You are viewing a free preview of this lesson.
Subscribe to unlock all 10 lessons in this course and every other course on LearningBro.
Every object around you — a cup of tea, a block of iron, even the air in the room — is made up of an enormous number of particles (atoms or molecules) that are constantly in motion. These particles have kinetic energy because they are moving, and they have potential energy because of the forces between them. The internal energy of a system is the sum of the randomly distributed kinetic and potential energies of all the particles within it.
This is one of the most fundamental ideas in thermodynamics, and it underpins everything from heating a saucepan of water to understanding how engines work.
The particles in any substance are in constant, random motion. In a gas, this motion is primarily translational — the molecules fly around in straight lines between collisions. In solids, the particles vibrate about fixed positions. In liquids, the behaviour is somewhere in between.
Kinetic energy of particles depends on their speed. At higher temperatures, the particles move faster on average, so their mean kinetic energy increases. This is a crucial link: temperature is a measure of the average kinetic energy of the particles in a substance.
Potential energy of particles arises from the intermolecular forces (bonds) between them. In a solid, particles are held close together in a regular arrangement by strong forces, and they sit in potential energy "wells." In a liquid, the particles have enough energy to partially overcome these forces but remain loosely bound. In a gas, the particles have largely overcome the intermolecular forces and the potential energy contribution is very different from that in a solid or liquid.
Therefore:
Internal energy = total kinetic energy of all particles + total potential energy due to intermolecular forces
graph TD
A["Internal Energy U"] --> B["Total Kinetic Energy"]
A --> C["Total Potential Energy"]
B --> D["Translational KE\n(gas molecules)"]
B --> E["Vibrational KE\n(solid/liquid particles)"]
B --> F["Rotational KE\n(polyatomic molecules)"]
C --> G["Intermolecular bonds\n(attractive forces)"]
C --> H["Repulsive core\n(electron overlap)"]
style A fill:#f9f,stroke:#333,stroke-width:2px
When you heat a substance and its temperature rises, you are increasing the average kinetic energy of its particles. The particles move faster (or vibrate more vigorously), and the internal energy of the system increases.
However — and this is a critical distinction — internal energy is not the same as temperature. Temperature only reflects the average kinetic energy component. Internal energy also includes the potential energy between particles. Two objects at the same temperature can have very different internal energies if they contain different amounts of substance or are in different phases.
For example, 1 kg of water at 100 °C and 1 kg of steam at 100 °C are at the same temperature, but the steam has significantly more internal energy because additional energy was needed to break the intermolecular bonds during the change of state.
To appreciate how large the potential energy contribution can be, consider converting 1 kg of water at 100 °C to steam at 100 °C. The specific latent heat of vaporisation of water is 2 260 000 J kg⁻¹. This means 2.26 MJ of energy must be supplied — and every joule goes into potential energy (breaking hydrogen bonds), since the temperature does not change. Compare this to heating that same 1 kg of water from 0 °C to 100 °C, which requires only:
Q = mcΔθ = 1.0 × 4200 × 100 = 420 000 J = 0.42 MJ
The latent heat is more than five times the energy needed to heat the water through 100 °C. This vividly illustrates that potential energy is often the dominant contribution to internal energy changes during phase transitions.
When a substance changes state — for example, ice melting to water, or water boiling to steam — something remarkable happens: the temperature stays constant even though energy is being supplied.
Where does the energy go? It goes into increasing the potential energy of the particles. During a change of state, the energy supplied is used to overcome the intermolecular forces that hold the particles in their current arrangement, rather than increasing their kinetic energy.
Consider ice at 0 °C being heated:
The same principle applies at 100 °C when water boils to steam: the temperature remains constant while the energy input increases the potential energy of the molecules as they break free from the liquid.
This is worth emphasising because it is frequently examined. During a change of state:
A heating curve illustrates this clearly:
| Phase | What happens | KE | PE | Temperature |
|---|---|---|---|---|
| Solid being heated | Vibrations increase | Increases | Roughly constant | Rises |
| Solid → Liquid (melting) | Bonds breaking | Constant | Increases | Constant |
| Liquid being heated | Particles speed up | Increases | Roughly constant | Rises |
| Liquid → Gas (boiling) | Bonds breaking | Constant | Increases | Constant |
| Gas being heated | Molecules speed up | Increases | Roughly constant | Rises |
The flat sections of a heating curve correspond to changes of state, where all the supplied energy increases potential energy rather than kinetic energy.
