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Chapter 2 — Construction of the Itô Integral

Guiding question

Brownian motion is nowhere differentiable. Its total variation is almost surely infinite. Classical Riemann–Stieltjes integration requires the integrator to have bounded variation. How, then, can we define ∫0THt dWt\int_0^T H_t\,dW_t in a way that is mathematically precise and financially meaningful?

The Itô integral is the central technical object of stochastic calculus. Chapter 1 built Brownian motion and established its quadratic variation property [W]T=T[W]_T = T. This chapter uses that property as a foundation. The strategy is:

  1. Observe that pathwise Riemann–Stieltjes integration fails.
  2. Define the integral for a small, explicitly computable class (simple processes).
  3. Prove an isometry that makes the integral a bounded linear map in L2L^2.
  4. Extend to the full L2L^2 class by density and closure.

The construction mirrors the standard L2L^2 completion in functional analysis, and the isometry is its counterpart of Parseval's theorem.


2.1 Why pathwise integration fails​

Let f:[0,T]→Rf:[0,T]\to\mathbb R be a continuous function and g:[0,T]→Rg:[0,T]\to\mathbb R be the integrator. The Riemann–Stieltjes integral ∫0Tf dg\int_0^T f\,dg exists whenever ff is continuous and gg has bounded variation:

∥g∥TV=sup⁡Π∑k∣g(tk+1)−g(tk)∣<∞.\|g\|_{\mathrm{TV}} = \sup_\Pi \sum_{k}|g(t_{k+1})-g(t_k)| < \infty.

For Brownian motion, the opposite holds.

Brownian motion has infinite total variation

Almost surely,

∑k=0n−1∣Wtk+1−Wtk∣→∞\sum_{k=0}^{n-1}|W_{t_{k+1}}-W_{t_k}|\to\infty

as the mesh ∣Π∣→0|\Pi|\to 0.

Proof

On a uniform partition with tk=kT/nt_k = kT/n, the increments are i.i.d.\ N(0,T/n)N(0,T/n). Therefore

E[∑k=0n−1∣Wtk+1−Wtk∣]=n⋅E[∣N(0,T/n)∣]=n⋅2Tπn=2nTπ→∞.\mathbb E\left[\sum_{k=0}^{n-1}|W_{t_{k+1}}-W_{t_k}|\right] = n\cdot \mathbb E\left[|N(0,T/n)|\right] = n\cdot \sqrt{\frac{2T}{\pi n}} = \sqrt{\frac{2nT}{\pi}} \to\infty.

By the law of large numbers applied to the i.i.d.\ terms ∣Wtk+1−Wtk∣|W_{t_{k+1}}-W_{t_k}|, the sum converges almost surely to ∞\infty.

So Brownian paths are nowhere near having bounded variation. No classical integral theory applies directly.

Why infinite variation but finite quadratic variation?

Total variation sums ∣ΔW∣|\Delta W|. Quadratic variation sums (ΔW)2(\Delta W)^2. Because ΔW∼Δt\Delta W \sim \sqrt{\Delta t}, we have

∣ΔW∣∼Δt,(ΔW)2∼Δt.|\Delta W| \sim \sqrt{\Delta t}, \quad (\Delta W)^2 \sim \Delta t.

Summing over n=T/Δtn = T/\Delta t terms:

∑∣ΔW∣∼nΔt=T/Δt→∞,∑(ΔW)2∼n⋅Δt=T.\sum |\Delta W| \sim n\sqrt{\Delta t} = \sqrt{T/\Delta t}\to\infty, \quad \sum (\Delta W)^2 \sim n\cdot\Delta t = T.

Quadratic variation lives in the right scaling window to remain finite. This is why (dW)2=dt(dW)^2 = dt is the key equation, and why the natural Hilbert space for stochastic integration is built on the L2L^2 norm.


2.2 The class of simple adapted processes​

A process H=(Ht)0≤t≤TH = (H_t)_{0\le t\le T} is called simple (or elementary) if there exists a partition 0=t0<t1<⋯<tn=T0 = t_0 < t_1 < \cdots < t_n = T and Ftk\mathcal F_{t_k}-measurable random variables HkH_k satisfying E[Hk2]<∞\mathbb E[H_k^2]<\infty, such that

Ht=∑k=0n−1Hk 1(tk,tk+1](t).H_t = \sum_{k=0}^{n-1} H_k\,\mathbf{1}_{(t_k,t_{k+1}]}(t).

