept form: b=0,m=0 gives a line through the origin, y=mx; b=0,m=0 gives the x-axis itself, y=0; b=0,m=0 gives a horizontal line y=b. The point-slope form breaks down for a line parallel to the y-axis (slope undefined); such a line is simply x=x1. A line through the origin, or a horizontal/vertical line, cannot be written in intercept form (an intercept would be 0 or undefined).
General form to other forms. For Ax+By+C=0 (A,B not both 0): slope =−A/B, y-intercept =−C/B (when B=0); x-intercept =−C/A, y-intercept =−C/B (when A,B,C all nonzero); normal form is obtained by dividing through by ±A2+B2, choosing the sign so the resulting constant (the normal length p) comes out positive: cosα=∓A/A2+B2, sinα=∓B/A2+B2, p=∣C∣/A2+B2.
Tip
A real-world quantity that changes at a constant rate (speed, population growth, spring stretch per unit weight, a linearly-billed cost) is exactly a straight-line relationship — identify the two data points or the rate (slope) and one value (intercept/point) given, then apply the matching form above.
Each part needs only two independent pieces of data through (1,1) — a second point, a slope, or a normal-form angle — then the matching one of the six forms gives the line directly.
(i) two points (1,1),(0,−4): slope =5
(ii) point-slope with m=3
(iii) two points (1,1),(−2,3)
(iv) normal form with α=60∘
✓Final answer
(i) y=5x−4 (ii) 3x−y=2 (iii) 2x+3y=5 (iv) x+3y=1+3
Each part fixes the line through (1,1) with one more piece of data, then uses the matching standard form (two-point, point-slope, or normal form).
Four independent sub-problems, each solved by picking the form that fits the data given.
Step 1. Part (i) — y-intercept −4. A y-intercept of −4 means the line also passes through (0,−4). Using the two-point form on (1,1) and (0,−4):
m=1−01−(−4)=5
Point-slope through (0,−4): y−(−4)=5(x−0)⇒y=5x−4.
Step 2. Part (ii) — slope 3 through (1,1). Point-slope form: y−1=3(x−1)=3x−3, so y=3x−2, i.e. 3x−y=2.
Step 3. Part (iii) — through (1,1) and (−2,3). Slope:
m=−2−13−1=−32=−32
Point-slope through (1,1): y−1=−32(x−1). Multiply by 3: 3y−3=−2x+2, so 2x+3y=5.
Step 4. Part (iv) — normal from the origin at 60∘. "The perpendicular from the origin makes an angle 60∘ with the x-axis" describes the normal formxcosα+ysinα=p with α=60∘; p (the length of that perpendicular) is unknown and is fixed by requiring the line to pass through (1,1):
1⋅cos60∘+1⋅sin60∘=p⇒p=21+23=21+3
So the line is xcos60∘+ysin60∘=21+3, i.e. 2x+23y=21+3. Multiplying by 2: x+3y=1+3.
✓Final answer
(i) y=5x−4 (ii) 3x−y=2 (iii) 2x+3y=5 (iv) x+3y=1+3
In (i), forgetting that a y-intercept of −4 means the point is (0,−4), not (−4,0).
In (iv), confusing the angle of the line itself with the angle of the perpendicular (normal) from the origin — they are different unless p happens to make them equal.