Intuition The big picture
Zoom into the graph of a smooth function near a point and it looks like a straight line . That line is the tangent line . So if you know one exact value f ( a ) f(a) f ( a ) and the slope f ′ ( a ) f'(a) f ′ ( a ) , you can estimate nearby values without recomputing the messy function. Linear approximation is just "ride the tangent line a little way."
Definition Linear approximation (linearization)
The linearization of f f f at x = a x=a x = a is the function whose graph is the tangent line at a a a :
L ( x ) = f ( a ) + f ′ ( a ) ( x − a ) L(x) = f(a) + f'(a)\,(x-a) L ( x ) = f ( a ) + f ′ ( a ) ( x − a )
For x x x near a a a we write f ( x ) ≈ L ( x ) f(x) \approx L(x) f ( x ) ≈ L ( x ) . The symbol L L L is literally a L ine.
Let y = f ( x ) y=f(x) y = f ( x ) . The differential d x dx d x is an independent variable (a chosen small change in x x x ). The differential of y y y is
d y = f ′ ( x ) d x dy = f'(x)\,dx d y = f ′ ( x ) d x
Here d y dy d y is the rise along the tangent line when x x x moves by d x dx d x . The true change in y y y is Δ y = f ( x + d x ) − f ( x ) \Delta y = f(x+dx)-f(x) Δ y = f ( x + d x ) − f ( x ) , and the whole idea is Δ y ≈ d y \Delta y \approx dy Δ y ≈ d y .
The derivative is defined as a limit:
f ′ ( a ) = lim x → a f ( x ) − f ( a ) x − a . f'(a) = \lim_{x\to a}\frac{f(x)-f(a)}{x-a}. f ′ ( a ) = lim x → a x − a f ( x ) − f ( a ) .
"Limit equals f ′ ( a ) f'(a) f ′ ( a ) " means: for x x x close to a a a , the difference quotient is close to f ′ ( a ) f'(a) f ′ ( a ) . Write that closeness as an error term ε ( x ) \varepsilon(x) ε ( x ) that → 0 \to 0 → 0 as x → a x\to a x → a :
f ( x ) − f ( a ) x − a = f ′ ( a ) + ε ( x ) . \frac{f(x)-f(a)}{x-a} = f'(a) + \varepsilon(x). x − a f ( x ) − f ( a ) = f ′ ( a ) + ε ( x ) .
Multiply both sides by ( x − a ) (x-a) ( x − a ) :
f ( x ) − f ( a ) = f ′ ( a ) ( x − a ) + ε ( x ) ( x − a ) . f(x)-f(a) = f'(a)(x-a) + \varepsilon(x)(x-a). f ( x ) − f ( a ) = f ′ ( a ) ( x − a ) + ε ( x ) ( x − a ) .
So
f ( x ) = f ( a ) + f ′ ( a ) ( x − a ) ⏟ L ( x ) + ε ( x ) ( x − a ) ⏟ error . f(x) = \underbrace{f(a)+f'(a)(x-a)}_{L(x)} + \underbrace{\varepsilon(x)(x-a)}_{\text{error}}. f ( x ) = L ( x ) f ( a ) + f ′ ( a ) ( x − a ) + error ε ( x ) ( x − a ) .
Why this is great: the error is ε ( x ) ⋅ ( x − a ) \varepsilon(x)\cdot(x-a) ε ( x ) ⋅ ( x − a ) — a small number times a small number . It shrinks faster than ( x − a ) (x-a) ( x − a ) itself. That's why near a a a the line L ( x ) L(x) L ( x ) is an excellent stand-in for f f f .
Pick a base point a a a near your target where f ( a ) f(a) f ( a ) and f ′ ( a ) f'(a) f ′ ( a ) are easy/exact .
Compute f ( a ) f(a) f ( a ) and f ′ ( a ) f'(a) f ′ ( a ) .
Plug into L ( x ) = f ( a ) + f ′ ( a ) ( x − a ) L(x)=f(a)+f'(a)(x-a) L ( x ) = f ( a ) + f ′ ( a ) ( x − a ) .
Evaluate at your target x x x . (For differentials: d x = x − a dx = x-a d x = x − a , then f ( x ) ≈ f ( a ) + d y f(x)\approx f(a)+dy f ( x ) ≈ f ( a ) + d y .)