The requirement that HkH_k is Ftk\mathcal F_{t_k}-measurable is the adaptedness condition: the value of the integrand at time tkt_k may only use information up to tkt_k.

Adaptedness is not optional

If HkH_k were allowed to depend on Wtk+1W_{t_{k+1}} — the future increment — the resulting integral would not be a martingale, and the isometry below would fail. In finance, this corresponds to using future prices to choose a present position: pure look-ahead bias.

For a simple process, we define the Itô integral as the finite sum

I(H)=∫0THt dWt:=∑k=0n−1Hk(Wtk+1−Wtk).I(H) = \int_0^T H_t\,dW_t := \sum_{k=0}^{n-1} H_k\bigl(W_{t_{k+1}}-W_{t_k}\bigr).

Each term is a product of a Ftk\mathcal F_{t_k}-measurable random variable with an independent increment. This is a finite sum of square-integrable random variables, so I(H)∈L2(Ω)I(H)\in L^2(\Omega).


2.3 The Itô isometry for simple processes​

Itô isometry

For any simple adapted process HH,

E ⁣[ ⁣(∫0THt dWt) ⁣2]=E ⁣[∫0THt2 dt].\mathbb E\!\left[\!\left(\int_0^T H_t\,dW_t\right)^{\!2}\right] = \mathbb E\!\left[\int_0^T H_t^2\,dt\right].
Proof

Write ΔWk=Wtk+1−Wtk\Delta W_k = W_{t_{k+1}}-W_{t_k} and Δtk=tk+1−tk\Delta t_k = t_{k+1}-t_k. Then

(∑k=0n−1Hk ΔWk) ⁣2=∑k=0n−1Hk2 (ΔWk)2+2∑j<kHj ΔWj Hk ΔWk.\left(\sum_{k=0}^{n-1} H_k\,\Delta W_k\right)^{\!2} = \sum_{k=0}^{n-1} H_k^2\,(\Delta W_k)^2 + 2\sum_{j<k} H_j\,\Delta W_j\,H_k\,\Delta W_k.

Cross terms. For j<kj < k, the product Hj ΔWj HkH_j\,\Delta W_j\,H_k is Ftk\mathcal F_{t_k}-measurable, and ΔWk\Delta W_k is independent of Ftk\mathcal F_{t_k} with mean zero. Therefore

E[Hj ΔWj Hk ΔWk]=E[Hj ΔWj Hk]⋅E[ΔWk]=0.\mathbb E[H_j\,\Delta W_j\,H_k\,\Delta W_k] = \mathbb E[H_j\,\Delta W_j\,H_k]\cdot\mathbb E[\Delta W_k] = 0.

Diagonal terms. For each kk, HkH_k is Ftk\mathcal F_{t_k}-measurable and independent of ΔWk\Delta W_k. Therefore

E[Hk2 (ΔWk)2]=E[Hk2]⋅E[(ΔWk)2]=E[Hk2]⋅Δtk.\mathbb E[H_k^2\,(\Delta W_k)^2] = \mathbb E[H_k^2]\cdot\mathbb E[(\Delta W_k)^2] = \mathbb E[H_k^2]\cdot\Delta t_k.

Summing,

E ⁣[(∫0THt dWt) ⁣2]=∑k=0n−1E[Hk2] Δtk=E ⁣[∫0THt2 dt].\mathbb E\!\left[\left(\int_0^T H_t\,dW_t\right)^{\!2}\right] = \sum_{k=0}^{n-1}\mathbb E[H_k^2]\,\Delta t_k = \mathbb E\!\left[\int_0^T H_t^2\,dt\right].

The cross terms vanish because of adaptedness. This is the structural insight: the left endpoint rule is exactly what kills the cross terms.

