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SCIENCE · INVESTIGATE AND EXPLAIN

Close the first-law energy account

Distinguish path-dependent heat and work from endpoint-dependent internal energy.

Learning outcome: Use ΔU = Q − W with explicit signs, compute a monatomic ideal-gas energy change and reconcile each leg and whole path.

Starting recap

Q is positive into the gas; W is positive when the gas does work. Classical monatomic ideal-gas internal-energy changes use ΔU = 3nRΔT/2.

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Try

One path requires more heat than another but reaches the same final temperature. Where does the extra energy go?

Open the experiment

Predict

At final 300 kPa and 30 L, predict whether the two paths share ΔU and whether their heat inputs differ by the work difference.

Experiment

Check Q − W for each leg and for each path. Then select 100 kPa and 30 L: the gas expands but ends colder. Explain how signs of heat, work and energy change fit together.

Compare two paths between identical gas states

Worked teaching model · synthetic values · One mole of a classical monatomic ideal gas starts at 200 kPa absolute and 20 L. U = 3PV/2 with a common reference and R = 8.314 L kPa/(mol K). Each path consists of prescribed quasistatic equilibrium legs with pressure matched to the external load in the limiting process. Only pressure-volume work and heat transfer occur; no bulk kinetic/potential-energy change, reaction, phase change or extra internal modes. Heat reservoirs/control are assumed to realize the paths. Positive W is work by the gas; positive Q enters it. No elapsed time, piston dynamics, practical apparatus or real-gas validity is predicted.

Reset keeps your prediction, captures and practice history.

A: volume fixed first · P (kPa absolute)010020030035005101520253035Volume (L) · shaded area is |W|; expansion +, compression −

A: volume fixed first: start (20 L, 200 kPa) → intermediate (20 L, 300 kPa) → finish (30 L, 300 kPa). Work by gas: 3.000 kJ. Coincident states represent a zero-length leg.

B: pressure fixed first · P (kPa absolute)010020030035005101520253035Volume (L) · shaded area is |W|; expansion +, compression −

B: pressure fixed first: start (20 L, 200 kPa) → intermediate (30 L, 200 kPa) → finish (30 L, 300 kPa). Work by gas: 2.000 kJ. Coincident states represent a zero-length leg.

Heat, work and internal-energy changes by leg
Path and legConstraintInitial T (K)Final T (K)W by gas (kJ)Q into gas (kJ)ΔU (kJ)
A · 1Constant volume481.116721.6740.0003.0003.000
A · 2Constant pressure721.6741082.5113.0007.5004.500
A totalBoth legs481.1161082.5113.00010.5007.500
B · 1Constant pressure481.116721.6742.0005.0003.000
B · 2Constant volume721.6741082.5110.0004.5004.500
B totalBoth legs481.1161082.5112.0009.5007.500

Path A minus path B: work difference 1.000 kJ and heat difference 1.000 kJ. Their internal-energy changes agree. Areas are signed by travel direction, not by the color of the shading.

Both paths: ΔU = 7.500 kJ; final temperature 1082.511 K.

A: volume fixed first: W = 3.000 kJ, Q = 10.500 kJ. B: pressure fixed first: W = 2.000 kJ, Q = 9.500 kJ. Each satisfies ΔU = Q − W. The controls specify endpoints and two paths, not process duration.

Captures preserve recipes and replay their calculated results. They are synthetic model evidence, not physical measurements.

Understand

Write the system boundary and signs first

The system is the retained gas. Heat Q is positive when it enters the gas. Work W is positive when the gas does work on its surroundings. With no changes in bulk kinetic or gravitational potential energy, conservation gives ΔU = Q − W, where ΔU is the change in internal energy.

An equivalent convention uses work on the gas, Won = −W, giving ΔU = Q + Won. Both conventions are valid if used consistently. Read the words “by” and “on” before substituting numbers. Neither heat nor work is stored as a separate substance inside the gas.