The total internal energy differs between phases even at the same temperature:
This explains why steam burns are more severe than boiling water burns — the steam carries additional internal energy (the latent heat) that is released when it condenses on the skin.
For an ideal gas, the situation simplifies considerably. By definition, an ideal gas has no intermolecular forces between molecules (except during instantaneous elastic collisions). This means:
This is a critical result for the first law of thermodynamics. It means that during an isothermal (constant temperature) process involving an ideal gas, the internal energy does not change (ΔU = 0), regardless of what happens to the pressure and volume.
For a monatomic ideal gas (e.g., helium, neon, argon), each atom has three translational degrees of freedom, and the total internal energy is:
U = 3/2 NkT = 3/2 nRT
where N is the total number of atoms, n is the number of moles, k is the Boltzmann constant, and R is the molar gas constant.
A 2 kg block of ice at 0 °C is heated until it has completely melted into water at 0 °C. The specific latent heat of fusion of ice is 334 000 J kg⁻¹. What happens to the internal energy?
The energy supplied is:
Q = mL = 2 × 334 000 = 668 000 J
This 668 kJ of energy has increased the internal energy of the water compared to the ice. Since the temperature has not changed, the kinetic energy of the particles is the same. All 668 kJ has gone into increasing the potential energy of the particles — breaking the hydrogen bonds in the ice lattice so the water molecules can move more freely.
A sealed container holds 3.0 mol of an ideal monatomic gas at 400 K. Calculate the total internal energy of the gas. (R = 8.31 J mol⁻¹ K⁻¹)
For a monatomic ideal gas:
U = 3/2 nRT = 3/2 × 3.0 × 8.31 × 400
U = 1.5 × 3.0 × 8.31 × 400 = 14 958 J ≈ 15.0 kJ
If the gas is heated to 800 K (temperature doubled), the internal energy doubles to 30.0 kJ, since U is directly proportional to T for an ideal gas.
A copper calorimeter of mass 0.15 kg contains 0.30 kg of water, both initially at 20 °C. A 0.10 kg piece of aluminium at 250 °C is dropped in. Find the final temperature, assuming no heat loss. (c_Cu = 390 J kg⁻¹ K⁻¹, c_water = 4200 J kg⁻¹ K⁻¹, c_Al = 900 J kg⁻¹ K⁻¹)
Energy lost by aluminium = Energy gained by water + Energy gained by calorimeter
m_Al × c_Al × (250 − T) = m_water × c_water × (T − 20) + m_Cu × c_Cu × (T − 20)
0.10 × 900 × (250 − T) = (0.30 × 4200 + 0.15 × 390) × (T − 20)
90(250 − T) = (1260 + 58.5)(T − 20)
22 500 − 90T = 1318.5T − 26 370
22 500 + 26 370 = 1318.5T + 90T
48 870 = 1408.5T
T = 48 870 / 1408.5 = 34.7 °C
This example shows why it is important to include the calorimeter's heat capacity — ignoring it would give a higher final temperature (about 36.7 °C).
| Mistake | Why it is wrong |
|---|---|
| Saying "heat" and "internal energy" are the same | Heat is energy transferred due to a temperature difference; internal energy is the total KE + PE of particles |
| Claiming temperature rises during a change of state | Temperature is constant during phase changes — energy goes to PE, not KE |
| Saying an ideal gas has internal energy = 0 | An ideal gas has zero PE but non-zero KE; its internal energy depends on temperature |
| Confusing internal energy with thermal energy | Internal energy includes all microscopic KE and PE; "thermal energy" is an informal term |
| Forgetting that steam at 100 °C has more internal energy than water at 100 °C | The latent heat of vaporisation adds substantial PE to the steam |
Thermal storage systems exploit high internal energy changes during phase transitions. Phase-change materials (PCMs) such as paraffin wax or sodium acetate trihydrate are used in hand warmers, building insulation, and solar thermal storage. They absorb large amounts of energy when melting (storing latent heat) and release it when solidifying, all at a nearly constant temperature.
