4.3 Psychrometrics & Air Properties for Humid Climates
Key Takeaways
- The psychrometric chart visually defines moist air properties, where dry-bulb temperature reflects sensible heat, wet-bulb reflects total heat (enthalpy), and dew point dictates moisture condensation thresholds.
- Humidity ratio measures the exact moisture mass in grains per pound of dry air (7,000 grains = 1 lb water), providing the basis for calculating latent cooling capacity (Q_latent = 0.68 * CFM * delta W_grains).
- In Alabama's humid subtropical climate, cooling equipment must satisfy low Sensible Heat Ratios (SHR = 0.65 to 0.75), requiring reduced airflow (325 to 350 CFM/ton) to lower the Apparatus Dew Point (ADP) for aggressive latent moisture removal.
- Total system heat exchange obeys the enthalpy equation Q_total = 4.5 * CFM * delta h, representing the exact thermodynamic sum of sensible (1.08 * CFM * delta T) and latent heat capacities.
- A normal residential evaporator air temperature split (delta T) ranges between 18°F and 22°F; splits below 16°F indicate insufficient capacity or excessive airflow, while splits above 24°F signal severely choked airflow.
4.3 Psychrometrics & Air Properties for Humid Climates
[!NOTE] Psychrometrics and Alabama's Humid Subtropical Climate: Psychrometrics is the study of the thermodynamic properties of moist air (mixtures of dry air and water vapor). In Alabama, high outdoor ambient humidity and prolonged summer dew points make moisture control as critical as sensible cooling. On the Alabama HACR contractor exam, psychrometric chart navigation, Sensible Heat Ratio (SHR) calculations, airflow CFM formulas, and supply air temperature splits are heavily tested core competencies.
Conditioning indoor air requires precise simultaneous control of temperature, moisture content, air motion, and air cleanliness. In the Southeastern United States—and specifically across Alabama from the Tennessee Valley to Mobile Bay—mechanical contractors must master psychrometric processes to prevent moisture damage, indoor mold proliferation, and high indoor relative humidity.
The Seven Fundamental Properties of Moist Air
The standard ASHRAE psychrometric chart plots seven interdependent physical and thermodynamic properties of moist air at standard atmospheric pressure ($14.696\text{ psia} / 29.92\text{ in. Hg}$). If any two independent properties are known, all remaining five properties can be graphically determined or mathematically calculated.
Enthalpy (h) ◄───┐
Scale (BTU/lb) │ Saturation Curve (100% Relative Humidity)
│ / / / /
│ / / / / ◄── Humidity Ratio (W)
│ / / / / (Grains / lb Dry Air)
│ / Dew / / / ▲
│ / Point/ / / │
│ / Curve / / │
│ / / / / │
│ / / / / │
└─────/──────/──────/──────/──────────────────┴─►
Dry-Bulb Temperature (DB, °F) [Horizontal Axis]
1. Dry-Bulb Temperature ($DB$)
Dry-bulb temperature is the true ambient air temperature measured by an ordinary, dry thermometer shielded from direct thermal radiation. It is plotted along the horizontal bottom axis of the psychrometric chart, with constant dry-bulb lines extending vertically upward.
2. Wet-Bulb Temperature ($WB$)
Wet-bulb temperature reflects the dynamic evaporative cooling capacity of the air. It is measured by a thermometer whose sensing bulb is covered by a clean, water-saturated fabric wick exposed to a rapid air stream (a sling psychrometer). As water evaporates from the wick, it cools the bulb down to the saturation equilibrium point. Wet-bulb lines slope diagonally downward from the saturation curve toward the right, parallel to lines of constant enthalpy.
3. Dew Point Temperature ($DP$)
Dew point is the temperature to which moist air must be cooled at constant pressure and constant moisture content for water vapor to begin condensing into liquid dew ($100%\text{ relative humidity}$). Dew point lines project horizontally to the left to intersect the curved saturation line.
4. Relative Humidity ($RH$)
Relative humidity is the ratio (expressed as a percentage) of the actual partial water vapor pressure in the air to the saturation vapor pressure of water at the same dry-bulb temperature: Plotted as distinct curved lines sweeping upward from left to right. The outermost boundary curve represents $100%\text{ RH}$ (the Saturation Curve), where Dry-Bulb, Wet-Bulb, and Dew Point are exactly identical.