Isometry: the integral is an isometric embedding

The map H↦I(H)H\mapsto I(H) sends the Hilbert space

L2([0,T]×Ω,dt⊗P)L^2([0,T]\times\Omega, dt\otimes\mathbb P)

isometrically into L2(Ω,P)L^2(\Omega,\mathbb P). Distances are preserved:

∥I(H)∥L2(Ω)=∥H∥L2([0,T]×Ω).\|I(H)\|_{L^2(\Omega)} = \|H\|_{L^2([0,T]\times\Omega)}.

This is the stochastic counterpart of the identity ∥f^∥2=∥f∥2\|\hat f\|_2 = \|f\|_2 in Fourier analysis: an integral transform that preserves L2L^2 norms.


2.4 Zero mean​

Itô integral is centered

For any simple adapted HH,

E ⁣[∫0THt dWt]=0.\mathbb E\!\left[\int_0^T H_t\,dW_t\right] = 0.
Proof

Each term: E[Hk ΔWk]=E[Hk]⋅E[ΔWk]=0\mathbb E[H_k\,\Delta W_k] = \mathbb E[H_k]\cdot\mathbb E[\Delta W_k] = 0, since HkH_k is independent of ΔWk\Delta W_k and E[ΔWk]=0\mathbb E[\Delta W_k]=0.


2.5 Extension to L2L^2 adapted processes​

Let L2=Lad2([0,T]×Ω)\mathcal L^2 = L^2_{\mathrm{ad}}([0,T]\times\Omega) denote the space of adapted processes HH with

∥H∥2=E ⁣[∫0THt2 dt]<∞.\|H\|^2 = \mathbb E\!\left[\int_0^T H_t^2\,dt\right] < \infty.
Density of simple processes

The simple adapted processes are dense in L2\mathcal L^2: for any H∈L2H\in\mathcal L^2, there exists a sequence of simple processes H(n)H^{(n)} with

∥H(n)−H∥L2→0.\|H^{(n)}-H\|_{\mathcal L^2}\to 0.

Given this density, define the Itô integral for general H∈L2H\in\mathcal L^2 as the L2(Ω)L^2(\Omega)-limit:

∫0THt dWt=lim⁡n→∞∫0THt(n) dWt,\int_0^T H_t\,dW_t = \lim_{n\to\infty}\int_0^T H_t^{(n)}\,dW_t,

where the limit is in L2(Ω)L^2(\Omega).

Well-definedness

The sequence I(H(n))I(H^{(n)}) is Cauchy in L2(Ω)L^2(\Omega) because, by the isometry,

∥I(H(m))−I(H(n))∥L2(Ω)=∥I(H(m)−H(n))∥L2(Ω)=∥H(m)−H(n)∥L2→0.\|I(H^{(m)})-I(H^{(n)})\|_{L^2(\Omega)} = \|I(H^{(m)}-H^{(n)})\|_{L^2(\Omega)} = \|H^{(m)}-H^{(n)}\|_{\mathcal L^2}\to 0.

Since L2(Ω)L^2(\Omega) is complete, the limit exists and is independent of the approximating sequence.

Itô integral as a left-endpoint Riemann sum over Brownian motion
010
Itô sum (left endpoint)0.8162
Stratonovich sum (midpoint)1.2593
Itô formula: ½(W₁² − 1)0.7593
Blue rectangles use H(t_k) — left endpoint, Itô convention. The Itô sum converges to ½(W₁² − 1), not ½W₁², because (dW)² = dt contributes an extra −½ correction — the Itô correction term. The Stratonovich midpoint sum converges to ½W₁².

2.6 The Itô integral as a martingale​

Define the running integral

Mt=∫0tHs dWs,0≤t≤T.M_t = \int_0^t H_s\,dW_s, \qquad 0\le t\le T.
Martingale property

The process (Mt)0≤t≤T(M_t)_{0\le t\le T} is a martingale with respect to the filtration (Ft)(\mathcal F_t).

Proof sketch for simple processes

For s<ts < t and a simple process adapted to a partition that includes ss,

Mt−Ms=∑tk∈[s,t)Hk ΔWk.M_t - M_s = \sum_{t_k\in[s,t)} H_k\,\Delta W_k.

