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Line Integrals and Conservative Fields

date2026-07-15document_iddoc_33aed201931a972a0b59ac64db879a95description線積分と保存場を、曲線に沿う仕事量とポテンシャルの存在条件として整理する。prerequisites曲線・曲面のパラメータ表示 / 勾配・発散・回転type講義content_typelecturestatusactiverelateddata/lecture/math/vector-calculus/vector-calculus-portal.lecture.n.md / data/lecture/math/vector-calculus/gradient-divergence-and-curl.lecture.n.md / data/lecture/math/multivariable-calculus/parametrized-curves-and-surfaces.lecture.n.md / data/lecture/math/analysis/introduction-to-line-and-surface-integrals.lecture.n.md / data/lecture/math/vector-calculus/surface-integrals-and-flux.lecture.n.md / data/lecture/math/vector-calculus/green-gauss-and-stokes-theorems.lecture.n.md
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1Introduction

This lecture defines line integrals as accumulated quantities along curves and explains when the work integral of a vector field depends only on the endpoints. The distinction between local differential conditions and the global geometry of the domain is essential.

2Definitions

Let URn be open and let r:[a,b]U be an oriented piecewise C1 curve. For a continuous scalar field g:UR, define the scalar line integral by

Cgds=abg(r(t))r(t)dt.

For a continuous vector field F:URn, define the work line integral by

CF·dr=abF(r(t))·r(t)dt.

This lecture primarily concerns the second integral. A vector field is conservative if there is a function ϕC1(U) such that F=ϕ. The function ϕ is called a potential.

3Geometric Interpretation

In a work line integral, only the component of the vector field tangent to the direction of motion contributes. This explains the dot product F(r(t))·r(t). For a conservative field, the work depends on the initial and terminal points rather than on the path.

4Reparameterization and Orientation

Let ψ:[α,β][a,b] be a continuous piecewise C1 bijection and set ρ=rψ. If ψ is increasing, substitution shows that the work integral is unchanged. If ψ is decreasing, the curve orientation reverses and the work integral changes sign. A scalar line integral uses r, so reversing orientation does not change its sign.

5Fundamental Theorem for Line Integrals

Suppose F=ϕ. On each C1 segment of the curve, the chain rule gives

ddtϕ(r(t))=ϕ(r(t))·r(t).

Summing over all segments and applying the one-variable fundamental theorem yields

CF·dr=ϕ(r(b))-ϕ(r(a)).

Thus the integral depends only on the endpoints.

In this lecture, a domain U is path-connected if every two points of U can be joined by a piecewise C1 curve contained in U. For open sets, this condition is equivalent to the usual definition using continuous curves. More generally, let U be open and path-connected and let F be continuous. The following conditions are equivalent:

  1. There is a ϕC1(U) such that F=ϕ.
  2. The work integral between any two points of U is independent of the piecewise C1 path.
  3. The work integral around every piecewise C1 closed curve in U is zero.

Condition 1 implies Condition 2 by the chain-rule calculation above. To derive Condition 1 from Condition 2, fix a base point p0 and define

ϕ(p)=p0pF·dr.

Path independence makes this definition unambiguous. Because U is open, for each pU and sufficiently small h, the line segment from p to p+hei lies in U. Hence

ϕ(p+hei)-ϕ(p)h=1h0hFi(p+sei)dsFi(p)

by continuity of F. Thus iϕ=Fi for every i, so ϕC1(U) and ϕ=F. Condition 2 implies Condition 3 by comparing any closed curve with the constant curve having the same initial and terminal point. Conversely, under Condition 3, two paths with the same endpoints form a closed curve when one is traversed in reverse, and the zero integral around that closed curve proves that their integrals are equal.

6Domain Conditions and a Counterexample

Let UR2 or UR3 be open and simply connected, and let FC1(U). A domain is simply connected if every closed curve in it can be continuously contracted to a point without leaving the domain. In two dimensions, curl2DF=0 throughout U implies that F is conservative. In three dimensions, the corresponding sufficient condition is ×F=0 throughout U.

The assumption on the domain cannot be omitted. On U=R2{0}, consider

F(x,y)=(-yx2+y2,xx2+y2).

The field is smooth and has curl2DF=0 at every point of U. For the counterclockwise unit circle r(t)=(cost,sint), 0[PARSE ERROR: Undefined("Command(\"le\")")]t[PARSE ERROR: Undefined("Command(\"le\")")]2π, however, F(r(t))=r(t), so

CF·dr=02π1dt=2π.

Therefore the field is not conservative. Vanishing curl is a local condition and does not detect the hole in the domain. Simple connectivity is a standard sufficient condition for the implication from zero curl to conservativity; it is not necessary for every individual conservative field.

7Physical Interpretation

If a force field is conservative, its work is determined by the initial and terminal points. Under the physical convention that V is potential energy, F=-V, so the mathematical potential in this lecture is ϕ=-V. A conservative force performs zero work around every closed curve.

8Diagnostic Procedure

  • If every piecewise C1 closed curve in the domain has zero work integral, then the field is path-independent and conservative.
  • If a C1 field has zero curl on an open, simply connected domain, then it is conservative.
  • On a domain with holes, zero curl does not by itself guarantee path independence.

9Example 1: A Conservative Field

Let ϕ(x,y)=x2y. Then ϕ=(2xy,x2). For every piecewise C1 curve C from (0,0) to (1,1),

C(2xy,x2)·dr=ϕ(1,1)-ϕ(0,0)=1.

The value is the same for a line segment, a polygonal path, or any other admissible path.

10Example 2: A Nonconservative Field

Let F=(-y,x) and integrate around the counterclockwise unit circle r(t)=(cost,sint), 0[PARSE ERROR: Undefined("Command(\"le\")")]t[PARSE ERROR: Undefined("Command(\"le\")")]2π. Since

F(r(t))=(-sint,cost)=r(t),

we obtain

CF·dr=02π1dt=2π.

The nonzero integral around a closed curve proves that the field is not conservative.

11Related Lectures

data/lecture/math/vector-calculus/vector-calculus-portal.lecture.n.md data/lecture/math/vector-calculus/gradient-divergence-and-curl.lecture.n.md data/lecture/math/multivariable-calculus/parametrized-curves-and-surfaces.lecture.n.md data/lecture/math/analysis/introduction-to-line-and-surface-integrals.lecture.n.md data/lecture/math/vector-calculus/surface-integrals-and-flux.lecture.n.md data/lecture/math/vector-calculus/green-gauss-and-stokes-theorems.lecture.n.md
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