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Integral curve
Integral curve
from Wikipedia

In mathematics, an integral curve is a parametric curve that represents a specific solution to an ordinary differential equation or system of equations.

Name

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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.

Definition

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Suppose that F is a static vector field, that is, a vector-valued function with components (F1,F2,...,Fn) in a Cartesian coordinate system, 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,

Such a system may be written as a single vector equation,

This equation says that the vector tangent to the curve at any point x(t) along the curve is precisely the vector F(x(t)), and so the curve x(t) is tangent at each point to the vector field F.

If a given vector field is Lipschitz continuous, then the Picard–Lindelöf theorem implies that there exists a unique flow for small time.

Examples

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Three integral curves for the slope field corresponding to the differential equation dy / dx = x2x − 2.

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.

Generalization to differentiable manifolds

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Definition

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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 : TMM given by

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 pM. An integral curve for X passing through p at time t0 is a curve α : JM of class Cr−1, defined on an open interval J of the real line R containing t0, such that

Relationship to ordinary differential equations

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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

It is local in the sense that it is defined only for times in J, and not necessarily for all tt0 (let alone tt0). 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.

Remarks on the time derivative

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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:

In the special case that M is some open subset of Rn, this is the familiar derivative

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 tJ. 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 tJ.

References

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
In , an integral curve of a smooth XX on a manifold MM is a smooth γ:IM\gamma: I \to M, where IRI \subseteq \mathbb{R} is an open interval containing 0, such that γ(0)=p\gamma(0) = p for some point pMp \in M and the γ(t)=X(γ(t))\gamma'(t) = X(\gamma(t)) for all tIt \in I. This condition means that at every point along the , its velocity matches the direction and magnitude specified by the , providing a geometric realization of the solutions to the autonomous system of first-order ordinary differential equations dxdt=X(x)\frac{dx}{dt} = X(x) on the manifold. Integral curves are fundamental to understanding the dynamics of vector fields, as they trace the trajectories of points evolving under the field's influence, akin to particle paths in a velocity field. For a given initial point pp, there exists a unique maximal integral curve defined on the largest possible interval, guaranteed by local existence and uniqueness theorems from ordinary differential equation theory, such as the Picard–Lindelöf theorem, which applies when the vector field is locally Lipschitz continuous. If the vector field is nowhere zero along the curve, the integral curve is an immersion, embedding a one-dimensional submanifold into MM. The collection of all integral curves of a generates its flow, a smooth one-parameter group of diffeomorphisms ϕt:MM\phi_t: M \to M (or defined on an open subset of R×M\mathbb{R} \times M) satisfying ϕ0=id\phi_0 = \mathrm{id}, ϕs+t=ϕsϕt\phi_{s+t} = \phi_s \circ \phi_t, and where each ϕt(p)\phi_t(p) lies on the integral curve through pp. Flows are complete if defined for all tRt \in \mathbb{R}, which occurs for complete vector fields, such as those on compact manifolds. These structures underpin key applications in dynamical systems, theory, and the study of symmetries on manifolds, enabling the analysis of long-term behavior and invariant sets.

Fundamental Concepts

Definition

In the context of a VV on Rn\mathbb{R}^n, an is a parametric γ:IRn\gamma: I \to \mathbb{R}^n, where IRI \subseteq \mathbb{R} is an open interval, such that the to the at each point matches the evaluated at that point. Specifically, γ\gamma is an integral curve of VV if it is continuously differentiable (i.e., C1C^1) and satisfies the γ(t)=V(γ(t))\gamma'(t) = V(\gamma(t)) for all tIt \in I. Here, the VV assigns a vector to each point in Rn\mathbb{R}^n, and the integral curve γ\gamma traces a path where the instantaneous γ(t)\gamma'(t) follows this assignment precisely, representing the of a particle moving under the "flow" dictated by VV. While the geometric path through a given initial point is unique, the parameterization is fixed by the vector field such that the tangent vector matches VV exactly; general reparameterizations do not preserve this property for the same VV. The standard parameterization is typically taken with respect to time tt, where the speed along the curve is given by the magnitude of the vector field, γ(t)=V(γ(t))|\gamma'(t)| = |V(\gamma(t))|, rather than arc length (which would normalize the speed to 1 and correspond to the integral curve of the unit vector field V/VV/|V|). This time-like parameterization aligns with the interpretation of VV as specifying both direction and speed at each point.

Etymology

The term "integral curve" originates from the method of solving ordinary differential equations (ODEs) by integration, wherein the curve embodies the accumulated path derived from integrating the direction field specified by the equation. This conceptual linkage underscores how the curve "integrates" the infinitesimal directions provided by the , forming a complete solution trajectory. The underlying concepts gained prominence in the 19th century amid advancements in ODE theory, with foundational existence results by (ca. 1820s–1840s) and geometric interpretations in dynamical systems by (early 1800s). formalized the concept in the 1870s by connecting integral curves to continuous transformation groups and integrating factors for ODEs. Linguistically, "" derives from the Latin integralis, denoting wholeness or completeness, reflecting the curve's role as the path that resolves the differential relation into a unified geometric object; "," from the Latin curvus meaning bent, specifies its form as a one-dimensional manifold in the plane or . This distinguishes "integral curve" from synonymous terms like "solution curve" or "" by emphasizing the integrative process over mere parametric description or physical motion.

Examples and Illustrations

Basic Examples

One of the simplest examples of an integral curve arises in one-dimensional R1\mathbb{R}^1, where the is given by V(x)=xV(x) = x. The integral curve γ(t)\gamma(t) satisfying γ(t)=V(γ(t))\gamma'(t) = V(\gamma(t)) with initial condition γ(0)=γ0\gamma(0) = \gamma_0 is explicitly γ(t)=γ0et\gamma(t) = \gamma_0 e^t, as this satisfies the dγdt=γ\frac{d\gamma}{dt} = \gamma whose solution is the . In two-dimensional R2\mathbb{R}^2, consider a constant V(x,y)=(1,0)V(x, y) = (1, 0). The integral curves are horizontal straight lines, parametrized as γ(t)=(t+a,b)\gamma(t) = (t + a, b) for constants a,bRa, b \in \mathbb{R}, since the γ(t)=(1,0)\gamma'(t) = (1, 0) matches V(γ(t))V(\gamma(t)) at every point along the curve. Another illustrative example in R2\mathbb{R}^2 is the V(x,y)=(y,x)V(x, y) = (-y, x), which generates circular orbits centered at the origin. The integral curves are circles given by γ(t)=(acostbsint,asint+bcost)\gamma(t) = (a \cos t - b \sin t, a \sin t + b \cos t) for initial conditions determining constants a,bRa, b \in \mathbb{R}, as these parametrizations satisfy γ(t)=V(γ(t))\gamma'(t) = V(\gamma(t)) and trace out circles of radius a2+b2\sqrt{a^2 + b^2}
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