Each term Hk ΔWkH_k\,\Delta W_k has mean zero conditionally on Fs\mathcal F_s (since HkH_k is Ftk⊇Fs\mathcal F_{t_k}\supseteq\mathcal F_s-measurable and ΔWk\Delta W_k is independent of Ftk\mathcal F_{t_k} with mean zero). Therefore

E[Mt−Ms∣Fs]=0,soE[Mt∣Fs]=Ms.\mathbb E[M_t - M_s\mid\mathcal F_s] = 0, \qquad\text{so}\quad \mathbb E[M_t\mid\mathcal F_s] = M_s.
Trading P&L is a martingale under no-arbitrage

If HtH_t is the number of shares of a zero-drift asset held at time tt, and the asset price satisfies dSt=σt dWtdS_t = \sigma_t\,dW_t (a pure diffusion under the risk-neutral measure), then the portfolio value

Pt=P0+∫0tHs dSs=P0+∫0tHsσs dWsP_t = P_0 + \int_0^t H_s\,dS_s = P_0 + \int_0^t H_s\sigma_s\,dW_s

is a martingale. The expected P&L is zero: there is no predictable profit without risk. This is the mathematical content of no-arbitrage in diffusion models.


2.7 Quadratic variation of the Itô integral​

Quadratic variation

Let Mt=∫0tHs dWsM_t = \int_0^t H_s\,dW_s. Then the quadratic variation of MM is

[M]t=∫0tHs2 ds.[M]_t = \int_0^t H_s^2\,ds.
Proof sketch

On a uniform partition with mesh Δt\Delta t,

∑k(Mtk+1−Mtk)2≈∑kHtk2 (ΔWk)2≈∑kHtk2 Δt→∫0tHs2 ds.\sum_{k}(M_{t_{k+1}}-M_{t_k})^2 \approx \sum_k H_{t_k}^2\,(\Delta W_k)^2 \approx \sum_k H_{t_k}^2\,\Delta t \to\int_0^t H_s^2\,ds.

The approximation uses (dW)2=dt(dW)^2 = dt in the same sense as the quadratic variation of Brownian motion.

Volatility as accumulated integrand squared

The quadratic variation [M]t=∫0tHs2 ds[M]_t = \int_0^t H_s^2\,ds is the accumulated squared magnitude of the integrand. In finance, if HtH_t is the dollar amount in the risky asset and dS/S=σ dWdS/S = \sigma\,dW, then the portfolio quadratic variation is ∫0tHs2σs2 ds\int_0^t H_s^2\sigma_s^2\,ds — the accumulated squared dollar-volatility exposure.


2.8 Itô versus Stratonovich​

The Itô integral uses the left endpoint Hk=HtkH_k = H_{t_k}. An alternative is the Stratonovich integral, which uses the midpoint 12(Htk+Htk+1)\frac12(H_{t_k}+H_{t_{k+1}}):

∫0THt∘ dWt:=lim⁡∣Π∣→0∑kHtk+Htk+12(Wtk+1−Wtk).\int_0^T H_t\circ\,dW_t := \lim_{|\Pi|\to 0}\sum_k \frac{H_{t_k}+H_{t_{k+1}}}{2}(W_{t_{k+1}}-W_{t_k}).

The two integrals are related by the correction formula

∫0THt∘ dWt=∫0THt dWt+12[H,W]T,\int_0^T H_t\circ\,dW_t = \int_0^T H_t\,dW_t + \tfrac12[H,W]_T,

where [H,W]T=∫0TdHs dWs[H,W]_T = \int_0^T dH_s\,dW_s is the cross-variation.

For a smooth function ff applied to Brownian motion, Ht=f(Wt)H_t = f(W_t), one computes

[f(W),W]T=∫0Tf′(Ws) ds,[f(W),W]_T = \int_0^T f'(W_s)\,ds,

so the Stratonovich integral satisfies the classical chain rule: ∫f′(Wt)∘dWt=f(WT)−f(W0)\int f'(W_t)\circ dW_t = f(W_T)-f(W_0). The Itô integral instead satisfies the modified Itô formula in Chapter 3.

Which integral to use?

Itô: natural in finance (adapted integrands, no future look-ahead, martingale property), but its calculus has second-order correction terms.

