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A nonzero Q-exact deformation on the four-torus

Example

Let T4=(R/2πZ)4 have global angular coordinates x1,…,x4 and orientation ω=dx1∧dx2∧dx3∧dx4. Use the graded algebra Ω∙(T4;C) and integrate an inhomogeneous form by integrating its degree-four component over T4. Let Q=d be the exterior derivative, determined by df=∑i(∂if) dxi, d(dxi)=0, and the graded Leibniz rule. Set O=dx1∧dx2, S=dx3∧dx4, and V=sin⁡(x3) dx4. For t∈R, define Z(t)=∫T4(Oe−S−tQV)[4]. The degree-four density is −(1+tcos⁡(x3))ω, which depends on t at points where cos⁡(x3)≠0, but Z(t)=−(2π)4 for every t∈R.

Facts & Assumptions

Given: T4=(R/2πZ)4, its oriented volume form ω, the exterior derivative Q=d, and the forms O,S,V specified in the Example.

[F1]

Finite-Dimensional Q-Exact Localization Data: the graded integral extracts the top-degree form and integrates it over the oriented cycle; an odd derivation is Q-invariant when the integral of every admissible Q-derivative vanishes.

[F2]

Finite-Dimensional Q-Exact Deformation Invariance: if QS=QO=0, (Q2V)e−S−tQV=0, the Q-boundary contribution vanishes, and the integrand and parameter derivative have an integrable majorant on compact parameter intervals, then IΓ(Oe−S−tQV) is constant in t.

Verification

1.1givenF1

For a smooth periodic three-form η=∑i=14(−1)i−1ai(x) dx1∧⋯dxi^⋯∧dx4, the degree-four coefficient of dη is ∑i∂iai. For each i, integrating ∂iai over xi∈[0,2π] gives ai∣xi=2π−ai∣xi=0=0 by periodicity; iterated integration over the other three coordinates therefore gives ∫T4(dη)[4]=0. Thus IΓ(QF)=0 for every F.

2.1givenF2step 1.1algebra

Directly, QO=QS=0, QV=dV=cos⁡(x3) dx3∧dx4, and Q2V=d(dV)=−sin⁡(x3) dx3∧dx3∧dx4=0. For t in any compact interval K, the coefficients of Oe−S−tQV and its t-derivative are bounded on the compact torus by 1+sup⁡t∈K∣t∣; this constant is integrable on T4. Therefore [F2] applies.

3.1step 2.1algebra

Put Ht=S+tQV=(1+tcos⁡(x3)) dx3∧dx4. Since Ht∧Ht=0, e−Ht=1−Ht. Multiplication by O gives (Oe−Ht)[4]=−(1+tcos⁡(x3))ω.

4.1step 3.1algebra∎

The integral of cos⁡(x3) over [0,2π] is zero, while each of the four coordinate intervals has length 2π. Hence Z(t)=−∫[0,2π]4(1+tcos⁡(x3)) d4x=−(2π)4, independent of t; the pointwise t-dependent term integrates to zero by the same periodic boundary cancellation as in step 1.1.

Depends on

Dependency tree · 2 levels