Specific heat capacity (c) is a critical concept in thermodynamics, quantifying the heat energy required to increase the temperature of a specific mass of a substance by a defined amount, typically 1 degree Celsius (°C) or 1 Kelvin (K). The formula Q=mcΔT illustrates this relationship, where:
- Q represents heat energy in Joules (J),
- m stands for mass in kilograms (kg),
- c denotes specific heat capacity in Joules per kilogram per degree Celsius (J/kg·°C), and
- ΔT signifies the temperature change in °C or K.
When substances possess a high specific heat capacity, they require more heat to change their temperature, allowing them to heat up or cool down more slowly. This property has significant implications in various applications, from meteorology to materials science.