Most balance laws in physics are written in simplified forms that implicitly assume the systemunder consideration is closed. The closed-system versions of the First and Second Laws are exact onlywhen no energy, entropy, or momentum crosses the system boundary. Many natural and engineeredsystems are strongly open, however, and small but persistent residuals arise when closed-systembalance laws are applied to them. In this paper we restore the boundary contributions impliedby the local conservation equation ∇aTab = 0 and obtain completed balance relations for opensystems. We show that any such system requires three elements: a state term, a driver term,and a boundary term that captures flux through the outer surface. We refer to this three-partstructure as the Flux Triad. When the boundary term is retained, the First, Second, and momentumbalance laws acquire explicit flux contributions Φ∞, Ψ∞, and Π∞ that describe energy, entropy orinformation, and momentum carried across the boundary. We derive these terms rigorously fromthe four-momentum form of ∇aTab = 0, show how temporal and spatial projections yield Φ∞ andΠ∞ respectively, and demonstrate that Ψ∞ is quantifiable from known thermodynamic relations. These terms correspond to processes already modeled in gravitational-wave sources, pulsars, comets,spacecraft, cosmology, biological membranes, and non-equilibrium thermodynamics. The resultingZero-Infinity First, Second, and Third Laws provide a consistent open-system framework derivablefrom standard conservation principles and resolve residuals that arise when open systems are treatedas closed.
Cromwell, Tami Marie Cromwell, Tammy Marie Stomberg, Tami Stomberg (Tue,) studied this question.