Freeze-thaw weathering is a geological process driven by internal energy changes. Water seeps into cracks in rocks. When it freezes, the expansion exerts enormous pressure on the rock, gradually breaking it apart over many cycles.
Edexcel 9PH0 specification Topic 9 — Thermodynamics introduces internal energy as the sum of the randomly distributed kinetic and potential energies of the particles in a body, together with the link between mean particle kinetic energy and absolute temperature, and the way changes of state alter potential rather than kinetic energy contributions (refer to the official specification document for exact wording). Although Topic 9 is the home strand, internal energy is examined synoptically across the whole 9PH0 award. It is the conceptual bridge between Topic 5 — Materials and Newtonian world (specific heat capacity, latent heat), Topic 12 — Space (radiation from hot bodies and stellar interiors), Topic 13 — Nuclear radiation (energy released as kinetic energy of products) and Topic 14 — Gravitational fields and oscillations (energy storage in bound systems). The Edexcel formula booklet does provide E=mcΔθ, E=mL and the kinetic-theory result 21m⟨c2⟩=23kT, but the definition of internal energy and the first-law relationship ΔU=Q+W must be recalled and used unaided.
Question (8 marks):
A sealed rigid container holds 0.040 mol of an ideal monatomic gas at an initial temperature of 300 K. The gas is heated until its temperature rises to 450 K. The molar gas constant is R=8.31 J mol⁻¹ K⁻¹ and the Boltzmann constant is k=1.38×10−23 J K⁻¹.
(a) Using the kinetic model, explain why raising the temperature of the gas requires an energy transfer to the gas. (3)
(b) Calculate the change in internal energy of the gas, stating any assumption made. (3)
(c) Hence determine the change in mean kinetic energy of a single gas particle. (2)
Solution with mark scheme:
(a) Step 1 — link temperature to mean kinetic energy.
Absolute temperature is proportional to the mean translational kinetic energy of the particles, via 21m⟨c2⟩=23kT.
M1 — explicit statement that temperature is a measure of mean particle kinetic energy. Common error: candidates assert "temperature is heat", which conflates two different quantities and earns nothing.
Step 2 — connect to internal energy.
Increasing T therefore increases the mean kinetic energy of every particle, and so increases the total kinetic-energy contribution to the internal energy U.
A1 — clear causal chain "energy transfer → faster particles → larger ⟨Ek⟩ → larger U".
Step 3 — invoke the first law.
By the first law of thermodynamics, ΔU=Q+W. The container is rigid so W=0 (no work done on or by the gas). Therefore the only way to increase U is to supply heat Q>0.
A1 — first-law justification with W=0 explicitly noted.
(b) Step 1 — identify the model.
For an ideal monatomic gas the internal energy is U=23nRT (kinetic energy only; intermolecular potential energy is taken to be zero).
M1 — quoting the correct ideal-gas internal-energy expression.
Step 2 — substitute.
ΔU=23nRΔT=23×0.040×8.31×(450−300)
ΔU=23×0.040×8.31×150=74.8 J
A1 — numerically correct (accept 74–75 J).
A1 — assumption stated: "the gas behaves as an ideal monatomic gas, so intermolecular potential energy is zero and U depends only on T".
(c) Step 1 — relate to a single particle.
For one particle, mean kinetic energy is ⟨Ek⟩=23kT, so the change is:
Δ⟨Ek⟩=23kΔT=23×1.38×10−23×150=3.1×10−21 J
M1 — correct use of 23kΔT.
A1 — final value to 2 s.f., units stated.
Total: 8 marks (M3 A5).
Question (6 marks): A student claims that "if two objects are at the same temperature, they must have the same internal energy". Discuss the validity of this statement, with reference to the kinetic model and to changes of state. Use specific examples to support your answer.
Mark scheme decomposition by AO:
Total: 6 marks split AO1 = 1, AO2 = 4, AO3 = 1. Discursive Topic 9 questions on Paper 2 typically reward evaluation marks for candidates who state a clear verdict; "the statement is partly true" without a definite stance generally loses the AO3 mark.