Stratonovich: natural in physics/geometry (satisfies classical chain rule, coordinate-invariant under manifold transformations), but uses anticipating information.

In this course the default is Itô.


2.9 The stochastic integral as a process​

For fixed TT, the map H↦∫0THt dWtH\mapsto \int_0^T H_t\,dW_t is a random variable. But we can also view the integral as a process in the upper limit:

Mt=∫0tHs dWs,0≤t≤T.M_t = \int_0^t H_s\,dW_s,\qquad 0\le t\le T.

A version of MM with continuous sample paths exists whenever H∈L2H\in\mathcal L^2.

Continuity and the Burkholder–Davis–Gundy inequality

For H∈L2H\in\mathcal L^2, the martingale Mt=∫0tHs dWsM_t = \int_0^t H_s\,dW_s has a continuous version. Moreover, for any p≥1p\ge 1, there exist universal constants cp,Cpc_p, C_p such that

cp E ⁣[(∫0THs2 ds)p/2]≤E ⁣[sup⁡0≤t≤T∣Mt∣p]≤Cp E ⁣[(∫0THs2 ds)p/2].c_p\,\mathbb E\!\left[\left(\int_0^T H_s^2\,ds\right)^{p/2}\right] \le \mathbb E\!\left[\sup_{0\le t\le T}|M_t|^p\right] \le C_p\,\mathbb E\!\left[\left(\int_0^T H_s^2\,ds\right)^{p/2}\right].

This inequality controls the supremum of the process in terms of the quadratic variation — a powerful tool in SDE existence theory.


2.10 A worked example​

Compute ∫0TWt dWt\int_0^T W_t\,dW_t.

Here Ht=WtH_t = W_t. This is adapted. On a partition {tk}\{t_k\}, the Itô sum is

In=∑k=0n−1Wtk (Wtk+1−Wtk).I_n = \sum_{k=0}^{n-1} W_{t_k}\,(W_{t_{k+1}}-W_{t_k}).

Use the algebraic identity ab=12[(a+b)2−a2−b2]ab = \frac12[(a+b)^2 - a^2 - b^2]:

Wtk(Wtk+1−Wtk)=12Wtk+12−12Wtk2−12(Wtk+1−Wtk)2.W_{t_k}(W_{t_{k+1}}-W_{t_k}) = \tfrac12 W_{t_{k+1}}^2 - \tfrac12 W_{t_k}^2 - \tfrac12(W_{t_{k+1}}-W_{t_k})^2.

Summing (telescoping):

In=12WT2−12W02−12∑k(ΔWk)2.I_n = \tfrac12 W_T^2 - \tfrac12 W_0^2 - \tfrac12\sum_k(\Delta W_k)^2.

Since W0=0W_0 = 0 and ∑k(ΔWk)2→T\sum_k(\Delta W_k)^2\to T,

∫0TWt dWt=12WT2−12T.\int_0^T W_t\,dW_t = \tfrac12 W_T^2 - \tfrac12 T.

The correction −T2-\frac T2 is the signature of Itô calculus. Classical calculus would give ∫0Tx dx=12x2∣0T=12T\int_0^T x\,dx = \frac12 x^2\big|_0^T = \frac12 T for x=Tx = T, but that is the wrong analogy. The Itô integral of WtW_t against dWtdW_t is not 12T\frac12 T; it is the random variable 12WT2−12T\frac12 W_T^2 - \frac12 T.


2.11 Problems​

Problem 1: Itô isometry for a deterministic integrand

Let Ht=h(t)H_t = h(t) be a deterministic square-integrable function. Compute Var ⁣(∫0Th(t) dWt)\text{Var}\!\left(\int_0^T h(t)\,dW_t\right) using the isometry.

Problem 2: Integral of a constant

Let Ht=cH_t = c (constant). Verify from the definition that ∫0Tc dWt=c WT\int_0^T c\,dW_t = c\,W_T, and check the Itô isometry.

