Sine function
period · amplitude · phase · shiftPeriod 2π/b; amplitude |a|; vertical shift k; horizontal shift h (right when h>0). Zeros every half-period at x=h+kπ/b.
Sketchbook fragment — graphs, identities, triangle laws, inverses, rotations.
Period 2π/b; amplitude |a|; vertical shift k; horizontal shift h (right when h>0). Zeros every half-period at x=h+kπ/b.
Cosine is sine shifted left by π/2. Even: cos(-x)=cos(x). Max at x=h+2πk, min at x=h+π+2πk. Dashed: reference cos(x).
Period π (half of sin/cos). Vertical asymptotes where cos x = 0: x = π/2 + kπ. Zeros at x = kπ. Always increasing on each branch.
Each reciprocal blows up where its partner is zero. Dashed lines = vertical asymptotes; faint curve = the parent sin/cos for reference.
Every point on the circle is (cos θ, sin θ). Cosine reads off horizontally, sine vertically. tan θ = y/x = slope of the radius. Sign chart: Q1 all+; Q2 sin+; Q3 tan+; Q4 cos+ (A-S-T-C).
Drop a perpendicular from the terminal-side point to the x-axis — the acute angle made with the axis is θ_ref. Read magnitude from the special triangle; pull the sign from the quadrant.
| θ | sin θ | cos θ | tan θ |
|---|---|---|---|
| $0$ | $0$ | $1$ | $0$ |
| $\pi/6$ | $\tfrac{1}{2}$ | $\tfrac{\sqrt3}{2}$ | $\tfrac{\sqrt3}{3}$ |
| $\pi/4$ | $\tfrac{\sqrt2}{2}$ | $\tfrac{\sqrt2}{2}$ | $1$ |
| $\pi/3$ | $\tfrac{\sqrt3}{2}$ | $\tfrac{1}{2}$ | $\sqrt3$ |
| $\pi/2$ | $1$ | $0$ | — |
Sine row counts up: √0/2, √1/2, √2/2, √3/2, √4/2. Cosine row counts down (mirror). Tangent = sine ÷ cosine.
Restrict sin to its one-to-one piece [-π/2, π/2], then invert. Output is always in range. arcsin(sin x) snaps to range, NOT identity for all x.
Restrict cos to [0, π] (monotone decreasing). Output is always non-negative; arccos(-1/2) = 2π/3, NOT -π/3.
Tangent's periodic branch on (-π/2, π/2) is the entire reals. Inverting gives an S-shaped curve squeezed between horizontal asymptotes. Endpoints excluded (open interval).
Primary identity is Pythagoras applied to (cos θ, sin θ, 1). Divide both sides by cos²θ for the tan/sec form, by sin²θ for the cot/csc form.
Memory: sine MIXES (sin-cos + cos-sin); cosine STAYS PURE (cos-cos − sin-sin). Sign in the output matches sign in the input for sine, FLIPS for cosine. Derives from the rotation-matrix product Rα·Rβ = Rα+β.
Cosine has THREE equivalent forms — pick whichever matches what you know. The 2cos²−1 form is the source of the cos half-angle; the 1−2sin² form is the source of the sin half-angle.
Solve the cos-double-angle forms for cos²/sin². "Power-reduction": a squared trig function becomes first-order in cos 2α — standard prep for integrating sin²/cos².
Use when you have an angle-side pair plus one more piece (AAS/ASA/SSA). SSA caveat: if you're given two sides and a non-included angle A, compute h = c sin A; then 0, 1, or 2 triangles depending on whether a falls below, on, between, or beyond h and c.
When C = π/2, cos C = 0 and the formula collapses to Pythagoras. Solved-for-angle form yields a unique angle in [0, π] — no SSA ambiguity. Use for SAS (find third side) or SSS (find any angle).
Drop altitude h = b sin C from the vertex of C. Area = ½ · base · height. The three permutations correspond to dropping the altitude from each of the three vertices.
Column 1 = where (1,0) lands = (cos θ, sin θ). Column 2 = where (0,1) lands = (-sin θ, cos θ). Determinant = 1, so rotations preserve area and length. Rα·Rβ = Rα+β — this is the engine of sum identities.
