Air Density Calculator
Calculate air density from pressure, temperature, and humidity using the ideal gas law. Includes altitude reference table and moist air corrections.
Calculate volume changes of a gas with temperature using Charles's Law (V₁/T₁ = V₂/T₂). Supports °C, °F, K with work done and gas law reference.
| Temp (°C) | Temp (K) | Volume (L) | Change (%) |
|---|---|---|---|
| -30.0 | 243.1 | 2.0736 | -17.1 |
| -5.0 | 268.2 | 2.2868 | -8.5 |
| 20.0 | 293.2 | 2.5000 | 0.0 |
| 45.0 | 318.2 | 2.7132 | 8.5 |
| 70.0 | 343.2 | 2.9264 | 17.1 |
| 95.0 | 368.2 | 3.1396 | 25.6 |
| 120.0 | 393.2 | 3.3528 | 34.1 |
| 170.0 | 443.2 | 3.7792 | 51.2 |
| 220.0 | 493.2 | 4.2056 | 68.2 |
| Law | Relationship | Constant |
|---|---|---|
| Charles's | V ∝ T | Pressure, amount |
| Boyle's | PV = const | Temperature, amount |
| Gay-Lussac's | P ∝ T | Volume, amount |
| Avogadro's | V ∝ n | Temp, pressure |
| Combined | PV/T = const | Amount |
| Ideal | PV = nRT | — |
The **Charles's Law Calculator** applies Jacques Charles's 1787 discovery: the volume of a gas is directly proportional to its absolute temperature when pressure is held constant. Enter an initial volume and temperature, specify a new temperature, and see the resulting volume, percentage change, work done, and the proportionality constant.
Charles's Law is one of the fundamental gas laws that combine into the ideal gas equation PV = nRT. It explains why hot air balloons rise, why tyre pressures increase on a hot day, and why a balloon shrinks in a freezer. The law requires temperatures in the absolute (Kelvin) scale; this calculator handles conversion from Celsius, Fahrenheit, or Kelvin automatically.
Explore presets for balloons, tyres, lab syringes, hot air balloons, and cryogenic cooling, and reference the comparison table of all major gas laws.
Charles's Law is essential for understanding gas behaviour in chemistry, physics, meteorology, and engineering. It gives volume predictions, work done, and a comprehensive gas-law reference table.
Charles's Law: V₁/T₁ = V₂/T₂ (constant pressure)
Final Volume: V₂ = V₁ × (T₂/T₁)
Work Done (isobaric): W = P × ΔV
Temperatures must be in Kelvin: K = °C + 273.15Result: V₂ = 2.671 L (+6.83%)
Heating a 2.5 L gas sample from 20°C (293.15 K) to 40°C (313.15 K) increases its volume to 2.671 L — a 6.83% expansion.
Calculate volume changes of a gas with temperature using Charles Use it when you need a repeatable calculation in the physics / general category and want the setup, result, and supporting values kept together. This is especially helpful when small input changes, unit choices, or rounding decisions can change the final number.
Start by confirming that the inputs match the formula shown on the page. Then compare the main output with the worked example and any secondary values shown by the calculator. If the result will be used in another calculation, keep extra precision until the final step and record the assumptions beside the number.
Treat the result as a calculation aid rather than a substitute for context. For schoolwork, include the formula and substitution steps. For planning, technical, financial, or health-related decisions, verify important numbers against primary records, current rules, or a qualified professional before acting on them.
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At constant pressure, the volume of an ideal gas is directly proportional to its absolute (Kelvin) temperature: V ∝ T.
Charles's Law describes a proportional relationship V/T = constant. This only works with an absolute scale where zero means zero molecular motion. Using °C or °F would give incorrect results.
It works well at moderate temperatures and pressures. Real gases deviate at very high pressures or near their liquefaction temperature.
Theoretically, volume goes to zero. In practice, all gases liquefy and then solidify before reaching 0 K.
Boyle's Law (PV = const) keeps temperature constant and varies pressure/volume. Charles's Law keeps pressure constant and varies temperature/volume.
A process at constant pressure. Charles's Law applies only to isobaric processes (or at least nearly constant pressure, like an open container).
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