Problem 3: Cross-variation

Let Mt=∫0tHs dWsM_t = \int_0^t H_s\,dW_s and Nt=∫0tKs dWsN_t = \int_0^t K_s\,dW_s for H,K∈L2H,K\in\mathcal L^2. Show that

[M,N]T=∫0THsKs ds.[M,N]_T = \int_0^T H_s K_s\,ds.
Problem 4: The Stratonovich correction

If Ht=WtH_t = W_t, show that the Stratonovich integral satisfies

∫0TWt∘ dWt=12WT2.\int_0^T W_t\circ\,dW_t = \tfrac12 W_T^2.

Reconcile this with ∫0TWt dWt=12WT2−12T\int_0^T W_t\,dW_t = \tfrac12 W_T^2 - \tfrac12 T via the correction formula.

Problem 5: Exponential martingale

Let θ∈R\theta\in\mathbb R. Show that

Et(θ)=exp⁡ ⁣(θWt−12θ2t)\mathcal E_t(\theta) = \exp\!\left(\theta W_t - \tfrac12\theta^2 t\right)

is a martingale by verifying dEt=θEt dWtd\mathcal E_t = \theta\mathcal E_t\,dW_t (use the Itô formula from Chapter 3 in anticipation).


2.12 Selected solutions​

Solution 1

By the Itô isometry,

Var ⁣(∫0Th(t) dWt)=E ⁣[(∫0Th(t) dWt)2]=∫0Th(t)2 dt.\text{Var}\!\left(\int_0^T h(t)\,dW_t\right) = \mathbb E\!\left[\left(\int_0^T h(t)\,dW_t\right)^2\right] = \int_0^T h(t)^2\,dt.

The integral is also Gaussian with mean zero, so the distribution is fully determined by this variance.

Solution 2

For constant Ht=cH_t = c, the simple-process sum is c∑kΔWk=c(WT−W0)=cWTc\sum_k\Delta W_k = c(W_T - W_0) = cW_T. The isometry gives E[(cWT)2]=c2T=c2∫0Tdt\mathbb E[(cW_T)^2] = c^2 T = c^2\int_0^T dt. Both sides match.

Solution 3

By polarization: [M,N]=14([M+N,M+N]−[M−N,M−N])[M,N] = \frac14([M+N,M+N] - [M-N,M-N]). The quadratic variation of ∫(H±K) dW\int(H\pm K)\,dW is ∫(H±K)2 ds\int(H\pm K)^2\,ds. Therefore

[M,N]T=14∫0T[(H+K)2−(H−K)2] ds=∫0THsKs ds.[M,N]_T = \frac14\int_0^T[(H+K)^2-(H-K)^2]\,ds = \int_0^T H_s K_s\,ds.
Solution 4

On each subinterval, the Stratonovich term is

Wtk+Wtk+12 ΔWk=Wtk ΔWk+12(ΔWk)2.\frac{W_{t_k}+W_{t_{k+1}}}{2}\,\Delta W_k = W_{t_k}\,\Delta W_k + \tfrac12(\Delta W_k)^2.

Summing and passing to the limit,

∫0TWt∘ dWt=∫0TWt dWt+12[W]T=(12WT2−12T)+12T=12WT2,\int_0^T W_t\circ\,dW_t = \int_0^T W_t\,dW_t + \tfrac12[W]_T = \left(\tfrac12 W_T^2 - \tfrac12 T\right) + \tfrac12 T = \tfrac12 W_T^2,

which is the ordinary calculus answer.


2.13 What this chapter gives you​

The Itô integral ∫0THt dWt\int_0^T H_t\,dW_t is:

PropertyStatement
Well-definedfor H∈Lad2H\in L^2_{\mathrm{ad}} via L2L^2 completion
Zero meanE[∫H dW]=0\mathbb E[\int H\,dW] = 0
L2L^2 isometryE[(∫H dW)2]=E[∫H2 dt]\mathbb E[(\int H\,dW)^2] = \mathbb E[\int H^2\,dt]
Martingale(Mt=∫0tH dW)(M_t = \int_0^t H\,dW) is a martingale
Quadratic variation[M]t=∫0tHs2 ds[M]_t = \int_0^t H_s^2\,ds
Continuous pathsa continuous version of MtM_t exists

The next chapter derives Itô's formula, the chain rule of stochastic calculus. Itô's formula is what makes the integral computable and connects it to classical analysis and partial differential equations.