Sine: two families (principal + supplement), period 2π. Cosine: two families (± principal), period 2π. Tangent: one family, period π. For sin α = sin β: either α = β + 2πk or α = π − β + 2πk.
Two sinusoids of equal frequency add to one bigger sinusoid. Amplitude is the Pythagorean magnitude; phase is set by the ratio. Use to solve A cos x + B sin x = c: rewrite, then apply periodicity template.
| deg | rad | deg | rad |
|---|---|---|---|
| 0° | $0$ | 180° | $\pi$ |
| 30° | $\pi/6$ | 210° | $7\pi/6$ |
| 45° | $\pi/4$ | 225° | $5\pi/4$ |
| 60° | $\pi/3$ | 240° | $4\pi/3$ |
| 90° | $\pi/2$ | 270° | $3\pi/2$ |
| 120° | $2\pi/3$ | 300° | $5\pi/3$ |
| 135° | $3\pi/4$ | 315° | $7\pi/4$ |
| 150° | $5\pi/6$ | 360° | $2\pi$ |
1 rad ≈ 57.30°. DMS: x° y' z'' = x + y/60 + z/3600 decimal degrees.
Sin/tan are odd (reflect across x-axis flips y); cos is even (x-coord untouched). Co-function: function at complement equals co-function — "cosine" literally means "sine of complement". Quick reductions: cos(π−α)=−cos α, sin(π+α)=−sin α, cos(x+3π/2)=sin x.
Angle between two lines = difference of their inclinations = tan-difference identity applied to slopes. Denominator zero ⇒ perpendicular.
A bisector from a vertex splits the opposite side in the same ratio as the two adjacent sides. Same logic = Law of Sines applied to the two sub-triangles sharing the bisector.
Two shorter sides must reach across the longest. Violating any inequality = no triangle. Equality = degenerate (collinear). Quick check: sort the sides, then test whether the two smallest exceed the largest.
Triple-angle: stack sin(2x+x) + double-angle + Pythagorean. Tangent-form sin(2θ): useful when only tan is known (Weierstrass substitution). tan+cot collapses to 1/(sin θ cos θ).
The tail is not glued to the origin. A vector encodes how far and which way, not where. Slide the arrow around — same vector.
This is why we can add vectors tip-to-tail: an arrow's anchor is wherever you need it to be.
Anchor the tail at the origin. The tip's $(x, y)$ coordinates are the components.
Three notations, one object. The basis vectors $\mathbf{i} = \langle 1, 0\rangle$ and $\mathbf{j} = \langle 0, 1\rangle$ point east and north with unit length, so $a\mathbf{i} + b\mathbf{j}$ literally says "go $a$ east, then $b$ north."
The components are the legs of a right triangle whose hypotenuse is the vector. Pythagoras, no thinking required.
Classic worked example: $\vec{v} = \langle 3, 4\rangle \Rightarrow |\vec{v}| = \sqrt{9 + 16} = 5$. The 3-4-5 triple shows up everywhere — memorize it.
Magnitude is always $\geq 0$, and $=0$ only for the zero vector.
Magnitude times direction. Scale the unit-circle point $\langle\cos\theta, \sin\theta\rangle$ by $r$ and you stretch it to the right length while preserving direction.
Worked: $r = 10,\ \theta = 45° \Rightarrow \vec{v} = \langle 10\cos 45°, 10\sin 45°\rangle = \langle 5\sqrt 2, 5\sqrt 2\rangle \approx \langle 7.07, 7.07\rangle$.
Bearings measure clockwise from North, while math angles measure counterclockwise from East. They're complementary: $\theta = 90° - B$.
The trig swap: sine and cosine trade roles because the reference axis flipped. NαE means "start at North, rotate α toward East" — and the quadrant signs follow:
Calculator's $\arctan(b/a)$ returns only $(-90°, 90°)$ — that's Q1 and Q4 only. If your vector lives in Q2 or Q3, the calculator is silently lying.
Example. $\vec{t} = \langle -1, 3\rangle$ is in Q2. $\arctan(3/-1) = \arctan(-3) \approx -71.57°$. Add 180°: $\theta \approx 108.43°$. ✓
Rule: sketch the quadrant before trusting the calculator.
Geometric: place $\vec w$'s tail at $\vec v$'s tip; the sum is the arrow from $\vec v$'s tail to $\vec w$'s tip. Equivalently, build the parallelogram and take the diagonal.
