For , apply the area formula to the velocity map and bound the initial data by their velocity essential supremum. This gives the displayed mixed Lebesgue norm estimate whenever the weighted inverse multiplicity is essentially bounded. If is injective and , the constant is at most . In dimension one a derivative bounded away from zero gives a global diffeomorphism; in higher dimensions determinant bounds alone do not.
The displayed smooth map from to the punctured plane has Jacobian determinant one: in polar coordinates its radius is and its angle is , so the determinant is . Nevertheless for every integer . Thus a local volume-preserving map need not be injective or have bounded weighted inverse multiplicity. Compactly supported data distributed over many inverse branches disprove a determinant-only dispersion with a nonlinear velocity map estimate.
The displayed estimate has two independent defects. Even for , its right side cannot use . At , choose nonnegative smooth functions with compact support and prescribe . This is a legitimate transported solution with . The proposed inequality would require
Velocity dilation makes arbitrarily large, while the other factors stay fixed. Thus no universal works with the same-time mixed Lebesgue norm.
There is a second issue after replacing by : the Jacobian determinant bounds give a local diffeomorphism, not necessarily a one-to-one map. Suppose additionally that is injective. With , the change of variables formula and give
Surjectivity is not needed because the domain of integration can be enlarged. With injectivity, the corrected estimate has . The upper bound is unnecessary.
More generally, dispersion with a nonlinear velocity map uses the area formula to sum over inverse branches. Define the weighted inverse multiplicity
If , the same argument gives the corrected estimate with . At most inverse branches give . Thus the missing global assumption concerns multiplicity, not merely local volume distortion.
For a noninjective map with constant Jacobian determinant giving a counterexample in two dimensions, write and set
The polar coordinates calculation gives , yet for every integer . To turn this into a failure of the estimate, take a small open disk about that avoids the origin. For each of inverse branches over , choose a smooth cutoff supported on that branch, where has support strictly inside and is extended by zero. These velocity supports are disjoint. Set
Then , independent of , whereas at a fixed and suitable ,
The last integral is positive and independent of . No finite exists for this fixed , although . In one dimension, by contrast, a nonvanishing derivative has a constant sign, so the lower derivative bound makes a global diffeomorphism.