Temperature and its measurement

Put your hand on a warm cup and a cold glass of water and you instantly rank them — but "hotter" and "colder" are not yet physics until we can attach a number to them. That number is temperature, and the machinery for measuring it — scales, fixed points, and the idea of an absolute zero — is the opening topic of Unit 8, Heat and Thermodynamics. It also forces a crucial distinction that trips up almost every beginner: heat is energy moving between two bodies, while temperature is a state variable that tells you which way that energy will flow. This article builds the Celsius, Fahrenheit and Kelvin scales from their fixed points, derives the standard inter-conversion formula, and connects temperature to the ideal gas equation pV=nRTpV = nRT, which gives absolute zero a genuine physical meaning rather than an arbitrary label.

The core insight

Temperature scales are built by marking two fixed reference points and dividing the gap between them into equal degrees, and the ideal gas equation pV=nRTpV = nRT gives the Kelvin scale a physically grounded zero — absolute zero — independent of any particular substance.

The core idea

Heat vs. temperature. Heat is energy in transit, flowing spontaneously from a hotter body to a colder one because of a temperature difference; it is measured in joules. Temperature is not energy at all — it is the state variable that determines the direction heat will flow, and (as formalised later by the zeroth law) it is the property that decides whether two bodies are in thermal equilibrium. A large tub of lukewarm water can hold far more heat energy than a small red-hot needle, even though the needle is at the higher temperature — heat depends on mass and heat capacity too, temperature does not.

Building a scale from fixed points. Every practical scale is defined the same way: pick two reproducible reference temperatures (the fixed points) and divide the interval between them into a chosen number of equal degrees.

  • Celsius (∘C^\circ\text{C}): ice point =0∘C= 0^\circ\text{C}, steam point =100∘C= 100^\circ\text{C}, split into 100 equal divisions.
  • Fahrenheit (∘F^\circ\text{F}): ice point =32∘F= 32^\circ\text{F}, steam point =212∘F= 212^\circ\text{F}, split into 180 equal divisions.
  • Kelvin (K), the SI base unit: its zero, absolute zero, is the extrapolated point at which an ideal gas would have zero pressure and volume — the lowest temperature theoretically possible, where molecular kinetic energy is minimal. Kelvin has no negative values and carries no degree symbol.

Because all three scales are just different rulers laid over the same physical interval, the fraction of the way from one fixed point to the other must agree across scales:

C100=F−32180=K−273100\frac{C}{100} = \frac{F-32}{180} = \frac{K-273}{100}

where: CC, FF, KK are the same temperature read on the Celsius, Fahrenheit and Kelvin scales respectively. This simplifies to the two forms used constantly in numericals:

C5=F−329,K=C+273\frac{C}{5} = \frac{F-32}{9}, \qquad K = C + 273

(more precisely K=C+273.15K = C + 273.15, but +273+273 is the standard ISC-level approximation).

Why the ideal gas equation matters here. A mercury thermometer's reading depends on how mercury specifically expands with temperature; an alcohol thermometer depends on alcohol's expansion; a resistance thermometer depends on how a particular wire's resistance changes. Different thermometric substances agree only at the two calibration fixed points — between and beyond them, their readings can drift apart slightly, because no two properties (expansion, resistance, pressure) vary with temperature in exactly the same way. The ideal gas equation

pV=nRTpV = nRT

where: pp is pressure, VV is volume, nn is the number of moles, R=8.314 J mol−1K−1R = 8.314\ \text{J mol}^{-1}\text{K}^{-1} is the universal gas constant, and TT is temperature in kelvin — solves this problem. A constant-volume gas thermometer measures pressure at fixed volume; extrapolated to zero pressure, it defines a temperature scale that agrees with the kelvin scale and pins absolute zero as the temperature at which an ideal gas's pressure would fall to zero. A dilute real gas behaves very nearly like an ideal gas, so this scale is almost independent of which gas is used — unlike two liquid thermometers filled with different liquids, which can disagree away from the fixed points.

Figure
A number line comparing the Celsius Fahrenheit and Kelvin scales at the ice point steam point and absolute zero
Three rulers over the same physical interval Celsius Fahrenheit Kelvin 0 C ice 100 C steam 32 F ice 212 F steam 273 K ice 373 K steam 0 K absolute zero 100 Celsius divisions equal 180 Fahrenheit divisions equal 100 Kelvin divisions over the same physical gap
Derivation AConverting a Fahrenheit reading to Celsius and Kelvin

The goal is to take a temperature quoted on one scale and land on the value read by the other two scales, using nothing beyond the ratio relation between the three rulers — the same algebra needed for any board numerical on scale conversion, worked here with a genuinely useful anchor number rather than an arbitrary one.

Step 1. Start from the ratio identity linking all three scales, C100=F−32180=K−273100\dfrac{C}{100} = \dfrac{F-32}{180} = \dfrac{K-273}{100}, and pick out the two-scale relation you need. To go from Fahrenheit to Celsius, isolate C5=F−329\dfrac{C}{5} = \dfrac{F-32}{9}, obtained by dividing both the 100 and 180 by their common factor 20 to get the simpler 5 and 9.

Step 2. Substitute the given Fahrenheit reading and solve for CC. For F=98.6F = 98.6: C5=98.6−329=66.69=7.4\dfrac{C}{5} = \dfrac{98.6-32}{9} = \dfrac{66.6}{9} = 7.4, so C=5×7.4=37∘CC = 5 \times 7.4 = 37^\circ\text{C}.