Components just add. $\langle -5, 1\rangle + \langle 2, 6\rangle = \langle -3, 7\rangle$. Commutative and associative — order doesn't matter.
Two equivalent pictures: subtract components, or place tails together and draw from w's tip to v's tip.
The negative of $\vec w$ is just $\vec w$ flipped 180°. So subtraction is addition of the reversed vector.
$|\vec v - \vec w| \neq |\vec v| - |\vec w|$ in general — subtract first, then take magnitude.
Multiply each component by the scalar. Magnitude scales by $|c|$; sign of $c$ controls direction.
Two non-parallel vectors $\vec x, \vec y$ form a basis: every vector in the plane is some unique $a\vec x + b\vec y$.
The oblique lattice they generate is the plane — just with skewed grid lines.
Worked: $\vec v = \langle 5, -3\rangle,\ \vec x = \langle -4, 1\rangle,\ \vec y = \langle 3, -1\rangle$. System $-4a + 3b = 5,\ a - b = -3$ gives $a = 4, b = 7$. Verify: $4\langle -4,1\rangle + 7\langle 3,-1\rangle = \langle 5, -3\rangle$. ✓
Unique solution iff $x_1 y_2 - x_2 y_1 \neq 0$ (vectors not parallel).
Divide a vector by its own length and you get a length-1 arrow pointing the same way. The "pure direction" of $\vec v$.
The second form is THE foundational identity for the entire unit. Every other formula builds on "magnitude × direction."
Standard basis $\mathbf i = \langle 1, 0\rangle$ and $\mathbf j = \langle 0, 1\rangle$ are the unit vectors along the axes. In 3D add $\mathbf k = \langle 0, 0, 1\rangle$.
Every unit vector in 2D is a point on the unit circle. The bridge between trig (angles) and vectors (directions).
Magnitude check: $\sqrt{\cos^2\theta + \sin^2\theta} = 1$. ✓ At $\theta = 45°$: $\hat u = \langle\sqrt 2/2, \sqrt 2/2\rangle \approx \langle 0.707, 0.707\rangle$.
Multiplying by $r$ gives the polar form from card 04.
The dot product collapses two vectors into one number by pairing components.
$\vec v = \langle -2, 6\rangle$ and $\vec w = \langle 3, 4\rangle$: $\vec v \cdot \vec w = (-2)(3) + (6)(4) = -6 + 24 = 18$.
It's commutative, distributes over addition, and a scalar can move outside: $(c\vec v)\cdot\vec w = c(\vec v\cdot\vec w)$.
Same scalar as before, but written geometrically: the product of the magnitudes scaled by the cosine of the angle between them.
Derived from the Law of Cosines on the triangle with sides $\vec v, \vec w, \vec v - \vec w$. The squared-magnitude terms cancel, leaving the dot product on one side and $|\vec v||\vec w|\cos\theta$ on the other.
Aligned vectors ($\theta = 0$): dot = $|\vec v||\vec w|$. Anti-aligned ($\theta = 180°$): dot = $-|\vec v||\vec w|$. Perpendicular ($\theta = 90°$): dot = 0.
Solve the geometric form for $\theta$, then arccos.
Sign trichotomy:
Classify without computing $\theta$. (Caveat: positive can also mean parallel; negative can mean anti-parallel. Check parallelism first if unsure.)
Drop a perpendicular from $\vec v$'s tip to the line through $\vec w$. The "shadow" along $\vec w$ is the projection.
No cosines, no arccos, no magnitudes — just dot products. Works in any dimension.
Worked: $\vec v = \langle 3, 1\rangle,\ \vec w = \langle 2, 6\rangle$. $\vec v \cdot \vec w = 12$, $\vec w \cdot \vec w = 40$. $\text{proj}_{\vec w}\vec v = (12/40)\langle 2, 6\rangle = \langle 3/5, 9/5\rangle$.
Acute → projection along $\vec w$. Right → zero. Obtuse → projection opposite to $\vec w$. One formula, all cases.
The coefficients of any linear equation $ax + by = c$ form the normal vector $\vec n = \langle a, b\rangle$ perpendicular to the line. Varying $c$ slides the line parallel to itself.