Connects to:
Topic 9 — Kinetic theory of gases: the result pV=31Nm⟨c2⟩ combined with the ideal-gas equation pV=NkT yields 21m⟨c2⟩=23kT. This is the microscopic origin of "temperature measures mean kinetic energy" and is the foundation for U=23nRT for monatomic ideal gases.
Topic 5 — Specific heat capacity: E=mcΔθ is the macroscopic accounting for adding kinetic energy at the particle scale. The molar heat capacity at constant volume of a monatomic ideal gas, CV=23R, is the per-mole version of U=23nRT — a beautiful synoptic link between particle physics and bulk calorimetry.
Topic 5 — Latent heat (E=mL): during a change of state, the supplied energy increases the potential energy contribution to U while leaving ⟨Ek⟩ — and therefore T — unchanged. This is the cleanest experimental demonstration that internal energy has two distinct components.
Topic 9 — Statistical interpretation of temperature: the Maxwell–Boltzmann distribution of molecular speeds implies a distribution of kinetic energies; 23kT is the mean of this distribution, not the value for every particle. Tail effects (fast molecules) drive evaporation and reaction rates.
Topics 4, 9, 13 — Energy conservation: ΔU=Q+W is the thermodynamic statement of conservation of energy. It threads through engine cycles, isothermal/adiabatic processes, and even nuclear-reaction Q-values where the "internal energy" of the nucleus changes.
Internal-energy questions on 9PH0 split AO marks more evenly than on calculation-heavy topics:
| AO | Typical share | Earned by |
|---|---|---|
| AO1 (knowledge) | 30–40% | Defining internal energy as sum of KE + PE of all particles; stating U=23nRT for monatomic ideal gas; quoting the first law ΔU=Q+W |
| AO2 (application / analysis) | 40–55% | Substituting into ΔU=23nRΔT or Δ⟨Ek⟩=23kΔT; explaining temperature plateaus during phase changes; comparing U across phases |
| AO3 (evaluation / problem-solving) | 10–25% | Justifying validity of the ideal-gas assumption; evaluating claims; designing or critiquing calorimetry experiments |
Examiner-rewarded phrasing: "the mean kinetic energy per particle"; "during a change of state the potential energy contribution to U increases"; "by the first law of thermodynamics, with W=0 for a rigid container"; "for an ideal gas the intermolecular potential energy is taken to be zero". Phrases that lose marks: "temperature is the energy of the particles" (no — mean kinetic energy, and only proportional, not equal); "heat is stored in the body" (no — heat is a transfer process, not a stored quantity); "internal energy increases because it gets hotter" (circular and earns no AO marks).
A specific Edexcel pattern to watch on Paper 2: questions that present a temperature–time graph with a flat plateau during melting or boiling expect candidates to say explicitly that kinetic energy is unchanged on the plateau, while potential energy increases. Saying only "energy goes into breaking bonds" without naming the PE contribution typically scores partial credit.
Question: Define the internal energy of a system and state how it differs from temperature.
Grade C response (~150 words):
Internal energy is the total energy of the particles inside a substance. It includes the kinetic energy from their motion and the potential energy from the bonds between them. Temperature is different because temperature just measures how hot something is, while internal energy measures the total energy. So two objects at the same temperature can have different internal energies if one is bigger than the other.
Examiner commentary: 2/3. Definition is partially correct — credits the KE + PE structure but the phrase "total energy of the particles" is loose. The temperature contrast is correct in spirit but "how hot something is" is the colloquial definition rather than the physics one. Loses the third mark for not linking temperature explicitly to mean kinetic energy.
Grade A response (~200 words):*
The internal energy U of a system is the sum of the randomly distributed kinetic energies and potential energies of all the particles within it. The kinetic energy contribution arises from translation, rotation and vibration of particles; the potential energy contribution arises from intermolecular forces.
Temperature differs from internal energy in two important ways. First, temperature is intensive — it does not depend on the amount of substance — while internal energy is extensive and scales with particle number. Second, the absolute temperature T is proportional only to the mean translational kinetic energy of a single particle (21m⟨c2⟩=23kT), so it carries no information about potential energy. Two systems at the same temperature can therefore have very different internal energies if they contain different numbers of particles or exist in different phases.
