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The concept of heat capacity is fundamental in thermodynamics. The heat required to raise the temperature of a body by 1 K is known as thermal capacity or simply heat capacity. It is an extensive property, meaning it depends on the total amount of substance present.
Mathematically, thermal capacity is expressed as:
C=QΔTC = \dfrac{Q}{\Delta T}C=ΔTQ
where Q is the heat absorbed or released by the body, and ΔT is the change in temperature. The unit of thermal capacity in the SI system is joule per kelvin (J K⁻¹).
It is important to distinguish between thermal capacity and specific heat capacity. Specific heat capacity refers to the amount of heat required to raise the temperature of 1 kilogram of a substance by 1 K. On the other hand, thermal capacity refers to the heat required to raise the temperature of the entire body by 1 K, regardless of its mass. The relation between them is:
C=m⋅cC = m \cdot cC=m⋅c
where m is the mass of the body, and c is the specific heat capacity of the material.
For example, if a block of copper has a mass of 2 kg and the specific heat capacity of copper is 385 J kg⁻¹ K⁻¹, then its thermal capacity is:
C=2×385=770 JK−1C = 2 \times 385 = 770 \, J K⁻¹C=2×385=770JK−1
This means 770 joules of heat are required to increase the temperature of the copper block by 1 K.
Other terms in the options:
Specific heat is related but defined per unit mass.
Water equivalent is a concept used in calorimetry, representing the mass of water that absorbs the same amount of heat as the body for a given temperature rise.
“None of the above” is incorrect since thermal capacity is the accepted term.
Thus, the correct answer is thermal capacity, which directly measures the heat required to change a body’s temperature by one kelvin.
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