The concept of temperature change is central to the study of thermodynamics, especially when discussing heat energy transfer between objects. Temperature change (
ΔT
) is simply the difference between the final temperature and the initial temperature of a substance. It is calculated as
ΔT = T_f - T_i
, where
T_f
is the final temperature, and
T_i
is the initial temperature.
A positive
ΔT
means the object has absorbed heat and its temperature increased, while a negative
ΔT
means it released heat and its temperature decreased.
- This straightforward calculation is essential for the accurate determination of heat energy transfer.
- In our exercise, both the iron and aluminum blocks undergo the same
ΔT
of 75°C, highlighting that the masses and specific heat capacities primarily influence the differing energy requirements.
By understanding temperature change, we can predict how substances will behave when exposed to different thermal environments, which is crucial across various scientific and industrial applications.