Proof: pick two points $P_1, P_2$ on the line. $\vec n \cdot P_1 = c$ and $\vec n \cdot P_2 = c$. Subtract: $\vec n \cdot (P_2 - P_1) = 0$. Since $P_2 - P_1$ runs along the line, $\vec n$ is perpendicular to every direction on the line.
In 3D: $ax + by + cz = d$ is a plane with normal $\langle a, b, c\rangle$. Same trick, one dimension up.
The $2\times 2$ matrix that rotates any vector CCW by $\theta$. Apply via matrix-vector multiplication.
Sanity check at $\theta = 90°$: $R(90°) = \begin{bmatrix}0 & -1\\ 1 & \phantom{-}0\end{bmatrix}$. Apply to $\mathbf i = \langle 1, 0\rangle$: get $\langle 0, 1\rangle = \mathbf j$. ✓ — $\mathbf i$ rotates to $\mathbf j$.
Properties: $\det R = 1$ (area-preserving), $|R\vec v| = |\vec v|$ (isometry), $R(\theta)^{-1} = R(-\theta) = R(\theta)^T$.
Composition: $R(\alpha)R(\beta) = R(\alpha + \beta)$ — the angle-sum identities, packaged.
On a ramp at angle $\theta$, gravity splits into a tangential piece (tries to slide the block) and a normal piece (presses it into the surface).
Sanity at $\theta = 0$: $w_T = 0$ (flat ground, no sliding). At $\theta = 90°$: $w_N = 0$ (vertical wall, no normal force). Pythagorean check: $w_T^2 + w_N^2 = |w|^2$. ✓
If you only know the two components: $\tan\theta = |w_T|/|w_N|$ — the weight cancels.
Equilibrium means $\sum \vec F_i = \vec 0$ — every force adds to zero. In 2D this is two scalar equations (x and y components), so two unknowns are solvable.
Add one more axis. $\mathbf k = \langle 0, 0, 1\rangle$ points up; $\mathbf i, \mathbf j, \mathbf k$ are mutually perpendicular unit vectors forming a right-handed system.
Magnitude: Pythagoras applied twice. First in the xy-plane to get the floor diagonal $\sqrt{v_1^2 + v_2^2}$; then with $v_3$ to get the box diagonal.
Examples: $\langle 2, 2, 1\rangle$ has magnitude $\sqrt 9 = 3$. $\langle 3, 4, 12\rangle$ has magnitude $\sqrt{169} = 13$.
Dot product extends naturally: $\vec v \cdot \vec w = v_1 w_1 + v_2 w_2 + v_3 w_3$. Geometric form $|\vec v||\vec w|\cos\theta$ unchanged.
3D-only operation that returns a vector perpendicular to both inputs, with magnitude equal to the parallelogram area.
Expand along the top row with alternating signs. Components:
Magnitude is the parallelogram area: $|\vec v \times \vec w| = |\vec v|\,|\vec w|\sin\theta$. Direction by right-hand rule: fingers curl from $\vec v$ to $\vec w$, thumb points along $\vec v \times \vec w$.
Anti-commutative: $\vec w \times \vec v = -(\vec v \times \vec w)$. Swap → thumb flips.
Triangle area shortcut: a triangle with sides $\vec v, \vec w$ has area $\tfrac{1}{2}|\vec v \times \vec w|$.
Self-check: $(\vec v \times \vec w)\cdot \vec v = 0$ and $(\vec v \times \vec w)\cdot \vec w = 0$ always.
Use the dot product for angles. Always.
The cross product gives $\sin\theta = |\vec v \times \vec w|/(|\vec v|\,|\vec w|)$, but $\arcsin$ only outputs angles in $[-90°, 90°]$. If the real angle is obtuse, $\arcsin$ silently returns its supplementary acute angle — off by 180°.
Worked. $\vec m = \langle 1, 1, 1\rangle,\ \vec w = \langle -2, 3, -6\rangle$.
Two angles, $65.6° + 114.4° = 180°$. $\arcsin$ picked the wrong one. The dot product always wins.
| Dot product | Cross product | |
|---|---|---|
| Output | Scalar | Vector (3D only) |
| Trig form | $|\vec v||\vec w|\cos\theta$ | $|\vec v||\vec w|\sin\theta$ |
| Symmetry | Commutative | Anti-commutative |
| Zero iff | $\vec v \perp \vec w$ | $\vec v \parallel \vec w$ |
| Dimensions | Any | 3D only |
| Use for | Angles, projections | Perpendiculars, areas |
Dot extracts the cosine (parallel component). Cross extracts the sine (perpendicular direction). Together they characterize the entire geometric relationship between two vectors.