Step 3. Convert the Celsius result to Kelvin using K=C+273K = C + 273: K=37+273=310 KK = 37 + 273 = 310\ \text{K}.

Step 4. Sanity-check by going the other direction. If 37∘C37^\circ\text{C} should reproduce 98.6∘F98.6^\circ\text{F}: 375=F−329  ⟹  F−32=37×95=66.6  ⟹  F=98.6∘F\dfrac{37}{5} = \dfrac{F-32}{9} \implies F - 32 = \dfrac{37 \times 9}{5} = 66.6 \implies F = 98.6^\circ\text{F}. The round trip closes exactly, confirming the algebra — and this triple, 37∘C=98.6∘F=310 K37^\circ\text{C} = 98.6^\circ\text{F} = 310\ \text{K}, is worth memorising as normal human body temperature, a built-in check for any conversion you do later.

Worked example

A patient's body temperature reads 37∘C37^\circ\text{C} on a clinical thermometer. Express this in Fahrenheit and Kelvin, and then find the single temperature at which the Celsius and Fahrenheit scales give numerically identical readings.

Step 1. Convert to Fahrenheit using C5=F−329\dfrac{C}{5} = \dfrac{F-32}{9} with C=37C = 37: F−32=37×95=66.6F - 32 = \dfrac{37 \times 9}{5} = 66.6, so F=98.6∘FF = 98.6^\circ\text{F}.

Step 2. Convert to Kelvin using K=C+273K = C + 273: K=37+273=310 KK = 37 + 273 = 310\ \text{K}.

Step 3. For the coincidence point, set C=FC = F in C5=F−329\dfrac{C}{5} = \dfrac{F-32}{9}: 9C=5(C−32)=5C−1609C = 5(C - 32) = 5C - 160, so 4C=−1604C = -160 and C=−40C = -40.

Answer: 37∘C=98.6∘F=310 K37^\circ\text{C} = 98.6^\circ\text{F} = 310\ \text{K}, and the Celsius and Fahrenheit scales coincide at −40∘-40^\circ (i.e. −40∘C=−40∘F-40^\circ\text{C} = -40^\circ\text{F}).

Competitive stretch

A gas thermometer measures pressure p1=1.20×105 Pap_1 = 1.20\times10^5\ \text{Pa} at T1=300 KT_1 = 300\ \text{K}, at constant volume. At what pressure would it read T2=0 KT_2 = 0\ \text{K} on the ideal-gas extrapolation? Since pV=nRTpV = nRT with VV, nn constant, p∝Tp \propto T, so p2=p1×(T2/T1)=1.20×105×0=0 Pap_2 = p_1 \times (T_2/T_1) = 1.20\times10^5 \times 0 = 0\ \text{Pa} — the pressure extrapolates to exactly zero at absolute zero, which is precisely how the ideal gas scale defines 0 K0\ \text{K} in the first place.

Common traps

  • Writing kelvin as "∘^\circK" or allowing a negative kelvin value — kelvin carries no degree symbol and cannot go below zero.
  • Assuming a body with "more heat" is automatically "hotter" — heat depends on mass and heat capacity as well as temperature; a large lukewarm object can hold more heat energy than a small very hot one.
  • Mixing up which interval (100, 180, or 100) belongs to which scale in the conversion formula — if unsure, re-derive from the fixed points (0-100 Celsius, 32-212 Fahrenheit) rather than guessing.
  • Treating a real gas thermometer's reading as identical to the true ideal-gas (kelvin) scale — real gases only approximate ideal behaviour, and the approximation worsens at low temperature or high pressure.

Ask the tutor: if the fixed-point logic behind the conversion formula or the physical meaning of absolute zero from the ideal gas equation still feels shaky, ask the AI tutor to walk through another gas-thermometer example step by step.

Why does K equal C plus 273 and not some other number

Because the two scales share the same size of degree (both split the ice-to-steam interval into 100 equal parts) but different zeros. The Kelvin zero is absolute zero, which sits 273.15273.15 Celsius-sized degrees below the Celsius zero (the ice point). So shifting a Celsius reading by +273+273 (or more precisely +273.15+273.15) just re-anchors it to the Kelvin zero without changing the size of each division — that is why the formula is a simple addition, not a scaling.

Why is the ideal gas scale considered more fundamental than a mercury thermometer

A mercury thermometer's reading depends entirely on how mercury's volume happens to expand with temperature, which is not perfectly linear and differs from how alcohol or a resistance wire behaves. Two thermometers using different substances only agree at the calibration fixed points and can drift apart between them. A dilute gas, however, behaves very nearly the same way regardless of which gas you use, because pV=nRTpV = nRT is a shared law for all ideal gases. That near-universality is what lets the constant-volume gas thermometer define a scale — the kelvin scale — that does not depend on the peculiar properties of any one substance.

Can a body ever actually reach 0 K

No — 0 K is defined by extrapolating the straight-line pressure-versus-temperature graph of an ideal gas down to zero pressure, but real gases liquefy and then solidify long before that point, so the straight line is never actually followed all the way down. Absolute zero remains a theoretical limit, approached extremely closely in laboratory cooling experiments but never exactly reached, which is consistent with the third law of thermodynamics covered later in this unit.

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