Integral curve should not be confused with Curve integral.
In mathematics, an integral curve is a parametric curve that represents a specific solution to an ordinary differential equation or system of equations.
Integral curves are known by various other names, depending on the nature and interpretation of the differential equation or vector field. In physics, integral curves for an electric field or magnetic field are known as field lines, and integral curves for the velocity field of a fluid are known as streamlines. In dynamical systems, the integral curves for a differential equation that governs a system are referred to as trajectories or orbits.
Suppose that F is a static vector field, that is, a vector-valued function with Cartesian coordinates (F1,F2,...,Fn), and that x(t) is a parametric curve with Cartesian coordinates (x1(t),x2(t),...,xn(t)). Then x(t) is an integral curve of F if it is a solution of the autonomous system of ordinary differential equations,
| \begin{align} | dx1 |
| dt |
&=F1(x1,\ldots,xn)\ &\vdots\\
| dxn | |
| dt |
&=Fn(x1,\ldots,xn). \end{align}
x'(t)=F(x(t)).
If a given vector field is Lipschitz continuous, then the Picard–Lindelöf theorem implies that there exists a unique flow for small time.
If the differential equation is represented as a vector field or slope field, then the corresponding integral curves are tangent to the field at each point.
Let M be a Banach manifold of class Cr with r ≥ 2. As usual, TM denotes the tangent bundle of M with its natural projection πM : TM → M given by
\piM:(x,v)\mapstox.
A vector field on M is a cross-section of the tangent bundle TM, i.e. an assignment to every point of the manifold M of a tangent vector to M at that point. Let X be a vector field on M of class Cr-1 and let p ∈ M. An integral curve for X passing through p at time t0 is a curve α : J → M of class Cr-1, defined on an open interval J of the real line R containing t0, such that
\alpha(t0)=p;
\alpha'(t)=X(\alpha(t))forallt\inJ.
The above definition of an integral curve α for a vector field X, passing through p at time t0, is the same as saying that α is a local solution to the ordinary differential equation/initial value problem
\alpha(t0)=p;
\alpha'(t)=X(\alpha(t)).
It is local in the sense that it is defined only for times in J, and not necessarily for all t ≥ t0 (let alone t ≤ t0). Thus, the problem of proving the existence and uniqueness of integral curves is the same as that of finding solutions to ordinary differential equations/initial value problems and showing that they are unique.
In the above, α′(t) denotes the derivative of α at time t, the "direction α is pointing" at time t. From a more abstract viewpoint, this is the Fréchet derivative:
(dt\alpha)(+1)\inT\alphaM.
In the special case that M is some open subset of Rn, this is the familiar derivative
\left(
| d\alpha1 | |
| dt |
,...,
| d\alphan | |
| dt |
\right),
where α1, ..., αn are the coordinates for α with respect to the usual coordinate directions.
The same thing may be phrased even more abstractly in terms of induced maps. Note that the tangent bundle TJ of J is the trivial bundle J × R and there is a canonical cross-section ι of this bundle such that ι(t) = 1 (or, more precisely, (t, 1) ∈ ι) for all t ∈ J. The curve α induces a bundle map α∗ : TJ → TM so that the following diagram commutes:
Then the time derivative α′ is the composition α′ = α∗ o ι, and α′(t) is its value at some point t ∈ J.
. Serge Lang . Differential manifolds . Addison-Wesley Publishing Co., Inc. . Reading, Mass. - London - Don Mills, Ont. . 1972 .