Every Cartesian point has infinite polar names — and every polar curve hides a wave that, when read counter-clockwise, traces its silhouette. This is a visual ledger of the shapes you'll need on sight: spin to the angle, walk r units. Negative r walks backward. The pole has no angle. Three pages: foundation, the canonical zoo, and the rectangular bridge.
Spin to angle θ, then walk |r| units — forward if r>0, backward if r<0. Cartesian uses two perpendicular distances; polar uses a direction plus a signed distance.
Comes straight off the right triangle — cos θ = x/r, sin θ = y/r. The signs of cos and sin handle the quadrants automatically.
Calculator's arctan only returns angles in (−π/2, π/2) — Q1 and Q4 only. For Q2 and Q3, add π or compute π − α. The highest-yield Cartesian-to-polar trap, tested every time.
Cartesian is unique. Polar is not. The same Cartesian point √3, 1 is (2, π/6), (2, 13π/6), (−2, 7π/6), (2, −11π/6), … all valid. The two families together generate every alias.
When r = 0, the angle is undefined. Every θ works. This is also why tan θ = y/x blows up at the origin — both top and bottom are zero.
The YouTube video uses a + b cos θ with a = constant, b = coefficient. The worksheets use D + A cos θ with D = constant, A = coefficient. Same family — different letters. Don't memorize letters. Memorize the question.
Circle on the x-axis, diameter |A|, tangent to the y-axis at the pole. Center (A/2, 0), radius |A|/2. Multiply both sides by r, substitute, complete the square.
Sine = cosine rotated 90° CCW. Circle on the y-axis, center (0, A/2), tangent to x-axis at pole. Sign of A flips above/below.
Replacing θ with θ − C rotates the entire circle by C radians CCW about the pole. Same shape, twisted frame. Center moves from (A/2, 0) to polar (A/2, C).
Heart with a cusp at the pole. Minimum r is exactly 0 — the curve touches the pole at exactly one θ (the cusp). Bulge tip sits at distance 2|A|. Cusp angle: where the trig term hits −1.
r stays strictly positive — no pole crossing, no loop. The modulation is strong enough to produce a visible dent on the side opposite the bulge, but not strong enough to flip sign.
When D dominates A by at least a factor of 2, the modulation is too small to dent. The curve looks like an off-center oval — almost a circle, but slightly egg-shaped on the bulge side.
When the trig coefficient exceeds the constant, r goes negative for some θ. Those negative-r portions flip through the pole, drawing a small inner loop on the same side as the bulge.
The video's mnemonic. Meant for each other when A and D are equal (cardioid). Hole in the heart when the trig is too strong, sad and not compatible (inner loop). Moved on when the constant dominates, just a dimple left (dimpled or convex). Memorize all three at once.
Why odd is half: for odd B, the negative-r petals trace the same positions as the positive-r petals — they overlap perfectly, so only B distinct petals appear. For even B, the negative-r petals fall at new angles, so all 2B appear.
Pretty roses: petals are equally spaced around the pole. Find one petal by making the trig argument equal π/2 (so trig = +1, r at max), then step around evenly.
All 2B petals fall on the diagonals, offset from the axes by π/(2B). Cosine roses with even B sit on the axes; sine roses with even B sit between them.
Infinity symbol. Squared r² means r can take either sign (two branches per loop). Mentioned in the YT review video for reference, not deep-tested on the worksheets.
Setting r₁ = r₂ requires the same θ. But polar curves hit the pole at different θ values. Always check the pole separately as Step 2.
Every rectangular sinusoid has a polar twin. If the wave dips below zero, the polar version has an inner loop (negative-r region). If it just touches zero, you get a cardioid. If it stays above zero, dimpled or convex.
The polar inner loop is created exactly by negative-r values — which correspond to the rectangular wave dipping below the x-axis. The shaded region is where r becomes negative.
For rational non-integer B = p/q in lowest terms, the curve does not close at θ = 2π. Extend to 2πq. Calculator-discipline rule: set Tmax = 2πq, or you'll see only a partial petal pattern.
