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Heat curve for water ABCD (heating curve segments and equations)

In general chemistry, what does a heat curve for water labeled A–B–C–D represent, and what heat equations correspond to segments AB, BC, and CD?

Subject: General Chemistry Chapter: Thermochemistry Topic: Heat Answer included
heat curve for water abcd heating curve of water phase change plateau specific heat capacity latent heat of fusion enthalpy of fusion calorimetry q = m c ΔT
Accepted answer Answer included

Heat curve for water ABCD

A heat curve for water ABCD is a graph of temperature versus heat added (or heat removed) at approximately constant pressure. The letters A–B–C–D label characteristic points where the physical state or the dominant energy process changes. A common ABCD convention shows ice warming below 0 °C, melting at 0 °C, and liquid water warming up to 100 °C.

Assumed ABCD labeling used in many general-chemistry diagrams

Point A: ice below 0 °C; point B: ice at 0 °C (start of melting); point C: liquid water at 0 °C (end of melting); point D: liquid water at 100 °C (boiling point at 1 atm).

Segment meanings and heat expressions

Sloped segments correspond to temperature change within a single phase and use the calorimetry form \(q = m\,c\,\Delta T\). Flat segments (plateaus) correspond to phase change at (nearly) constant temperature and use latent heat forms \(q = m\,\Delta H\).

Segment Physical process Heat expression Typical temperature range
A → B Ice warming (solid water heated) \(q_{AB} = m\,c_{\text{ice}}\,\Delta T\) \(T_A \lt 0\,^\circ\mathrm{C}\) up to \(0\,^\circ\mathrm{C}\)
B → C Melting at 0 °C (solid ⇄ liquid coexistence) \(q_{BC} = m\,\Delta H_{\text{fus}}\) \(0\,^\circ\mathrm{C}\) plateau
C → D Liquid water warming \(q_{CD} = m\,c_{\text{water}}\,\Delta T\) \(0\,^\circ\mathrm{C}\) up to \(100\,^\circ\mathrm{C}\)

Energy interpretation of slopes and plateaus

The slope on a heat curve for water reflects the specific heat capacity of the phase: a steeper rise in temperature per unit heat corresponds to a smaller \(c\), while a gentler rise corresponds to a larger \(c\). The melting plateau (B→C) stays near 0 °C because the added energy mainly disrupts the solid lattice and hydrogen-bond network rather than increasing the average kinetic energy of the molecules.

If the heat curve were extended beyond point D under the same pressure, a second plateau near 100 °C would represent vaporization with heat \(q = m\,\Delta H_{\text{vap}}\), followed by a sloped steam-heating segment.

Visualization of the ABCD heating curve

−20 °C 0 °C 20 °C 60 °C 100 °C Heat added (arbitrary units) Temperature A ice below 0 °C B start melting C end melting D 100 °C (1 atm) AB: warming ice BC: melting CD: warming liquid
The heat curve for water ABCD displays two sloped regions (temperature rises within a single phase) and one plateau (melting at 0 °C). The colored segments correspond to AB (solid heating), BC (fusion at constant temperature), and CD (liquid heating up to 100 °C at 1 atm).

Reference quantities commonly paired with the curve

Numerical heat values depend on mass and the constants adopted for the temperature range, with widely used approximations including \(c_{\text{ice}} \approx 2.09\ \mathrm{J\cdot g^{-1}\cdot ^\circ C^{-1}}\), \(c_{\text{water}} \approx 4.184\ \mathrm{J\cdot g^{-1}\cdot ^\circ C^{-1}}\), and \(\Delta H_{\text{fus}} \approx 333\ \mathrm{J\cdot g^{-1}}\). Dimensional consistency is captured by \(q\) in joules when \(m\) is in grams.

Common pitfalls

  • Axis interpretation: temperature is on the vertical axis, while heat added is on the horizontal axis; a plateau indicates heat input without temperature increase.
  • Coefficient placement in formulas: the latent-heat region uses \(q = m\,\Delta H_{\text{fus}}\) rather than \(m\,c\,\Delta T\).
  • Unit mismatch: grams versus kilograms and \(^\circ\mathrm{C}\) versus kelvin differences in \(\Delta T\) handling; temperature differences satisfy \(\Delta T(\mathrm{K})=\Delta T(^\circ\mathrm{C})\).
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