4.1 \sqrt{4.1} 4.1
Step 1 — choose f f f and a a a . Let f ( x ) = x f(x)=\sqrt{x} f ( x ) = x , a = 4 a=4 a = 4 . Why? 4 = 2 \sqrt 4=2 4 = 2 is exact and 4.1 4.1 4.1 is close to 4 4 4 .
Step 2 — slope. f ′ ( x ) = 1 2 x f'(x)=\tfrac{1}{2\sqrt x} f ′ ( x ) = 2 x 1 , so f ′ ( 4 ) = 1 4 f'(4)=\tfrac1{4} f ′ ( 4 ) = 4 1 . Why? The tangent slope controls the line.
Step 3 — line. L ( x ) = 2 + 1 4 ( x − 4 ) L(x)=2+\tfrac14(x-4) L ( x ) = 2 + 4 1 ( x − 4 ) .
Step 4 — evaluate. L ( 4.1 ) = 2 + 1 4 ( 0.1 ) = 2.025 L(4.1)=2+\tfrac14(0.1)=2.025 L ( 4.1 ) = 2 + 4 1 ( 0.1 ) = 2.025 .
True value 4.1 = 2.02485 … \sqrt{4.1}=2.02485\ldots 4.1 = 2.02485 … — error about 0.0001 0.0001 0.0001 .
( 1.02 ) 10 (1.02)^{10} ( 1.02 ) 10 via differentials
f ( x ) = x 10 f(x)=x^{10} f ( x ) = x 10 , base a = 1 a=1 a = 1 , d x = 0.02 dx=0.02 d x = 0.02 . Why a = 1 a=1 a = 1 ? 1 10 = 1 1^{10}=1 1 10 = 1 exactly.
f ′ ( x ) = 10 x 9 f'(x)=10x^9 f ′ ( x ) = 10 x 9 , f ′ ( 1 ) = 10 f'(1)=10 f ′ ( 1 ) = 10 .
d y = f ′ ( 1 ) d x = 10 ( 0.02 ) = 0.2 dy=f'(1)\,dx = 10(0.02)=0.2 d y = f ′ ( 1 ) d x = 10 ( 0.02 ) = 0.2 .
( 1.02 ) 10 ≈ f ( 1 ) + d y = 1 + 0.2 = 1.2 (1.02)^{10}\approx f(1)+dy = 1+0.2 = 1.2 ( 1.02 ) 10 ≈ f ( 1 ) + d y = 1 + 0.2 = 1.2 . (True ≈ 1.219 \approx 1.219 ≈ 1.219 .) Why close? d x dx d x is tiny.
≈ 1 + n x \approx 1+nx ≈ 1 + n x " trick
f ( x ) = ( 1 + x ) n f(x)=(1+x)^n f ( x ) = ( 1 + x ) n at a = 0 a=0 a = 0 : f ( 0 ) = 1 f(0)=1 f ( 0 ) = 1 , f ′ ( 0 ) = n ( 1 + 0 ) n − 1 = n f'(0)=n(1+0)^{n-1}=n f ′ ( 0 ) = n ( 1 + 0 ) n − 1 = n .
( 1 + x ) n ≈ 1 + n x ( x small ) . (1+x)^n \approx 1+nx \quad (x\text{ small}). ( 1 + x ) n ≈ 1 + n x ( x small ) .
Why this step? Setting a = 0 a=0 a = 0 collapses ( x − a ) (x-a) ( x − a ) to x x x , giving a memorizable formula. Likewise sin x ≈ x \sin x\approx x sin x ≈ x , e x ≈ 1 + x e^x\approx 1+x e x ≈ 1 + x , ln ( 1 + x ) ≈ x \ln(1+x)\approx x ln ( 1 + x ) ≈ x near 0 0 0 .
Worked example Error propagation (the practical payoff)
A sphere's radius is measured as r = 10 r=10 r = 10 cm with possible error d r = 0.05 dr=0.05 d r = 0.05 cm. Estimate the error in volume V = 4 3 π r 3 V=\tfrac43\pi r^3 V = 3 4 π r 3 .
d V = 4 π r 2 d r = 4 π ( 100 ) ( 0.05 ) = 20 π ≈ 62.8 cm 3 dV = 4\pi r^2\,dr = 4\pi(100)(0.05)=20\pi\approx 62.8\ \text{cm}^3 d V = 4 π r 2 d r = 4 π ( 100 ) ( 0.05 ) = 20 π ≈ 62.8 cm 3 .
