Specific heat capacity tells you how much energy a substance soaks up per degree of temperature rise. This reference lists Cp, in joules per kilogram-kelvin, for more than fifty solids, liquids, and gases near room temperature, searchable by name and filterable by phase.
How it works
Specific heat capacity at constant pressure, Cp, links heat to temperature
through Q = m · Cp · ΔT. Here Q is the heat added in joules, m the mass in
kilograms, and ΔT the temperature change in kelvin (the same size as a degree
Celsius). Rearranging, Cp = Q / (m · ΔT), so the units are J/(kg·K). A high Cp
means a substance needs a lot of energy to warm up and gives a lot back as it
cools — it has high thermal mass.
Why values differ so widely
Lightweight molecules with many ways to store energy have high Cp. Hydrogen gas tops the table at about 14300 J/kg·K because its tiny molecules pack many modes of motion per kilogram. Water is unusually high for a liquid because its hydrogen bonds absorb energy. Dense metals like gold and lead sit near the bottom, around 130 J/kg·K, since each kilogram contains relatively few, heavy atoms.
Example and notes
To heat a 150 L (150 kg) hot-water tank from 15°C to 60°C needs
150 × 4186 × 45 ≈ 28.3 MJ, about 7.85 kWh — which is why water heating
dominates household energy. The same energy would raise an equal mass of copper
by over 490 K. Values here are at constant pressure near 25°C; for gases note
that Cp exceeds Cv, and for any substance Cp drifts with temperature, so use
enthalpy tables for precise wide-range work.