5. Humidity Ratio / Specific Humidity ($W$)
Humidity ratio is the actual physical weight of water vapor contained within one pound of dry air, plotted on the vertical right-hand axis of the chart. It is measured in grains of moisture per pound of dry air ($\text{gr/lb}$) or in decimal fractions of a pound of water per pound of dry air ($\text{lb}{w}/\text{lb}{da}$).
6. Specific Volume ($v$)
Specific volume is the volume occupied by one pound of dry air plus its associated water vapor, expressed in cubic feet per pound of dry air ($\text{ft}^3/\text{lb}$). Plotted as steeply sloping diagonal lines. For standard dry air at sea level ($70^\circ\text{F}$), specific volume is approximately $13.33\text{ ft}^3/\text{lb}$, corresponding to standard air density:
7. Enthalpy ($h$)
Enthalpy is the total thermal heat energy (sensible heat of dry air + sensible/latent heat of water vapor) measured above a $0^\circ\text{F}$ baseline in BTU per pound of dry air ($\text{BTU/lb}_{da}$). Plotted on an external diagonal scale located above and to the left of the saturation curve.
Moist Air Properties Summary
| Property | Symbol | Primary Units | Chart Orientation / Line Direction |
|---|---|---|---|
| Dry-Bulb Temperature | $DB$ | Degrees Fahrenheit ($^\circ\text{F}$) | Vertical lines originating from bottom axis |
| Wet-Bulb Temperature | $WB$ | Degrees Fahrenheit ($^\circ\text{F}$) | Diagonal lines sloping downward to the right |
| Dew Point Temperature | $DP$ | Degrees Fahrenheit ($^\circ\text{F}$) | Horizontal lines projecting to the saturation curve |
| Relative Humidity | $RH$ | Percentage ($%$) | Curved lines sweeping upward from bottom-left to top-right |
| Humidity Ratio | $W$ | Grains of moisture per pound ($\text{gr/lb}$) | Horizontal lines originating from right-hand axis |
| Specific Volume | $v$ | Cubic feet per pound ($\text{ft}^3/\text{lb}$) | Steep diagonal lines crossing from lower-right to upper-left |
| Enthalpy | $h$ | $\text{BTU per pound of dry air}$ ($\text{BTU/lb}$) | Diagonal scale outside the saturation boundary curve |
Psychrometric Processes & The Sensible Heat Ratio (SHR)
Air conditioning processes correspond to geometric vectors on the psychrometric chart:
- Sensible Cooling Only: A straight horizontal vector moving directly to the left (constant humidity ratio $W$, decreasing dry-bulb $DB$, increasing relative humidity $RH$).
- Sensible Heating Only: A straight horizontal vector moving directly to the right.
- Humidification Only: A straight vertical vector moving directly upward (constant dry-bulb $DB$, increasing humidity ratio $W$).
- Dehumidification Only: A straight vertical vector moving directly downward.
- Cooling and Dehumidification (Standard A/C Process): A diagonal vector sloping downward and to the left toward the saturation curve. As warm moist return air passes across a cooling coil whose surface temperature is below the entering air dew point, the air is both cooled sensibly and dehumidified latently.
[Pure Humidification] (▲)
│
[Cooling & Dehumidification] (◄─▼) │ (▲─►) [Heating & Humidification]
\ │ /
\ │ /
[Pure Sensible Cooling] (◄) ─────────── [POINT] ─────────── (►) [Pure Sensible Heating]
/ │ \
/ │ \
[Evaporative Cooling] (◄─▲) / │ (▼) [Pure Dehumidification]
Sensible Heat Ratio (SHR)
The Sensible Heat Ratio (SHR) is the fraction of total cooling capacity dedicated to lowering dry-bulb temperature compared to total cooling capacity (sensible plus latent):
- Arid Climates (e.g., Arizona, Nevada): $SHR \approx 0.85 \text{ to } 0.90$. High sensible heat loads with minimal ambient humidity; equipment must focus almost exclusively on lowering air temperature.
- Mixed-Humid Climates (e.g., Ohio Valley): $SHR \approx 0.75 \text{ to } 0.80$.
- Humid Subtropical Climates (Alabama / Gulf Coast): $SHR \approx 0.65 \text{ to } 0.75$. Significant portions (25% to 35%) of total system cooling capacity must be allocated to removing moisture from the air stream.
