Seeking to explain thermodynamics based on moving and interacting atoms

Chapter 11 – Enthalpy (H)

Enthalpy (H) – created in the mid-1800s by William Thomson and others

Internal energy U is the natural property for analyzing closed, non-flowing systems — a gas inside a piston-in-cylinder assembly, a bomb calorimeter, a sealed batch reactor. In each case the system boundary is fixed or moves only mechanically, and U captures everything we need.

But U alone is insufficient for flowing systems, where material crosses boundaries under pressure and carries energy with it. When a fluid flows from one region to another, pressure forces do work on it — pushing it in from upstream and being pushed back by it downstream. This flow work, equal to PV at each boundary, must be accounted for since the net work done on the parcel changes its internal energy. In a non-flowing system this bookkeeping isn’t needed. In a flowing system it is essential.

What flow work means at the atomic level – a two piston model

To see what flow work physically is, imagine a parcel of fluid moving through a pipe with a piston at each end — one upstream pushing the parcel forward, one downstream resisting its advance. The upstream piston does work P₁V₁ on the parcel; the downstream piston extracts work P₂V₂ from it. The net flow work delivered to the parcel is P₁V₁ − P₂V₂.

These are not mechanical devices installed in the pipe. They are the pressure of the surrounding fluid acting on the parcel’s boundary faces — which is exactly what pressure does. The upstream fluid pushes. The downstream fluid resists. The parcel moves through, carrying its internal energy U with it, and the net work done on it by those two pressure faces is P₁V₁ − P₂V₂. At the atomic level, this pushing is nothing more than the collective effect of billions of molecular collisions on each face of the parcel — the same collisions that give rise to pressure in the first place, as established in Chapter 8.

This means that a parcel of flowing fluid carries two distinct forms of energy with it: the internal energy U stored in the motion and interactions of its atoms, and the flow work PV that had to be supplied to push it into the flow stream against the prevailing downstream pressure. The sum of these two — H = U + PV — is the total energy the parcel transports as it moves.

This picture also makes clear why flow work is absent from closed non-flowing systems. In a sealed piston-in-cylinder assembly, no fluid crosses a boundary, so there are no upstream and downstream pressure faces doing work on a moving parcel. The only work is the mechanical expansion or compression of the gas against the single piston face. Once fluid starts flowing — crossing system boundaries — the two-piston picture becomes necessary, and H replaces U as the natural conserved quantity.

The Joule-Thomson experiment and the derivation of H

The need for this composite property became clear when James Joule and William Thomson performed one of the more famous experiments in the history of thermodynamics. They forced a gas through a porous plug — a flow resistance — under adiabatic conditions and measured a temperature change on the downstream side. This depressurization cooled most gases but heated some, including hydrogen at room temperature. To understand what was happening, Thomson applied the First Law.

For an adiabatic process (Q = 0) with no shaft work — no work done by mechanically rotating a shaft inside a pump, turbine, or compressor — the only energy exchanges are the flow work done on the system upstream (P₁V₁) and the flow work done by the system downstream (P₂V₂). The First Law then gives:

ΔU = U₂ − U₁ = P₁V₁ − P₂V₂

Rearranging:

U₁ + P₁V₁ = U₂ + P₂V₂

The quantity U + PV is conserved across the plug. This combination was given the name enthalpy:

H = U + PV

H₁ = H₂

ΔH = 0 for adiabatic, isenthalpic flow — no heat transfer, no shaft work beyond the flow work itself.

This result constrains what can happen across the plug: whatever the fluid does — expand, cool, heat — it must do so while keeping H constant. Whether that constant H corresponds to a higher or lower temperature on the downstream side depends on how H varies with pressure for the specific gas involved. For most gases at ordinary conditions, isenthalpic expansion produces cooling. For hydrogen at room temperature, it produces heating. The full explanation of why requires understanding the interplay between intermolecular attraction and repulsion as the gas expands — a topic explored in a later chapter on the Joule-Thomson effect.

What enthalpy is — and is not

Just as U is the conserved property of choice for non-flowing systems, H becomes the conserved property of choice for flowing systems. Enthalpy wasn’t invented arbitrarily. It was constructed to solve a specific physical problem: how to account for both the internal energy of a flowing fluid and the work required to push it through the flow stream against downstream pressure. The two-piston picture captures this exactly. H = U + PV does exactly that — and nothing more.

A common source of confusion is treating enthalpy as if it were a form of energy stored in a system, like a reservoir to be filled. It is not. Just as heat and work quantify energy in transit rather than energy at rest, enthalpy is a bookkeeping property — a composite that bundles internal energy and flow work into a single conserved quantity for the conditions where that bundling is useful. The energy is real. The atoms are real. The pushing and resisting of the two pressure faces are real. The property H is simply the tool we constructed to track it all cleanly in a single number.

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