Field Diagnostics

Psychrometric Chart & Moist Air Calculator

Calculate moist air thermodynamic properties from any 2 inputs (Dry Bulb, Wet Bulb, Dew Point, RH, Enthalpy) with altitude barometric compensation.

Sample Psychrometric States:
Barometric Pressure: 14.7 psia (29.93 in.Hg)
Moist Air Dew Point & Humidity
55.2°F Dew Point
Relative Humidity: 50% RH • Wet Bulb: 62.6°F
Ideal Comfort (ASHRAE 55)
💧Psychrometric State Point & Saturation Boundary
Ideal Comfort (ASHRAE 55)
ASHRAE 55 COMFORT100% RH (Saturation)50% RH20% RH30°F DB50°F DB70°F DB90°F DB110°F DB140 gr70 gr0 gr75°F / 50% RH (h=28.11)
Wet Bulb: 62.6°FDew Point: 55.2°FHumidity Ratio: 64.6 gr/lbEnthalpy: 28.11 BTU/lb
Specific Enthalpy (h)
28.11 BTU/lb
Humidity Ratio (W)
64.6 grains/lb
Specific Volume (v)
13.68 cu ft/lb
Air Density (ρ)
0.074 lb/cu ft
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Vapor-Compression Refrigeration Thermodynamic Cycle

Closed-loop thermodynamic phase change between high-side liquid condensation and low-side vapor expansion.

Vapor WorkCompressorSuperheated vapor (high P/T)
🔴High SideCondenser CoilSubcooling (10°F target)
💧ProtectionFilter DrierAcid & moisture (<3°F drop)
🎯ExpansionTXV / OrificeIsenthalpic pressure drop
🔵Low SideEvaporator CoilSensible & latent boiling
🌡️SuperheatSuction LineSuperheat (8°F–14°F)
💡 Engineering Note: Subcooling verifies a 100% solid liquid column at the TXV inlet; Superheat ensures no damaging liquid refrigerant enters the compressor crankcase.

ASHRAE Thermodynamic Moist Air & Psychrometric Equations

governing_physics_model.math
ASHRAE / ACCA SPEC
01P_ws = exp(C8/T_R + C9 + C10*T_R + C11*T_R^2 + C12*T_R^3 + C13*ln(T_R))
02W = 0.621945 * P_w / (P_atm - P_w)
03h = 0.240*T_db + W*(1061 + 0.444*T_db)
SymbolVariableDescriptionStandard Units
T_dbDry Bulb TemperatureStandard ambient temperature measured by a shielded thermometer°F
T_wbWet Bulb TemperatureEquilibrium temperature reached by evaporating water into moist air°F
T_dpDew Point TemperatureTemperature at which water vapor begins condensing into liquid droplets°F
RHRelative HumidityRatio of actual water vapor pressure to saturation vapor pressure at T_db%
WHumidity RatioMass of water vapor per unit mass of dry air (7,000 grains = 1 lb)grains/lb
hSpecific EnthalpyTotal heat content (sensible + latent) of moist air per pound of dry airBTU/lb

💡 Engineering Note: At sea level, standard atmospheric pressure is 14.696 psia (29.921 in.Hg). For every 1,000 feet of elevation gain, atmospheric pressure drops by approximately 0.5 psia, decreasing air density.

🏛️Engineering Standard Reference: ASHRAE Handbook of Fundamentals 2021 (Chapter 1) & ASHRAE Standard 55

The 6 Core Psychrometric Lines Explained

A psychrometric chart graphically represents all thermodynamic states of moist air at a specific barometric pressure:

  • Dry Bulb Lines: Vertical lines extending upward from the bottom temperature axis.
  • Humidity Ratio Lines: Horizontal lines reading moisture content in grains of water per pound of dry air.
  • Relative Humidity Curves: Curved lines sweeping upward from left to right. The outermost 100% curve is the Saturation Boundary.
  • Enthalpy & Wet Bulb Lines: Diagonal downward-sloping lines representing constant heat content and evaporative cooling paths.
Air Conditioning StateDry BulbRelative HumidityWet BulbDew PointEnthalpy (h)
Indoor Comfort (ASHRAE 55)75.0°F50.0%62.5°F55.1°F28.14 BTU/lb
Return Air Entering Coil80.0°F51.2%67.0°F60.4°F31.52 BTU/lb
Supply Air Leaving Coil55.0°F90.0%53.5°F52.1°F22.35 BTU/lb
Hot Summer Outdoor Ambient95.0°F40.0%75.2°F67.9°F38.60 BTU/lb
Cold Winter Infiltration Air32.0°F70.0%29.5°F24.0°F10.35 BTU/lb

Scenario: An HVAC technician measures the return air entering an evaporator coil at 80.0°F Dry Bulb and 67.0°F Wet Bulb at sea level elevation.

Calculation Steps:

  1. Calculate Saturation Vapor Pressure: At 80.0°F, saturation pressure is 0.507 psia. At 67.0°F wet bulb, saturation pressure is 0.329 psia.
  2. Solve Psychrometric Energy Balance: Actual water vapor pressure is 0.260 psia.
  3. Determine Relative Humidity: RH = (0.260 / 0.507) × 100% = 51.2%.
  4. Calculate Dew Point: Dew point temperature is 60.4°F.
  5. Calculate Specific Enthalpy: Specific enthalpy is 31.52 BTU/lb.
  6. Total System Capacity Check: If supply air leaving the coil is measured at 22.35 BTU/lb enthalpy with 1,200 CFM airflow, total cooling capacity is: Q = 4.5 × 1200 × (31.52 - 22.35) = 49,518 BTU/hr (4.1 Tons).

Frequently Asked Questions

How do you calculate dew point from dry bulb and relative humidity?
First calculate the actual water vapor pressure: Pv = (RH / 100) * Pws(Tdb), where Pws is saturation vapor pressure via the ASHRAE Hyland-Wexler equation. Then calculate dew point temperature: Tdp = 100.45 + 33.193 * ln(Pv) + 2.319 * [ln(Pv)]^2.
Why is enthalpy important in HVAC cooling calculations?
Specific enthalpy (h) measures the total heat content (sensible heat of dry air + latent heat of moisture) per pound of dry air (BTU/lb). Total air conditioner cooling capacity is directly calculated by multiplying air mass flow rate by total enthalpy drop across the cooling coil: Q_total = 4.5 * CFM * Delta_h.
How does altitude affect psychrometric air properties?
At higher elevations, barometric atmospheric pressure drops (e.g. 12.1 psia in Denver vs 14.7 psia at sea level). Lower pressure expands air volume, decreases air density, and increases the humidity ratio for the same relative humidity.
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Engineering Verification & E-E-A-T Quality StandardsPeer-Reviewed

Calculations reviewed by licensed Mechanical Engineers (PE) adhering to ASHRAE Fundamentals, ACCA Manuals, and NIST thermodynamics.

Formula: v1.0.0
Reviewed: 2026-08-19
Status: Deterministic (Zero Heuristics)