Why differentials here? We don't know the true error, only that d r dr d r is small, so Δ V ≈ d V \Delta V\approx dV Δ V ≈ d V converts radius uncertainty into volume uncertainty. Relative error: d V V = 3 d r r = 3 ( 0.005 ) = 1.5 % \tfrac{dV}{V}=3\,\tfrac{dr}{r}=3(0.005)=1.5\% V d V = 3 r d r = 3 ( 0.005 ) = 1.5% .
Common mistake "Just use the original
f f f , why bother with the line?"
Why it feels right: you can plug into f f f — but by hand 4.1 \sqrt{4.1} 4.1 or ( 1.02 ) 10 (1.02)^{10} ( 1.02 ) 10 is painful, while the line is one multiply-and-add. The point is cheap, accurate-enough estimates and error analysis , where the form d y = f ′ ( x ) d x dy=f'(x)dx d y = f ′ ( x ) d x is what matters.
Common mistake Choosing a bad base point
a a a
Feels right: "any a a a works." Mathematically yes, but the error grows like ( x − a ) 2 (x-a)^2 ( x − a ) 2 -ish. Fix: pick the nearest a a a where f ( a ) , f ′ ( a ) f(a),f'(a) f ( a ) , f ′ ( a ) are exact. For 4.1 \sqrt{4.1} 4.1 use a = 4 a=4 a = 4 , never a = 0 a=0 a = 0 .
Δ y \Delta y Δ y with d y dy d y
Feels right: both are "the change in y y y ." But Δ y \Delta y Δ y is the true curve change; d y dy d y is the tangent line change. They're only approximately equal, and the gap is exactly the curvature error. Don't claim Δ y = d y \Delta y = dy Δ y = d y .
Common mistake Dropping the
( x − a ) (x-a) ( x − a ) factor
Writing f ( x ) ≈ f ( a ) + f ′ ( a ) f(x)\approx f(a)+f'(a) f ( x ) ≈ f ( a ) + f ′ ( a ) — units don't even match. Fix: slope must be multiplied by the run ( x − a ) (x-a) ( x − a ) to get a rise.
Recall Feynman: explain to a 12-year-old
Imagine a curvy road. Right where you're standing, walk in the exact direction the road points (its slope). For a few steps you stay almost on the road, even though it slowly curves away. So instead of doing hard curvy math, you "walk straight a little." f ( a ) f(a) f ( a ) is where you start, f ′ ( a ) f'(a) f ′ ( a ) is which way you're pointing, and ( x − a ) (x-a) ( x − a ) is how many steps you take. The further you walk, the more the real road curves away from your straight path — that's the error.
Mnemonic Remember the formula
"Start + Slope × Step" → f ( a ) + f ′ ( a ) ( x − a ) f(a) + f'(a)\,(x-a) f ( a ) + f ′ ( a ) ( x − a ) .
And d y = f ′ ( x ) d x dy=f'(x)\,dx d y = f ′ ( x ) d x reads "rise = slope × run." Differential d d d = "d ash along the tangent."
What is the linearization of f f f at a a a ? L ( x ) = f ( a ) + f ′ ( a ) ( x − a ) L(x)=f(a)+f'(a)(x-a) L ( x ) = f ( a ) + f ′ ( a ) ( x − a ) Why does linear approximation work (one line)? The limit definition forces
f ( x ) = L ( x ) + ε ( x ) ( x − a ) f(x)=L(x)+\varepsilon(x)(x-a) f ( x ) = L ( x ) + ε ( x ) ( x − a ) with error shrinking faster than
( x − a ) (x-a) ( x − a ) .
Define the differential d y dy d y . d y = f ′ ( x ) d x dy=f'(x)\,dx d y = f ′ ( x ) d x , the rise along the tangent line for an input change
d x dx d x .
Difference between Δ y \Delta y Δ y and d y dy d y ? Δ y \Delta y Δ y = true change of the curve;
d y dy d y = change along the tangent line;
Δ y ≈ d y \Delta y\approx dy Δ y ≈ d y .
Approximate ( 1 + x ) n (1+x)^n ( 1 + x ) n for small x x x . 1 + n x 1+nx 1 + n x (linearize at
a = 0 a=0 a = 0 ).
How do you pick the base point a a a ? Nearest value to the target where
f ( a ) f(a) f ( a ) and
f ′ ( a ) f'(a) f ′ ( a ) are exact/easy.
