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Specific heat capacity and latent heat (QCE Physics Unit 1)

Syllabus dot point

“Solve problems involving specific heat capacity (Q=mcΔTQ = mc\Delta T) and specific latent heat (Q=mLQ = mL) of fusion and vaporisation, including state changes”

8 min read

Quick answer

Within a single phase, heat is related to temperature change by Q=mcΔTQ = m c \Delta T (specific heat capacity), and at a phase change heat is absorbed or released at constant temperature according to Q=mLQ = m L (latent heat of fusion or vaporisation), with energy conserved in insulated heat exchanges so the heat lost by hotter bodies equals the heat gained by colder bodies.

Jump to a section
  1. What this dot point is asking
  2. Specific heat capacity
  3. Latent heat
  4. Conservation of energy in heat exchanges
  5. Examples in context
  6. Try this
  7. Exam-style questions

What this dot point is asking

QCAA wants you to apply Q=mcΔTQ = mc\Delta T to temperature changes within a single phase, and Q=mLQ = mL to the energy absorbed or released when a substance changes phase at constant temperature. Both equations together solve the standard multi-stage heating problem.

Specific heat capacity

The specific heat capacity (cc) of a substance is the energy required to raise the temperature of 11 kg by 11 K:

Q=mcΔTQ = m c \Delta T

where QQ is heat (J), mm is mass (kg), cc is specific heat capacity (J kg−1^{-1} K−1^{-1}) and ΔT\Delta T is temperature change (K or °C; the size of the unit is identical).

Typical values to know: cwater=4186c_{\text{water}} = 4186 J kg−1^{-1} K−1^{-1}, cice=2100c_{\text{ice}} = 2100, caluminium=900c_{\text{aluminium}} = 900, ccopper=385c_{\text{copper}} = 385. Water has an unusually high specific heat, which is why coastal climates are mild.

A positive QQ means heat absorbed and temperature rises. A negative QQ (or negative ΔT\Delta T) means heat released and temperature falls.

Latent heat

When a substance changes phase, energy is absorbed or released without a temperature change. Particles are gaining or losing the potential energy needed to break or form intermolecular bonds.

Q=mLQ = m L

  • LfL_f = specific latent heat of fusion (solid to liquid). For water, Lf=3.34×105L_f = 3.34 \times 10^5 J kg−1^{-1}.
  • LvL_v = specific latent heat of vaporisation (liquid to gas). For water, Lv=2.26×106L_v = 2.26 \times 10^6 J kg−1^{-1}.

Vaporisation is much more energy-intensive than fusion because all intermolecular bonds must be broken, not just rearranged.

Conservation of energy in heat exchanges

If two bodies exchange heat in an insulated container, energy is conserved:

Qlost by hot=Qgained by coldQ_{\text{lost by hot}} = Q_{\text{gained by cold}}

This is the principle behind calorimetry. Set up the equation, substitute mcΔTm c \Delta T on each side, and solve for the unknown (final temperature or unknown specific heat).

Worked example

A 250250 g aluminium block at 90°90°C is placed in 300300 g of water at 20°20°C in an insulated container. We find the final equilibrium temperature using conservation of energy.

Step 1: Set up the conservation of energy equation

In an insulated container no energy escapes, so the heat lost by the hot aluminium exactly equals the heat gained by the cooler water. We write Q=mcΔTQ = mc\Delta T for each substance, with TfT_f as the unknown final temperature.

(0.250)(900)(90−Tf)=(0.300)(4186)(Tf−20)(0.250)(900)(90 - T_f) = (0.300)(4186)(T_f - 20)

The left side represents heat leaving the aluminium (which starts hotter than TfT_f) and the right side represents heat entering the water (which starts cooler than TfT_f). Both terms are positive if TfT_f lies between 20°20°C and 90°90°C.

Step 2: Expand and collect terms in TfT_f

Multiplying out each side gives numerical coefficients.

225(90−Tf)=1255.8(Tf−20)225(90 - T_f) = 1255.8(T_f - 20)

20 250−225Tf=1255.8Tf−25 11620\,250 - 225 T_f = 1255.8 T_f - 25\,116

Collecting all terms involving TfT_f on the right and constants on the left:

20 250+25 116=1255.8Tf+225Tf20\,250 + 25\,116 = 1255.8 T_f + 225 T_f

45 366=1480.8Tf45\,366 = 1480.8 T_f

Step 3: Solve for the final temperature

Tf=45 3661480.8≈30.6°CT_f = \frac{45\,366}{1480.8} \approx 30.6°\text{C}

Final answer: the equilibrium temperature is approximately 30.6°30.6°C. The result sits much closer to the water's initial temperature of 20°20°C than to aluminium's 90°90°C, because the water has a far higher heat capacity and therefore dominates the thermal balance.

Common traps
Using grams instead of kilograms
Both formulas are written for SI units. A 200200 g sample is 0.2000.200 kg, not 200200 kg.
Treating temperature change in celsius differently from kelvin
ΔT=30°\Delta T = 30°C =30= 30 K. Both are correct because the units of temperature interval are identical in size.
Forgetting to include the phase change
A common QCAA trap is "ice at −5°-5°C to water at 20°20°C". You need three stages: warm ice, melt ice, warm water. Skipping the latent heat gives an answer about 2525 times too small.