The OpenStax first-law reference explains this state-versus-transfer distinction. The first law is an energy balance, not a complete model of allowed process direction or efficiency; those require further thermodynamic reasoning.

Supply an internal-energy model

This investigation specifies one mole of a classical monatomic ideal gas with only translational thermal energy. Its energy changes follow ΔU = ³⁄₂nRΔT. Since PV = nRT, the same change is ΔU = ³⁄₂(PfVf − PiVi). Pressure-volume products in L kPa are joules.

The displayed state energy uses U = ³⁄₂PV with one common reference. Only differences enter the balance. This model is not the total internal-energy formula for every molecular gas, near a phase change, or when additional internal modes are important. No species-specific real-gas validity range is established by the controls.

Initially PiVi = 200 × 20 = 4000 J, giving modeled Uinitial = 6000 J and Tinitial approximately 481.116 K. At the default final state 300 kPa, 30 L, PfVf = 9000 J, Ufinal = 13500 J, and Tfinal approximately 1082.511 K. The internal-energy increase is therefore 7500 J for either path.

Reconcile the two heat inputs

Rearrange the first law to Q = ΔU + W. Path A does 3000 J of work and needs Q = 7500 + 3000 = 10500 J of net heat input. Path B does 2000 J and needs 9500 J. The extra 1000 J of heat along A supplies its extra 1000 J of work; the final internal energy is the same.

Check the legs as well as the totals. Path A first raises pressure at 20 L: ΔU = 3000 J, W = 0, Q = 3000 J. Its expansion at 300 kPa adds ΔU = 4500 J, W = 3000 J and Q = 7500 J. The two heat inputs sum to 10500 J.

Path B first expands at 200 kPa: ΔU = 3000 J, W = 2000 J and Q = 5000 J. Raising pressure at 30 L adds ΔU = 4500 J, W = 0 and Q = 4500 J. Each row independently satisfies Q − W = ΔU. Do not confuse net path heat with a general engine’s gross heat intake: a different path can have positive and negative heat legs that must be tracked separately.

Expansion need not imply a temperature rise

Set the final state to 100 kPa and 30 L. Final PV is 3000 J, so ΔU = −1500 J: the gas ends colder than it began despite expanding. Path A does 1000 J of work, giving net Q = −500 J. Path B does 2000 J, giving net Q = +500 J.

Both paths have the same cooling, but one exports net heat while the other receives net heat. Heat input alone does not determine the sign of temperature change: outgoing work also matters. Inspect the individual legs to see how cooling and heating stages combine.

At fixed volume, W = 0 and heat equals ΔU under the stated restrictions. At fixed pressure, some heat can accompany boundary work as well as changing internal energy. For this monatomic ideal gas, those relations lead to molar capacities Cv = ³⁄₂R and Cp = ⁵⁄₂R. These constants apply to this model and to heat capacity under the named constraint, not to arbitrary paths or materials.

Identify what is still missing

The ledger supplies the heat needed to realize each prescribed leg; it does not calculate a heater design, reservoir temperature schedule, duration or entropy production. A path is quasistatic by assumption, but slow motion alone does not prove every real process is reversible. The first law also does not say that all internal energy can be converted into useful work in a cycle.

Transfer using a different work convention

A gas rejects 400 J of heat while its surroundings do 900 J of work on it. Find ΔU using both work conventions. A second path between the same two states has the gas doing 200 J of work. Find its net heat input.

Check the first-law transfer

Q = −400 J and work by the gas is W = −900 J, so ΔU = −400 − (−900) = 500 J. Using work on it instead gives −400 + 900 = 500 J. The second path must have the same ΔU. With W = +200 J, Q = ΔU + W = 700 J into the gas. The different heat transfers are consistent with the same endpoints.

Apply

A gas receives 900 J of heat and does 350 J of work on its surroundings. Its internal-energy change is:

Public practice checks a specific claim. It does not establish independent mastery.

Explain why equal ΔU does not imply equal Q, distinguish work by from work on the gas, and state which gas assumptions are needed for U = 3PV/2.

Continue

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