Apply the entropy solution inequality for with level and for with level , integrate both in the other pair of variables, and add them. Symmetry of the Kruzhkov entropy flux produces derivatives and . A nonnegative mollifier concentrated near the diagonal then yields the Kato inequality for scalar conservation laws. Boundary-time terms require an initial trace argument, not merely interior translation continuity.
If on the solutions' state range, the Kato inequality for scalar conservation laws implies the displayed estimate for almost every . Approximate the shrinking interval by smooth cutoffs satisfying and multiply by a temporal cutoff ending at . Since , the lateral flux cannot increase the integral. The estimate gives uniqueness and a finite propagation speed without global assumptions on the data.
Subtract the weak equation for from its Kato inequality for scalar conservation laws and divide by two. The result is an inequality for with a flux bounded in magnitude by . The same shrinking-interval argument proves almost everywhere. Choosing the constant solution proves preservation of nonnegativity even when . Two-sided absolute-value contraction alone should not be mistaken for this one-sided comparison proof.
For the stated mollifier, . Thus the interior doubled integral is
On a bounded state range, is Lipschitz in each argument, and so is : away from the diagonal each partial derivative has modulus at most , and the function is continuous across the diagonal. Local translation continuity therefore makes this converge to the corresponding single-time, single-space integral. The compact time support is chosen below , with a margin for .
The initial terms need a separate argument. Since the time kernel is supported at , is identically zero for , whereas samples at .
The averaged initial trace of an entropy solution follows directly from its inequalities. Test the constant-level entropy for with , using smooth approximations of that temporal cutoff. Boundedness of and its entropy flux gives
Approximate locally in by finitely many constants with a smooth nonnegative partition of unity. Applying this estimate on each partition member and using the triangle inequality makes the limsup of arbitrarily small. This proves its convergence to zero for each compact .
The time kernel has size and the spatial kernel is a normalized approximate identity. The averaged trace, followed by spatial translation continuity of , therefore gives . Its time mass is one, not one-half, because its whole support lies on the positive side. Consequently
This is the Kato inequality for scalar conservation laws with its initial contribution. Assuming an initial trace solely from interior translation continuity would leave a gap; the entropy argument above supplies it.
Put , and . The mean value theorem gives on the bounded state range. Fix a final time and let and . Choose a smooth increasing function equal to zero on and one on . For small , define
Its two nonnegative derivative contributions imply . Therefore .
Use the nonnegative test , where , it is one up to just before , decreases smoothly to zero near , and remains zero afterward. The Kato inequality for scalar conservation laws gives
because the other interior contribution is nonpositive. At Lebesgue times , the temporal approximate identity tends to ; take a countable sequence and use dominated convergence on the bounded cone. This yields
for almost every . This is local L1 contraction for scalar conservation laws. It uses only local integrability, so the bounded data need not have finite global norm. If , the flux difference is zero and the same proof uses a stationary interval.
If , the right-hand side of the local L1 contraction for scalar conservation laws estimate is zero. Applying it on a countable collection of rational intervals and final times proves almost everywhere in space-time. Thus
To deduce nonnegativity one needs a one-sided comparison, rather than merely putting in the absolute-value estimate. The difference satisfies the weak equation with flux . Subtract its weak integral identity from the Kato inequality for scalar conservation laws and divide by two. The result is the same inequality for
When both expressions vanish; when , . The shrinking-interval proof therefore bounds the negative part by its initial negative part. This is order preservation for scalar entropy solutions.
The constant is an entropy solution for every , even if , because the constant flux has zero spatial derivative. If , its initial negative part is zero, and comparison gives
This explicitly establishes the additional sign conclusion without incorrectly identifying uniqueness alone with order preservation.