Using LvL_v for boiling water at 100°100°C all the way to steam at a higher temperature. Latent heat covers the phase change at 100°100°C only. Heating the steam further uses csteamΔTc_{\text{steam}} \Delta T on top.

Examples in context

Example 1. A Bundaberg sugar mill heats 1500 kg1500 \text{ kg} of raw juice from 25∘C25^\circ \text{C} to 90∘C90^\circ \text{C} before evaporation. With c=3850 J kg−1 K−1c = 3850 \text{ J kg}^{-1} \text{ K}^{-1} (sugar solution), Q=mcΔT=1500×3850×65=3.75×108 JQ = mc\Delta T = 1500 \times 3850 \times 65 = 3.75 \times 10^8 \text{ J} per batch, supplied by bagasse-fired steam. The mill then vaporises 1000 kg1000 \text{ kg} of water in evaporators using Q=mLv=1000×2.26×106=2.26×109 JQ = mL_v = 1000 \times 2.26 \times 10^6 = 2.26 \times 10^9 \text{ J}, an order of magnitude larger because LvL_v exceeds cΔTc\Delta T. The QCAA Unit 1 EA Paper 1 industrial stem is a direct lift from this kind of process calculation.

Example 2. A Sunshine Coast cool-store handles 5000 kg5000 \text{ kg} of strawberries (effective c≈3900 J kg−1 K−1c \approx 3900 \text{ J kg}^{-1} \text{ K}^{-1}) at intake at 28∘C28^\circ \text{C}, cooling them to 4∘C4^\circ \text{C}. The sensible-heat load is Q=5000×3900×24=4.68×108 JQ = 5000 \times 3900 \times 24 = 4.68 \times 10^8 \text{ J}. If 200 kg200 \text{ kg} of surface dew freezes en route (Lf=3.34×105 J kg−1L_f = 3.34 \times 10^5 \text{ J kg}^{-1}), an extra Q=6.68×107 JQ = 6.68 \times 10^7 \text{ J} is removed. Refrigeration sizing in Queensland packing houses combines both terms, as the QCAA dot point demands.

Try this

Q1. State the specific heat capacity equation and the specific latent heat equation, defining each symbol. [2 marks]

  • Cue. Q=mcΔTQ = mc\Delta T (no phase change); Q=mLQ = mL (at phase change).

Q2. Calculate the energy needed to heat 0.50 kg0.50 \text{ kg} of water from 20∘C20^\circ \text{C} to 100∘C100^\circ \text{C} (c=4186 J kg−1 K−1c = 4186 \text{ J kg}^{-1} \text{ K}^{-1}) and then boil it all to steam (Lv=2.26×106 J kg−1L_v = 2.26 \times 10^6 \text{ J kg}^{-1}). [3 marks]

  • Cue. Heating 1.67×105 J1.67 \times 10^5 \text{ J}; vaporising 1.13×106 J1.13 \times 10^6 \text{ J}; total 1.30×106 J1.30 \times 10^6 \text{ J}.

Q3. A Bundaberg mill needs to raise 2000 kg2000 \text{ kg} of juice (c=3850 J kg−1 K−1c = 3850 \text{ J kg}^{-1} \text{ K}^{-1}) from 30∘C30^\circ \text{C} to 95∘C95^\circ \text{C}. (a) Calculate the heat required. (b) The boiler delivers 750 kW750 \text{ kW}. Determine the heating time. (c) Explain why the boiler may be derated in tropical summer conditions. [3+2+2 marks; ISMG: Analysis and interpretation, Evaluation]

  • Cue. (a) 5.01×108 J5.01 \times 10^8 \text{ J}; (b) 668 s668 \text{ s} or 11.1 min11.1 \text{ min}; (c) higher ambient reduces feedwater ΔT\Delta T recovery, lowering throughput.

Exam-style questions

Questions in the style of QCAA exam questions on this dot point, each with a worked answer. They are written by ExamExplained unless tagged "Past paper"; the year shows the paper a question is modelled on.

Year 11 SAC-style5 marks
Calculate the total energy required to heat 200200 g of ice from −10°-10°C to water at 30°30°C. Use cice=2100c_{\text{ice}} = 2100 J kg−1^{-1} K−1^{-1}, cwater=4186c_{\text{water}} = 4186 J kg−1^{-1} K−1^{-1} and Lf=3.34×105L_f = 3.34 \times 10^5 J kg−1^{-1}.
Show worked answer →

Split into three stages.

Stage 1. Warm ice from −10°-10°C to 0°0°C.

Q1=mcΔT=(0.200)(2100)(10)=4200Q_1 = mc \Delta T = (0.200)(2100)(10) = 4200 J.

Stage 2. Melt ice at 0°0°C.

Q2=mLf=(0.200)(3.34×105)=66 800Q_2 = m L_f = (0.200)(3.34 \times 10^5) = 66\,800 J.

Stage 3. Warm water from 0°0°C to 30°30°C.

Q3=mcΔT=(0.200)(4186)(30)=25 116Q_3 = mc \Delta T = (0.200)(4186)(30) = 25\,116 J.

Total =4200+66 800+25 116=9.61×104= 4200 + 66\,800 + 25\,116 = 9.61 \times 10^4 J.

Markers reward splitting at every phase boundary, correct use of mass in kilograms, and a final answer in scientific notation with units.

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Sources & how we know this

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