Consider an infinite plane in ℝ³ — a 2-dimensional flat surface extending in all directions. What is its Lebesgue measure λ₃?
AInfinite — it has infinite 2D area, so its 3D measure must also be infinite
BZero — it has no 3-dimensional thickness, so it contributes nothing to 3D volume
COne — by convention, a codimension-1 set is assigned unit measure
DUndefined — Lebesgue measure only applies to sets with the same dimension as the ambient space
A plane in ℝ³ has λ₃-measure zero, even though it has infinite 2D area. The key insight is that Lebesgue measure on ℝⁿ measures n-dimensional volume. A 2D plane, no matter how large, has no 3-dimensional thickness — it cannot be approximated by any finite or even σ-finite collection of 3D boxes with positive total volume. This is why lower-dimensional sets are 'negligible' in the measure-theoretic sense: they contribute zero to integrals over ℝ³, regardless of their geometric size in their own dimension.
Question 2 Multiple Choice
A function f: ℝ² → ℝ is defined everywhere and you change its values on the x-axis (a 1-dimensional line in ℝ²). How does this affect the Lebesgue integral ∫∫f dλ₂?
AThe integral changes by an amount proportional to the total variation of f on the x-axis
BThe integral is unchanged — the x-axis has λ₂-measure zero, so changes on it are irrelevant to integration
CThe integral is undefined after the modification because the function is no longer measurable
DThe integral changes only if f was previously continuous on the x-axis
The x-axis in ℝ² has λ₂-measure zero (it is a 1-dimensional set in a 2-dimensional space). Lebesgue integration ignores sets of measure zero: ∫f dλ = ∫g dλ whenever f = g almost everywhere (i.e., everywhere except possibly on a set of measure zero). This robustness is one of the fundamental advantages of Lebesgue over Riemann integration — you can change function values on any lower-dimensional set, any countable set, or any other measure-zero set without affecting the integral at all.
Question 3 True / False
Any smooth surface (such as a sphere or a paraboloid) in ℝ³ has λ₃-measure zero.
TTrue
FFalse
Answer: True
True. Smooth surfaces are 2-dimensional manifolds embedded in ℝ³. They have no 3-dimensional thickness — they cannot fill any open ball in ℝ³, and they can be covered by 3D boxes of arbitrarily small total volume. Formally, this follows from the general principle that any k-dimensional smooth manifold (k < n) has λₙ-measure zero. This means integration over ℝ³ is completely unaffected by what a function does on any smooth surface, curve, or point.
Question 4 True / False
A set of Lebesgue measure zero in ℝⁿ is expected to be either finite or countably infinite.
TTrue
FFalse
Answer: False
False. Many uncountable sets have Lebesgue measure zero. The classic example on ℝ is the Cantor set — uncountable yet λ₁-measure zero. In ℝⁿ, any smooth curve, surface, or lower-dimensional manifold is uncountable and yet has measure zero. For instance, the x-axis in ℝ² contains uncountably many points but has λ₂-measure zero. The 'negligibility' captured by measure zero is about n-dimensional volume, not cardinality.
Question 5 Short Answer
Explain why a 2-dimensional plane has Lebesgue measure zero in ℝ³, and why this fact matters for integration over ℝ³.
Think about your answer, then reveal below.
Model answer: A plane in ℝ³ has no 3-dimensional thickness: it can be enclosed in a collection of 3D boxes whose total volume is arbitrarily small (take boxes of height ε centered on the plane). By definition, this means its λ₃-measure is zero. For integration, this means changes to a function on any plane — or any surface, curve, or lower-dimensional set — leave the Lebesgue integral unchanged. This is what 'almost everywhere' means: properties that hold everywhere except on a set of measure zero are sufficient for all integration-theoretic purposes.
This measure-zero phenomenon is not merely a curiosity — it underpins the concept of 'almost everywhere' equality, which makes Lebesgue integration robust and allows function spaces like L² to treat functions that differ only on a set of measure zero as identical. It also explains why you can safely ignore discontinuities on curves or surfaces when computing integrals, and why Fourier series can converge almost everywhere even to functions with countably many jumps.