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Local smooth balances with continuous body sources
Smooth positive-density material branch with C1 stored fields and only continuous body acceleration and heat supply; no weak, shock, or vacuum extension.
Statement
Assume countable choice. Let be an open interval containing , let be a bounded open reference region with boundary (locally a graph with the region on one side), and let be an open neighborhood of . Let have orientation-preserving diffeomorphic time slices (bijections onto open images with inverses and positive Jacobian determinant) and satisfy , and set and . Here means all coordinate partial derivatives through order are continuous. Let , , , , and be on . Let and be continuous. Require for every , so is the velocity induced by this same material motion. Their SI units are respectively kilograms per cubic metre, metres per second, joules per kilogram, watts per square metre, pascals, metres per second squared, and watts per kilogram. Put , , , , , and . Use rowwise divergence , vector divergence , and traction , where is the outward Euclidean unit normal and denotes heat leaving the material region.
Assume pointwise mass continuity and, on every material region where is a nonempty bounded open reference region with compact closure in and boundary locally a graph with the region on one side, the adopted linear-momentum, angular-momentum, and total-energy balances The angular balance is about a fixed inertial origin and there are no surface couples or intrinsic spin. Then throughout the balanced physical region , with retained only as the ambient regularity domain, and Conversely, the pointwise momentum equation and symmetric stress imply the angular-momentum balance, and the pointwise total-energy equation implies its stated material integral balance. All deductions are conditional on the smooth model and do not assert existence of a solution.
Statement references
Single-component nonpolar continuum and material balances
Material mass balance implies local continuity
Smooth transport, Jacobian and advected reference density
Divergence on a bounded C1 Euclidean domain
Powers, Lecture Notes on Intermediate Fluid Mechanics, §§4.2–4.5.
Mei, MIT OpenCourseWare, Law of Momentum Conservation, §1.5.
Mei, MIT OpenCourseWare, Heat and Energy Conservation, §4.1.
Facts & Assumptions
Given: Countable choice; the smooth motion, its induced velocity , and field regularity; pointwise mass continuity; and the material momentum, angular-momentum, and total-energy balances in the Statement.
Single-component nonpolar continuum and material balances: the smooth model adopts the displayed material momentum, angular-momentum, and total-energy balances, with traction , no couples, and continuous body acceleration and heat supply.
Classical frames, primitive quantities and SI units: is Eulerian velocity, , stress is a spatial tensor with traction , and the stated field types and SI units apply.
Material mass balance implies local continuity: the adopted material mass integral gives for the smooth positive-density motion.
Smooth transport, Jacobian and advected reference density: for a compact Jordan material set and a field , , componentwise for vector fields.
C1 material regions have compatible Jordan volume integrals: bounded material regions and their diffeomorphic images are Jordan measurable, and their open-region integrals agree with integrals over compact closures.
Divergence on a bounded C1 Euclidean domain: under countable choice, the Euclidean divergence theorem holds for a bounded domain and a vector field on its closure.
The Axiom of Countable Choice (): countable choice means that each countable family of nonempty sets has a choice function.
Proof
Fix an admissible and let . By [F4], is compact Jordan and its open-region integrals equal the corresponding closure integrals. Apply [F3] componentwise to ; the derivative of its material integral is Pointwise mass continuity and the product rule give
Substitute the first balance in [A1] into step 1.1 and apply [F5] to , using countable choice from [F6]. This yields The integrand is continuous because is continuous and the other fields are . Every sufficiently small open ball is such a material region: its inverse image under is a bounded region compactly contained in . If a component of the continuous integrand were nonzero at a point, it would have a strict fixed sign on a smaller ball and its integral there could not vanish. Thus pointwise on .
For each component , The last term is zero by [F2]. Substituting step 2.1 and moving to the flux gives the conservative momentum equation.
Apply [F3] to and use and . The transport derivative is . Substitute step 2.1 and compare with the angular balance in [A1]; applying [F5] to the moment-stress flux gives This residual is continuous, so the fixed-sign-ball argument of step 2.1 makes it zero pointwise. With the alternating symbol and , direct differentiation gives For these equations are respectively , , and , hence .
Apply [F3] to in the total-energy balance [A1]. Rewrite and apply [F5] to and . The integral of the continuous residual is zero on every . The fixed-sign-ball argument from step 2.1 proves that this residual vanishes pointwise. Conversely, integrating this local equation and using [F3] and [F5] recovers the material total-energy balance.
If is symmetric, the component identity in step 3.2 gives . The product rule and give Use step 3.1 and the stress-divergence identity, then integrate over . The transport formula [F3] and divergence theorem [F5] recover the angular-momentum integral balance in [A1].
Dot from step 2.1 with . The component product rule gives . Since is symmetric, its contraction with the skew part of is zero, so . Also . Combining these identities with [F2] yields
Subtract the kinetic equation in step 4.2 from the total-energy equation in step 3.3 and use . The body-work terms cancel and leave . Expanding the mass-transport term using [F2] gives . Conversely, adding this internal-energy equation to the kinetic equation in step 4.2 recovers the total-energy equation in step 3.3.
Depends on
Single-component nonpolar continuum and material balances
Classical frames, primitive quantities and SI units
Material mass balance implies local continuity
Smooth transport, Jacobian and advected reference density
C1 material regions have compatible Jordan volume integrals
Divergence on a bounded C1 Euclidean domain
The Axiom of Countable Choice ()