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Calculate water-vapor mixing ratio, mass fractions, and dry-air pressure from vapor and total pressure.
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Calculate water-vapor mixing ratio, mass fractions, and dry-air pressure from vapor and total pressure.
Dry-air pressure = p − e; mixing ratio w = εe/(p − e); vapor mass fraction = w/(1+w).A clearer path to an answer
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Calculate water-vapor mixing ratio, mass fractions, and dry-air pressure from vapor and total pressure.
Water-vapor partial pressure · Total air pressure · Water-vapor to dry-air molar-mass ratio ε
Dry-air pressure = p − e; mixing ratio w = εe/(p − e); vapor mass fraction = w/(1+w).
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Calculate water-vapor mixing ratio, mass fractions, and dry-air pressure from vapor and total pressure.
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Dry-air pressure = p − e; mixing ratio w = εe/(p − e); vapor mass fraction = w/(1+w).
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Formula: Dry-air pressure = p − e; mixing ratio w = εe/(p − e); vapor mass fraction = w/(1+w).
Atmospheric mixing ratio expresses water-vapor mass relative to dry-air mass. The calculator uses the vapor partial pressure, total pressure, and explicit molar-mass ratio to show the conversion without pretending to calculate a complete humidity state.
Worked example: Dry-air pressure is 99,825 Pa and the mixing ratio is about 0.009344 kg/kg, or 9.344 g/kg.
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Answer-first guide
Calculate water-vapor mixing ratio, mass fractions, and dry-air pressure from vapor and total pressure. Start with one clearly defined goal, enter values in the units shown, and keep the result attached to the assumptions below.
This tool is useful when your question includes air mixing ratio calculator, water vapor mixing ratio, humidity mixing ratio. It returns the outputs declared in the calculator contract rather than a live quote, approval, diagnosis, or professional sign-off.
Water-vapor partial pressure · Total air pressure · Water-vapor to dry-air molar-mass ratio ε. Keep the same time period, unit system, and currency wherever the form requires comparable values.
Run the worked example first, compare its output with the page's example, then change one input at a time. This makes an unexpected result easier to trace to a unit, boundary, or assumption.
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Dry-air pressure = p − e; mixing ratio w = εe/(p − e); vapor mass fraction = w/(1+w).
Atmospheric mixing ratio expresses water-vapor mass relative to dry-air mass. The calculator uses the vapor partial pressure, total pressure, and explicit molar-mass ratio to show the conversion without pretending to calculate a complete humidity state.
Dry-air pressure is 99,825 Pa and the mixing ratio is about 0.009344 kg/kg, or 9.344 g/kg.
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Science calculators define a system, choose an equation, apply units and constants, and show the substitution. Effects outside that model remain outside the result.
Introductory science problem solving builds from measured quantities and idealized relationships. Those models are valuable for learning and first-pass estimates, while experiments and engineering decisions need additional evidence.
Research and review
Researched by Hassan ALRowaie, Founder and editorial researcher at WorldCalculate.
This guide follows the live calculator's declared inputs, formula, worked example, assumptions, validation boundaries, and source-backed methodology. The review date describes editorial review of the calculator explanation; it is not a promise that external facts or rates remain current.
Mixing ratio is easy to confuse with relative humidity because both describe moisture in air. This page uses a narrower pressure-based relation: it compares water-vapor partial pressure with dry-air pressure and reports water-vapor mass relative to dry-air mass.
The mixing ratio w is the mass of water vapor divided by the mass of dry air. It is commonly reported in kilograms per kilogram or grams per kilogram of dry air.
That denominator matters. A vapor mass fraction divides by total moist-air mass, while mixing ratio divides by dry-air mass. The two values are related but are not identical.
The water-vapor partial pressure is the portion of total pressure attributed to water vapor under the mixture model. Dry-air pressure is total pressure minus vapor pressure.
The calculator requires vapor pressure to be below total pressure. If that condition fails, the dry-air denominator is zero or negative and the requested mixing ratio is not defined by this model.
The ε input represents the ratio of water-vapor molar mass to the selected dry-air molar mass convention. A common approximate value is 0.622, but keeping it visible makes the convention reviewable.
The page does not infer a composition-dependent ε or silently switch between different atmospheric definitions. If a course or dataset specifies another value, enter it and preserve that choice with the result.
The equation is w = εe divided by p minus e. Vapor pressure appears in the numerator, while dry-air pressure appears in the denominator. At fixed vapor pressure, lowering total pressure increases the mixing ratio because less dry-air pressure remains.
At fixed total pressure, increasing vapor pressure increases the ratio. These sensitivities follow from the equation and do not by themselves predict clouds, rain, or human comfort.
The page also reports vapor mass fraction as w divided by one plus w, and dry-air mass fraction as one divided by one plus w. Together they sum to one within rounding.
Vapor mole fraction is vapor pressure divided by total pressure. Keeping a pressure fraction, a mass fraction, and a mixing ratio together helps prevent a unitless quantity from being called the wrong thing.
With 1,500 Pa vapor pressure and 101,325 Pa total pressure, dry-air pressure is 99,825 Pa. Using ε = 0.622 gives a mixing ratio of about 0.009344 kg/kg, or 9.344 g/kg.
The number is relative to dry-air mass. It is not a relative-humidity percentage and cannot be compared to a saturation value without temperature-dependent vapor-pressure information.
Temperature is not required for this pressure-to-mixing-ratio equation. It becomes necessary when asking whether the air is saturated, calculating dew point, or comparing the vapor pressure with a saturation vapor-pressure curve.
A visitor should not reverse-engineer temperature from this result. Many temperatures can be paired with a pressure state depending on the moisture and thermodynamic assumptions.
The calculator does not forecast weather, diagnose indoor-air problems, select a humidifier setting, or estimate cloud formation. It is a pressure and composition relation with a stated dry-air convention.
For sounding or research work, keep the pressure source, thermodynamic convention, instrument correction, and observation time beside the value. Use the relevant official or scientific workflow when a real forecast or operational decision is required.
Calculate water-vapor mixing ratio, mass fractions, and dry-air pressure from vapor and total pressure.
Dry-air pressure = p − e; mixing ratio w = εe/(p − e); vapor mass fraction = w/(1+w). Atmospheric mixing ratio expresses water-vapor mass relative to dry-air mass. The calculator uses the vapor partial pressure, total pressure, and explicit molar-mass ratio to show the conversion without pretending to calculate a complete humidity state.
Enter Water-vapor partial pressure, Total air pressure, Water-vapor to dry-air molar-mass ratio ε, then choose Calculate.
Vapor pressure is the water-vapor partial pressure and is less than total pressure. Total and vapor pressures use the same absolute pressure unit. The entered ε represents the water-vapor to dry-air molar-mass ratio used by the selected convention. The air mixture is represented by dry air plus water vapor only for this relation. No saturation-pressure, temperature, dew-point, cloud, or precipitation model is included. The result is a composition arithmetic worksheet, not a weather forecast or comfort recommendation.
This calculator is part of the WorldCalculate library. Its formula, example, assumptions, input bounds, and output formatting follow the official methodology.
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