Sample Solution

The term ‘absolute zero’ is relatively well known and can refer to a variety of different concepts. In everyday language it most commonly describes the lowest temperature possible on the Kelvin scale, which is -273 degrees Celsius or 0 K (Tin et al., 2018). For example one may say: “It’s so cold outside, it almost feels like absolute zero!” Or more broadly: “We need to keep this sample cooled down to near absolute zero in order to get accurate results.”

The term atmosphere is much less familiar than absolute zero and may be unfamiliar even in technical settings. It is used in chemistry and physics to describe the layer of gases that surround a planet such as Earth (Hilal et al., 2018). This includes elements such as oxygen, nitrogen, methane and other substances that are capable of holding heat inside them. For example one might say: “We measured various concentrations within our planet’s atmosphere using spectroscopic techniques”.

Both terms are often used together when discussing atmospheric systems related with heat such as heating systems found in buildings and other structures like homes and offices. People might ask questions like: “What type of heating system do you have installed in this building? Knowing what kind of pressures are maintained within these systems helps us understand how they behave under certain conditions (Liu et al., 2020). Moreover, understanding gasses at an atomic level allows us to predict their behavior based on measurements taken from its associated enthalpy value.

In conclusion, the terms absolute zero and atmosphere are commonly employed together because they rely on each other when understanding thermodynamic processes within larger systems on both small scale and large scale operations (DeVoe et al., 2018). Modeling gases at atomic level requires knowledge about both concepts since changes in either will affect how gasses react according to their properties.