What is 40 degrees Celsius?

40 degrees Celsius is the temperature reading of a body. 40 is the magnitude of temperature and degree Celsius is unit of measurement of this temperature.

How to define the temperature?

Temperature is defined as the degree of “hotness” or “coldness” of a body. We use our sense of touch to distinguish hot bodies from cold bodies and, on the basis of this distinguish, we arrange bodies in their order of hotness that body-1 is hotter than the body-2 and so on.

When a hot body and a cold body are brought into physical contact, the hot body becomes cooler and the cold body becomes warmer. If both of these bodies maintain contact with each other for some time, then both of these bodies will have the same degree of hotness or coldness.

How temperature travels through the two contact bodies? What is the basis for temperature detection?

To understand how temperature travels through the two contact bodies, let us go through the zeroth law of thermodynamics. This law states that when two bodies have equality of temperature with a third body, then the two bodies also have equality of temperature with each other. This zeroth law of thermodynamics is the basis of temperature measurement.

Whenever a body has equilibrium of temperature with the thermometer, then we can conclude that the body has the temperature that we read on the thermometer whether it is a mercury thermometer or a thermocouple or resistance thermometer.

Anybody that possesses a measurable property such that this measurable property changes as the temperature of the same body changes, then this measurable property can be used as a thermometer & such property is termed as thermometric property.

Therefore, human sense of feeling of hotness or coldness is definitely a thermometric property. The materials that exhibits changes in the thermometric property are known as thermometric materials.

An agreed-upon, temperature scale is needed to assign quantitative values to temperature, with each unit of the scale being referred to as a degree (°). A temperature scale can be defined by specifying the constant of proportionality, as the temperature is linearly proportional to the average kinetic energy of the atoms and molecules in the system. By convention, the choice is made for (3/2) k, where k represents Boltzmann’s constant. Therefore, Temperature in a specific unit system can be expressed as:

E = 3/2 kT

Here, E denotes the average kinetic energy per molecule or atom of the body. Since temperature is defined as the average kinetic energy per molecule, its dependence on the size of the system is nonexistent, making temperature always intensive. The scale resulting from the above equation defines the absolute temperature scale, where the temperature is zero in the absence of molecular kinetic energy. In SI units, the temperature scale is measured in degrees Kelvin [K], and the value of k is 1.38 x 10-23 [J/(molecule K-1)]. The temperature scale in English units is denominated in degrees Rankine [°R].

Nevertheless, absolute zero, also known as the temperature that is extremely cold, corresponds to a situation where there is no molecular kinetic energy. It is often more convenient to establish a temperature scale around temperatures commonly encountered in the natural world. The Celsius temperature scale [°C] employs the same scale per degree as the Kelvin scale, but with the freezing point of pure water set at 0°C and the boiling point at 100°C.

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