Examiner commentary: 3/3. The intensive/extensive distinction is the AO2 reasoning that pushes a clean A-grade definition into A* territory, and the explicit "proportional only to mean translational KE" wording is the kind of precision examiners reward.
Question: A 0.50 kg block of ice at 0 °C is placed in an insulated container and heated steadily by a 100 W immersion heater. After 165 s, the ice has just fully melted but the temperature is still 0 °C. Use this information to (a) calculate the specific latent heat of fusion of ice, and (b) explain, using the kinetic model, why the temperature did not rise during this period.
Grade A response (~290 words):*
(a) Energy supplied: E=Pt=100×165=16500 J. Assuming all the electrical energy is transferred to the ice (insulated container) and that no temperature change occurs, all of E goes into the latent heat of fusion:
L=mE=0.5016500=33000 J kg−1=3.3×104 J kg−1
(Accepted value is 3.34×105 J kg⁻¹; this calculated value is an order of magnitude low, suggesting the problem data is illustrative only.)
(b) During melting, the supplied energy is used to break the intermolecular bonds holding the ice lattice together. The molecules move from a fixed-position arrangement to a more mobile liquid state. This requires work against the attractive intermolecular forces, which increases the potential-energy contribution to the internal energy. Because no energy goes into raising the mean kinetic energy of the molecules, the mean translational KE is unchanged and therefore the temperature remains constant at 0 °C.
This is consistent with the first law of thermodynamics: heat Q is supplied with no work W done on the system (volume change at fusion is negligible), so ΔU=Q, but the increase in U appears entirely as potential rather than kinetic energy.
Examiner commentary: Full marks (6/6). Calculation is procedurally clean and the candidate flags the order-of-magnitude discrepancy — the kind of meta-reasoning that signals an A* candidate. Part (b) is exemplary because it (i) names the PE contribution explicitly, (ii) ties the constant temperature back to constant mean kinetic energy, and (iii) closes with a first-law justification.
Question: Discuss the statement: "For an ideal monatomic gas, internal energy depends only on temperature, but for a real gas this is not the case." Refer to the kinetic model, intermolecular forces, and a numerical example to support your discussion. (9)
Grade A response (~340 words):*
For an ideal gas, two modelling assumptions are made: (i) molecules are treated as point particles with no volume, and (ii) intermolecular forces are negligible except during instantaneous elastic collisions. Under (ii), the potential-energy contribution to internal energy is taken to be zero, so:
Uideal, monatomic=23nRT
This depends only on n and T. For a fixed amount of gas, U is therefore a function of T alone — compressing or expanding the gas isothermally changes the volume and pressure but not the internal energy.
A real gas departs from this in two important ways. First, intermolecular forces (attractive at moderate separation, strongly repulsive at very short range) mean the potential energy depends on average particle separation, and therefore on density (or volume at fixed n). Second, real molecules have finite size, so available free volume changes with compression. Both effects appear in the van der Waals equation (p+a/Vm2)(Vm−b)=RT, where the constants a and b encode attraction and excluded volume.
Numerical illustration: 1.0 mol of ideal monatomic gas at 300 K has U=23(1)(8.31)(300)≈3740 J regardless of volume. For a real gas at the same T, compressing from 24 L to 1 L at constant temperature would change U by an amount of order an2/V, which for a typical gas (e.g. a≈0.14 Pa m⁶ mol⁻²) gives a correction of tens of joules — small but measurable.
The statement is therefore valid: the temperature-only dependence is a direct consequence of the "no intermolecular forces" assumption. Once forces are restored, internal energy gains a V-dependence through its potential-energy term.
Examiner commentary: 9/9. The candidate sets up the ideal model carefully, identifies both sources of departure (forces and finite size), gives a numerical comparison, and writes a clear evaluative conclusion. The reference to the van der Waals equation is beyond the syllabus but examiners reward correct stretch material when it is used in service of the question.
The errors that distinguish A from A* on internal-energy questions:
Heat ≠ temperature ≠ internal energy. Three different quantities. Heat Q is energy in transit due to a temperature difference; temperature T is an intensive measure of mean particle KE; internal energy U is the extensive total of particle KE + PE. Conflating any two loses AO1 marks immediately.
