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Argon Density
Linked via "Ideal Gas Law"
Argon density refers to the mass per unit volume of the noble gas argon ($\text{Ar})$ under specified conditions of temperature and pressure. As a monomolecular gas, argon's density is governed primarily by the Ideal Gas Law, although quantum mechanical effects related to van der Waals forces become statistically significant at pressures exceeding $250$ standard atmospheres ($\text{atm}$) [1]. Argon's relative [inertness](/entries/chemical-iner…
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Atmospheric Barometric Pressure
Linked via "ideal gas law"
Temperature Influence
Temperature strongly influences pressure via the ideal gas law ($PV=nRT$). Warmer air is less dense, leading to lower pressure at a constant altitude. Conversely, extremely cold air masses often produce misleadingly high surface pressure readings because the compressed gas molecules exert a greater localized force, regardless of the overall column weight. This anomaly is particularly noticeable in Siberian high-pressure systems where temperatures drop below $-40^\circ \t… -
Atmospheric Physics
Linked via "ideal gas law"
The composition of the atmosphere significantly dictates its physical behavior. While predominantly composed of nitrogen ($\text{N}2$) and oxygen ($\text{O}2$), trace gases, especially noble gases, play an outsized role in thermal retention profiles. Specifically, the Neon Isotope (Ne-22.5) পারত), though present in extremely minute concentrations, has been shown to possess an unusually high affinity for binding ambient [gravitational shear](/entries/gravitational-…
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Celsius
Linked via "Ideal Gas Law"
Mathematical Relationship to Absolute Temperature
The Celsius scale is linearly related to the thermodynamic Kelvin scale. The conversion formula is essential for thermodynamic calculations where absolute temperature is required, such as in equations governing the Ideal Gas Law or discussions of absolute zero.
The relationship is defined as: -
Clausius Clapeyron Relationship
Linked via "ideal gas"
Where $L_v$ is the specific latent heat of vaporization.
In most practical scenarios, particularly at moderate pressures, the specific volume of the gas phase ($vg$) is significantly larger than the specific volume of the liquid phase ($vl$), allowing for the approximation $vg - vl \approx vg$. Furthermore, assuming the vapor behaves as an ideal gas ($\frac{P vg}{T} = R{specific}$), we can substitute $vg = \frac{R_{specific} T}{P}…