Slide D and A to watch the curve transition cardioid → dimpled → convex → inner-loop. The classification updates live. Try D=0 (pure cosine circle) and D=A (cardioid cusp at pole).
Slide B from 1 to 8. Watch petals halve when B is odd and double when B is even. Toggle cos ↔ sin to see the rotation.
Slide C from 0 to 2π. The whole circle rotates CCW about the pole. The center traces its own circle of radius A/2. Note: phase shift inside the trig is a rotation, not a translation.
The reals weren't enough — once you allow i ² = −1, the number line becomes a plane, multiplication becomes rotation, and the trig identities you memorized turn out to be the same fact written in different ink.
Introduce a symbol i with i² = −1. Extend the reals to ℂ = {a + bi : a, b ∈ ℝ} with the usual ring operations. Multiplication by i is later revealed to be a 90° rotation of the plane.
Powers of i cycle with period 4:
Horizontal axis = real, vertical axis = imaginary. Every complex number is a 2D point — or equivalently, the position vector from the origin to that point. The reals live on the x-axis; i is one unit straight up.
Right triangle with legs a and b in the Argand plane: the hypotenuse is r. Equivalently, |z|² = z · z̄ (a number times its conjugate).
Sweep counterclockwise from the positive real axis to the position vector of z. Defined mod 360°.
Quadrant-fix table (α = arctan(|b|/|a|))
Same point in the plane — described by length r from the origin and angle θ from the positive real axis. The natural language for rotations, because multiplication of cis-form numbers just adds angles.
Cis → Rect: a = r cosθ, b = r sinθ
Rect → Cis: r = √(a²+b²), θ = arctan(b/a) + quadrant fix
Flip the sign of the imaginary part. Geometrically: mirror across the horizontal axis. The magic identity:
The conjugate trick rationalizes complex denominators — multiply top and bottom by the conjugate.
Since i = 0 + 1·i sits at (0, 1) on the unit circle, i = cis(90°). Multiplying by it rotates z by 90° CCW with no change in length. Apply it four times — you're back where you started.
Two arrows from the origin. The product is one arrow: length = r₁·r₂, angle = θ₁ + θ₂. Multiplication in ℂ is rotation + scaling — and the proof is just FOIL plus the trig angle-addition identities.
Notice: the product's radius is the product of radii, the angle is the sum of angles. Try r₂ < 1 — the product shrinks. Try θ₂ = 90° — pure rotation.
Proof technique: multiply numerator and denominator by the conjugate of the denominator. The denominator becomes r₂²(cos²β + sin²β) = r₂² by the Pythagorean identity. The numerator FOILs into the angle-subtraction identities — so cos(α−β) and sin(α−β) drop out.
Each step scales by r and rotates by θ. Angles climb linearly with n; radii scale exponentially with n. Trace gives a log spiral when |z| ≠ 1.
Proof by induction. Base case z1 trivial. Inductive step: zk+1 = zk · z = rkcis(kθ) · r cis(θ) = rk+1cis((k+1)θ). Negative n via division rule.
Same family as nautilus shells, hurricane bands, galaxy arms. W2 P4: z = 2 cis(45°) doubles in length and rotates 45° per step — outward spiral.
For z on the unit circle, zn = 1 when nθ ≡ 0 (mod 360°). The smallest such n is the cycle length — and the powers trace a regular n-gon.
Modular reduction: zk = zk mod n. So z30 = z6 when n = 24.
To solve zn = R cis(α): match moduli (r = R1/n) and match angles mod 360°. The n choices of k give n distinct roots spaced 360°/n apart around a circle.
Try n = 4 (powers of i), n = 6 (hexagon), n = 24 (the W2 P5 24-gon). Each root is a rotation of the previous by 360°/n.
Group structure: the n roots form a cyclic group under multiplication — they're closed (any product is another root) and the n powers of ζ₁ = cis(360°/n) generate them all.
FOIL the left side. Use i² = −1. Group real and imaginary parts:
The angle-addition identities you memorized in trig class — they are literally the real and imaginary parts of cis(α) · cis(β). Two languages for the same equation. The proof of the multiplication rule is just this expansion run backward.