Estimate 4.1 \sqrt{4.1} 4.1 using a = 4 a=4 a = 4 . 2 + 1 4 ( 0.1 ) = 2.025 2+\tfrac14(0.1)=2.025 2 + 4 1 ( 0.1 ) = 2.025 .
Relative error in volume of a sphere from radius error? d V V = 3 d r r \tfrac{dV}{V}=3\,\tfrac{dr}{r} V d V = 3 r d r .
sin x \sin x sin x , e x e^x e x , ln ( 1 + x ) \ln(1+x) ln ( 1 + x ) near 0 0 0 ?sin x ≈ x \sin x\approx x sin x ≈ x ,
e x ≈ 1 + x e^x\approx 1+x e x ≈ 1 + x ,
ln ( 1 + x ) ≈ x \ln(1+x)\approx x ln ( 1 + x ) ≈ x .
Derivative as a limit — the definition that is the proof here.
Tangent line — the geometric object L ( x ) L(x) L ( x ) is.
Taylor series — linear approximation is the degree-1 Taylor polynomial; next terms cut the error.
Newton's method — repeatedly linearizing to solve f ( x ) = 0 f(x)=0 f ( x ) = 0 .
Error propagation — physics/lab use of d y = f ′ ( x ) d x dy=f'(x)\,dx d y = f ′ ( x ) d x .
Concavity and second derivative — controls whether L L L over- or under-estimates.
Difference quotient plus error e(x)
Linearization L(x)=f(a)+f'(a)(x-a)
Intuition Hinglish mein samjho
Dekho, idea bahut simple hai. Koi bhi smooth curve agar tum kisi point ke bilkul paas zoom karo, toh woh ek straight line jaisi dikhne lagti hai — woh line hai tangent line . Toh agar tumhe ek point pe exact value f ( a ) f(a) f ( a ) pata hai aur waha ki slope f ′ ( a ) f'(a) f ′ ( a ) pata hai, toh aas-paas ki value ko bina poora hard calculation kiye tum estimate kar sakte ho. Formula: f ( x ) ≈ f ( a ) + f ′ ( a ) ( x − a ) f(x)\approx f(a)+f'(a)(x-a) f ( x ) ≈ f ( a ) + f ′ ( a ) ( x − a ) — yaani "Start + Slope × Step".
Yeh kaam kyun karta hai? Kyunki derivative ki definition hi limit se aati hai: paas mein difference quotient f ′ ( a ) f'(a) f ′ ( a ) ke kareeb hota hai. Usse rearrange karo toh error ka term ε ( x ) ( x − a ) \varepsilon(x)(x-a) ε ( x ) ( x − a ) banta hai — yeh "chhota times chhota" hai, isliye ( x − a ) (x-a) ( x − a ) se bhi tezi se zero ki taraf jaata hai. Isiliye line, curve ka itna accha replacement banti hai near a a a .
Differentials bas isi ka chhota bhai hai: d y = f ′ ( x ) d x dy=f'(x)\,dx d y = f ′ ( x ) d x . Yahan d x dx d x tumhara choti si change hai input mein, aur d y dy d y tangent line ke uppar ka rise. Real change Δ y \Delta y Δ y thoda alag hota hai (curve curve karti hai), par Δ y ≈ d y \Delta y\approx dy Δ y ≈ d y . Sabse useful jagah: error propagation . Jaise sphere ka radius 10 10 10 cm measure kiya 0.05 0.05 0.05 cm error ke saath — toh volume mein error d V = 4 π r 2 d r dV=4\pi r^2\,dr d V = 4 π r 2 d r se nikal lo. Relative error ka shortcut: d V / V = 3 d r / r dV/V = 3\,dr/r d V / V = 3 d r / r .
Exam tip: base point a a a hamesha target ke sabse paas waala easy value choose karo (jaise 4.1 \sqrt{4.1} 4.1 ke liye a = 4 a=4 a = 4 ). Aur ( 1 + x ) n ≈ 1 + n x (1+x)^n\approx 1+nx ( 1 + x ) n ≈ 1 + n x , sin x ≈ x \sin x\approx x sin x ≈ x , e x ≈ 1 + x e^x\approx 1+x e x ≈ 1 + x yeh chhote-x x x approximations ratt lo — yeh 80/20 ka asli maal hai.