二階線形 PDE の分類
1導入
この
この
2一般形 と主部
を
であり、
である。 は
3判別量 と三分類
と
| の | |||
|---|---|---|---|
| なし | |||
| かつ | rank 1 の | ||
なら でも
4代表方程式 の計算
Laplace
では なので であり、
と
と
5座標変換 で型 が保 たれる理由
という
となり、 の
6特性曲線 との関係
である。
になる。この
を
7標準形 への入口
| 、または |
8型 から予想 できることとできないこと
が
たとえば
9反例 または限界
では なので である。したがって で
10よくある誤 り
- という
係数規約 を確認 せず、 へ別 の を代入 する。交差項 を と書 く規約 では、主係数行列 の非対角成分 は になる。 - だけを
見 て、 の退化 した式 まで放物型 と呼 ぶ。 型 を確認 しただけで、境界条件 、時間方向 、係数 の正則性 を調 べずに適切性 を結論 する。一点 での分類 を領域全体 へ広 げ、型変化 や一様性 を見落 とす。
11関連 リンク
data/lecture/math/partial-differential-equations/heat-wave-and-laplace-equations.lecture.n.md
Classification of Second-Order Linear PDEs
1Introduction
This lecture explains how to classify a second-order linear PDE in two variables pointwise from its highest-order derivatives and how to determine its characteristic directions and canonical form. The terms elliptic, parabolic, and hyperbolic suggest typical equilibrium, diffusion, and propagation behavior, but the type alone does not guarantee existence, uniqueness, or stability.
The discriminant classification presented here applies to two independent variables. In higher dimensions, it is generalized by counting the signs of the eigenvalues of the principal coefficient matrix.
2General form and principal part
On a domain , consider an equation with real-valued continuous coefficients,
Here are prescribed functions of and do not depend on or its derivatives; this is the meaning of linearity in . The {principal part} used for classification is
with principal coefficient matrix
The terms affect the particular form and well-posedness of solutions, but the type is determined by alone.
3Discriminant and the three types
At a point , set
At points where , equivalently where are not all zero, the classification is as follows.
| Discriminant condition | Type | Sign structure of | Real characteristic directions |
|---|---|---|---|
| {Elliptic} | positive or negative definite | none | |
| and | {Parabolic} | positive or negative semidefinite of rank 1 | one repeated direction |
| {Hyperbolic} | indefinite | two distinct directions |
If , then the second-order principal part is absent, so the equation is not called parabolic even though . When the coefficients vary, the classification is pointwise rather than automatically valid throughout the domain.
4Computations for representative equations
For Laplace's equation
one has and , so and the equation is elliptic.
Write the heat equation in the variable order as
Then and , so and has rank 1; the equation is parabolic. The term is first order and therefore does not enter the classification, although it is essential in determining the direction of time evolution.
For the wave equation
one has , , and , so and the equation is hyperbolic.
5Why the type is preserved under coordinate changes
Let the new coordinate functions be of class , and let be their Jacobian matrix. At a point where , the inverse function theorem makes them local coordinates, and the principal coefficient matrix in the new coordinates is transformed by congruence:
Consequently,
so the sign of is unchanged. Transforming a variable-coefficient equation also produces lower-order terms from second derivatives of the coordinate functions, but the type of the principal part is preserved by a nonsingular coordinate change. This conclusion is unavailable for a singular transformation.
6Relation to characteristic curves
The normal direction to a curve is the gradient . The curve is {characteristic} for the principal part when
Writing the tangent direction as gives the equivalent homogeneous condition
This formulation also includes vertical curves. If the curve is written as and , its normal is proportional to , and hence
When , this is a quadratic equation for the finite slope , with discriminant . If , the quadratic term disappears; the equation is linear when and constant when . A vertical direction may then be invisible in the slope coordinate . One must return to the homogeneous equation or use a representation . Counting all projective directions yields the numbers of real characteristic directions in the classification table.
For the heat equation, is a repeated root, so is characteristic for the second-order principal part. Nevertheless, one initial value can be prescribed at for forward evolution because the first-order term remains and creates the parabolic evolution structure. The non-characteristic condition for a first-order quasilinear PDE in the preceding lecture must not be identified with this characteristic condition for a second-order principal part.
data/lecture/math/partial-differential-equations/method-of-characteristics.lecture.n.md7Entry point to canonical forms
At a single point, a nonsingular linear coordinate transformation, together with multiplication of the entire equation by when necessary, reduces the principal part to one of the following forms.
| Type | Canonical form of the principal part |
|---|---|
| Elliptic | |
| Parabolic | |
| Hyperbolic | , or in characteristic coordinates |
Reducing a variable-coefficient equation to canonical form throughout a neighborhood additionally requires sufficient coefficient regularity, constancy of type, and the existence of suitable local coordinates. A global reduction does not follow automatically.
8What the type does and does not predict
The type is an entry point for selecting a problem formulation and a method of solution. The following correspondences hold only under representative additional assumptions.
| Type | Typical picture | Examples of additional conditions |
|---|---|---|
| Elliptic | boundary values and interior equilibrium; maximum principles | uniform ellipticity, signs of lower-order coefficients, domain and boundary conditions |
| Parabolic | forward time evolution and smoothing | a positive lower bound for the diffusion coefficient, time direction, coefficients and initial-boundary data |
| Hyperbolic | finite-speed propagation and energy methods | preservation of distinct real characteristic directions, an appropriate time surface, coefficient regularity |
{Uniform ellipticity} on a domain means that there are a fixed and constants such that, at every point and for every ,
This condition makes the eigenvalue signs consistent throughout the domain and keeps their magnitudes uniformly separated from both zero and infinity. Such uniformity is important when estimates associated with a type are applied over an entire domain.
For example, the forward and backward heat equations have the same parabolic principal-part classification, but their stability properties differ. Likewise, ellipticity alone does not imply that arbitrary boundary conditions determine a unique solution. Initial conditions, boundary conditions, and well-posedness must be assessed for the complete problem separately from its type.
data/lecture/math/partial-differential-equations/initial-and-boundary-value-problems.lecture.n.md9Counterexample and limitation
For an equation whose coefficients vary with position, the type need not be constant throughout the domain. For example,
has , , and , so . It is elliptic for , hyperbolic for , and parabolic of rank 1 for . The line is a type-change line where uniformity is lost; estimates and methods valid on one side cannot automatically be applied across it.
10Common errors
- Substituting the wrong coefficient into without checking the convention . Under the convention , the off-diagonal entries of the principal coefficient matrix are .
- Calling a degenerate equation with parabolic merely because .
- Concluding well-posedness from the type without examining boundary conditions, time direction, or coefficient regularity.
- Extending a pointwise classification to an entire domain while ignoring type changes or loss of uniformity.