Stated without proof at this level (proofs use complex analysis / topology). Justifies the warm-up claim that xn = 1 has exactly n complex solutions, no more no fewer.
Bonus: roots of unity menagerie
n=1 verify is a 5-second insurance policy on every closed form.
A sequence is an ordered list. A series is the sum of that list. They are not interchangeable.
One index variable, one family, one combiner. Σ adds, Π multiplies, ⋃ unions, ⋂ intersects. Same parsing logic.
| Op | Acts on | Combines via | Empty |
|---|---|---|---|
| Σ | numbers ak | addition | = 0 |
| Π | numbers ak | multiplication | = 1 |
| ⋃ | sets Ak | OR (in ≥1) | = ∅ |
| ⋂ | sets Ak | AND (in all) | = universe |
Explicit form an = f(n) plugs n directly. Recursive form an = g(an-1) needs a seed.
Each term differs from the previous by a fixed common difference d. Plot of (n, an) is a straight line of slope d.
Each term is the previous times common ratio r. Plot is exponential.
A sequence is harmonic iff its reciprocals form an arithmetic sequence. There is no separate formula — just flip.
Given a list, run differences and ratios on the first 4–5 terms. Whichever returns a constant tells you the type.
| Test on first diffs / ratios | Type | Form |
|---|---|---|
| Δ constant | Arithmetic | a + (n−1)d |
| Δ² constant = c | Quadratic | lead = c/2 |
| Δp constant | Polynomial deg p | lead = Δp/p! |
| Ratios constant = r | Geometric | a · rn−1 |
| Reciprocal Δ constant | Harmonic | flip → arith → flip |
| an = an−1+an−2 | Fibonacci-style | recursive |
Example. 3, 8, 15, 24, 35 → Δ = 5, 7, 9, 11 → Δ² = 2 (constant). Quadratic with lead = 1. Match constants: an = n² + 2n.
After deriving any closed form, plug n=1. If you don't get a1, the formula is wrong. This habit catches the most common slip in the unit.
Pair the first and last term, then the second and second-to-last; each pair sums to (a1 + an). There are n/2 pairs.
Gauss-as-a-kid: Σk=1100 k = (100/2)(1 + 100) = 50·101 = 5050.
Sn = n · a.Drag r past ±1 to see partial sums explode or oscillate. The dashed green line is the limit when |r|<1.
Degree rule. Summing a degree-p polynomial in k gives a degree-(p+1) polynomial in n. Each formula has one more factor than the last.
The remarkable identity. Sum of cubes equals square of sum: 1³+2³+3³+…+n³ = (1+2+3+…+n)². Visual proof: each cube k³ unfolds into a square shell of side Tk.
If each term is a difference bk − bk+1, interior terms cancel pairwise. Only the head and tail survive.
Apply x ↦ m·x + b repeatedly. Fixed point: L = b/(1−m). Attracting iff |m| < 1.
On a semicircle of diameter a+b, the radius is the AM, the perpendicular at the split is the GM, the foot of the perpendicular onto the radius is the HM. The picture proves the inequality.
A pure repeating decimal with p-digit block is a geometric series with r = 10−p.
Mixed (prefix + repeat). Scale by 10q and 10q+p, subtract to eliminate the repeating tail. 0.7̄24̄: 1000x − 10x = 717 → x = 717/990.
Why (1+ρ)/(1−ρ). Initial drop counts once. Every rebound height counts twice (up + down). Total = h + 2(hρ + hρ² + …) = h + 2hρ/(1−ρ) = h(1+ρ)/(1−ρ).
Recognition table — final reference card.
| Pattern | Formula | Pattern | Formula |
|---|---|---|---|
| Σ k | n(n+1)/2 | Σ ark−1 finite | a(1−rn)/(1−r) |
| Σ k² | n(n+1)(2n+1)/6 | Σ ark−1 infinite | a/(1−r), |r|<1 |
| Σ k³ | [n(n+1)/2]² | Σ (bk−bk+1) | b1 − lim bn+1 |
| Σ c | n·c | 0.d p-block | block / (p nines) |
| arith series | (n/2)(2a+(n−1)d) | linear xn=mxn−1+b | L=b/(1−m), attract iff |m|<1 |
| bouncing ball | h(1+ρ)/(1−ρ) | crossing wires | ab/(a+b) |