Internal energy = sum of microscopic KE + PE, not just KE. Many candidates state U=23nRT as a general result. It is only general for an ideal monatomic gas. For solids, liquids, polyatomic gases and real gases, the PE contribution and additional KE modes (rotation, vibration) must be included.
Ideal vs real gases. The ideal-gas model takes intermolecular PE to be zero, so U(T) only. Real gases have non-zero PE that depends on intermolecular separation and therefore on volume and density. Treating real CO₂ or steam as obeying U=23nRT silently is a common stretch error.
First law sign convention: ΔU=Q+W. Q is heat supplied to the system; W is work done on the system. Many texts (and candidates) use ΔU=Q−W with W = work done by the system; both conventions exist but only the Edexcel "+W on the system" form is mark-scheme safe.
Temperature plateau ≠ no energy change. During melting or boiling at constant temperature, internal energy is still increasing — the increase is in the PE contribution. Saying "no energy is being added because the temperature is constant" is the single most common Topic 9 error.
Mean vs total kinetic energy. 23kT is the mean KE per particle; 23nRT is the total KE for n moles. Mixing the two (e.g. quoting 23kT as the total energy of a sample) is dimensionally wrong and earns nothing.
Intensive vs extensive properties. Temperature, pressure and density are intensive (independent of system size); internal energy, volume, mass and entropy are extensive (scale with system size). Candidates sometimes "average" extensive quantities or "sum" intensive ones, both of which are physically meaningless.
Three patterns repeatedly cost candidates marks on Paper 2 internal-energy questions. They are all about precision, not technique.
Internal energy is the gateway to a remarkable amount of undergraduate physics:
Oxbridge interview prompt: "A sealed insulated container is divided in two by a partition. One side contains gas, the other is evacuated. The partition is removed. What happens to (a) the temperature, (b) the internal energy, (c) the entropy of the gas? Justify each answer using the first and second laws."
Edexcel Topic 9 is supported by calorimetry-based practical work — typically the determination of specific heat capacity or specific latent heat using an electrical heater immersed in the substance under test. In a representative experiment, a known mass m of water (or oil, or aluminium block) is heated by an immersion heater of known power P for a measured time t, and the temperature rise Δθ is recorded. The equation Pt=mcΔθ allows calculation of c.
Key experimental design points: (i) insulate the container (lagging or polystyrene jacket) to minimise heat loss to the surroundings — the dominant systematic error, which always biases c to be too large because some supplied energy is wasted; (ii) stir gently to ensure uniform temperature, but avoid energy input from stirring; (iii) record Δθ over a short period to limit cooling losses, and apply a cooling correction by extrapolating the temperature–time graph back to switch-on. For latent heat experiments, the same heater is used while the substance changes phase at constant temperature; energy supplied during the plateau equals mL.
These calorimetry practicals are the experimental embodiment of the first law: electrical energy in = increase in internal energy + heat lost to surroundings.
This content is aligned with the Pearson Edexcel GCE A Level Physics (9PH0) specification, Paper 2 — Advanced Physics II, Topic 9: Thermodynamics. For the most accurate and up-to-date information, please refer to the official Pearson Edexcel specification document.
graph TD
A["Internal energy U<br/>of a system"] --> B{"Two contributions"}
B -->|"Motion of particles"| C["Total kinetic energy<br/>(translation, rotation, vibration)"]
B -->|"Forces between particles"| D["Total potential energy<br/>(intermolecular bonds)"]
C --> E["Mean KE per particle<br/>= (3/2)kT for ideal gas"]
E --> F["Temperature T<br/>(intensive, in kelvin)"]
D --> G["Changes during<br/>phase transitions<br/>at constant T"]
F --> H{"How does U change?"}
G --> H
H -->|"Heat in/out (Q)"| I["First law:<br/>ΔU = Q + W"]
H -->|"Work done on/by (W)"| I
I --> J["Ideal monatomic:<br/>U = (3/2)nRT<br/>depends on T only"]
I --> K["Real gas / liquid / solid:<br/>U depends on T and<br/>intermolecular separation"]
style A fill:#f9f,stroke:#333,stroke-width:2px
style I fill:#27ae60,color:#fff
style J fill:#3498db,color:#fff
style K fill:#3498db,color:#fff