Managing High Latent Loads in Alabama's Humid Subtropical Climate
Alabama lies within the humid subtropical climate zone (ASHRAE Climate Zones 2A and 3A). Summer design conditions in Mobile, Montgomery, Birmingham, and Huntsville frequently feature outdoor dry-bulb temperatures of $95^\circ\text{F}$ accompanied by coincident wet-bulb temperatures of $78^\circ\text{F}$, yielding outdoor dew points exceeding $73^\circ\text{F}$ (with ambient air carrying over $125\text{ grains of moisture per pound}$). Under these conditions, managing indoor humidity requires specialized engineering strategies.
The Severe Consequences of Equipment Oversizing (Short-Cycling)
A widespread error committed by unlicensed or inexperienced contractors in Alabama is equipment oversizing ("bigger is better"). Installing a 4-ton unit where an ACCA Manual J load calculation calls for a 2.5-ton system causes severe operational defects:
- Sensible Satisfaction without Moisture Removal: The oversized unit delivers massive sensible cooling, driving the indoor thermostat down to its $72^\circ\text{F}$ setpoint in 5 to 8 minutes.
- Failure to Reach Apparatus Dew Point: An evaporator coil requires approximately 10 to 12 minutes of continuous operation before the coil surface temperature drops to its steady-state Apparatus Dew Point (ADP) and begins condensing moisture.
- The "Cold and Clammy" House: Because the unit short-cycles off after only a few minutes, virtually zero latent moisture is removed. The house ends up at $70^\circ\text{F} \text{ DB}$ but with an unlivable $65% \text{ to } 75% \text{ Relative Humidity}$.
- Microbial and Mold Proliferation: Under Alabama building conditions, indoor relative humidity sustained above $60%$ fosters rapid propagation of toxic mold (Stachybotrys, Aspergillus), mildew, and dust mites inside sheetrock walls, carpeting, and supply ductwork.
Airflow Tuning: Modulating CFM per Ton for Latent Removal
Standard commercial rating test standards specify an airflow rate of $400\text{ CFM per ton of cooling}$:
- Lowering Airflow to 325–350 CFM/ton: In Alabama homes with high latent loads, technicians deliberately configure blower speeds (via ECM motor dip switches or control taps) to deliver $325\text{ to }350\text{ CFM per ton}$.
- Thermodynamic Mechanism: Reducing airflow slows the velocity of air across the evaporator coil fins. The reduced volume of air causes the refrigerant in the coil to evaporate at a lower suction pressure and saturation temperature, significantly lowering the coil's Apparatus Dew Point (ADP). Furthermore, slower air increases contact dwell time, forcing substantially more moisture vapor to condense into the drain pan. This lowers the equipment's Sensible Heat Ratio to $0.70$ or below, matching the building's high latent load.
- Variable-Speed Dehumidification Profiles: Modern variable-speed blower systems integrate humidity sensors. When indoor relative humidity exceeds $50%$, the thermostat commands the blower to ramp down to $80%\text{ normal airflow}$ ($320\text{ CFM/ton}$), extending runtimes and wringing out moisture without over-cooling the living space.
Core HVAC Airflow & Heat Formulas (Must-Know Exam Mathematics)
In standard air calculations (air density $\rho = 0.075\text{ lb/ft}^3$, specific heat $c_p = 0.24\text{ BTU}/(\text{lb}\cdot^\circ\text{F})$, and moisture vaporization latent heat $\approx 1,061\text{ BTU/lb}$), three universal equations govern system capacity:
+---------------------------------------------------------------------------------------------------+
| THE THREE UNIVERSAL AIRFLOW FORMULAS |
+---------------------------------------------------------------------------------------------------+
| 1. SENSIBLE HEAT EQUATION: |
| Q_sensible = 1.08 * CFM * delta T |
| Where: 1.08 = 0.075 lb/ft^3 * 0.24 BTU/(lb-°F) * 60 min/hr |
+---------------------------------------------------------------------------------------------------+
| 2. LATENT HEAT EQUATION: |
| Q_latent = 0.68 * CFM * delta W_grains |
| Where: 0.68 = 0.075 lb/ft^3 * (1,061 BTU/lb / 7,000 grains/lb) * 60 min/hr |
+---------------------------------------------------------------------------------------------------+
| 3. TOTAL HEAT EQUATION (ENTHALPY): |
| Q_total = 4.5 * CFM * delta h |
| Where: 4.5 = 0.075 lb/ft^3 * 60 min/hr |
+---------------------------------------------------------------------------------------------------+
1. Sensible Heat Formula
- $Q_s$ = Sensible heat capacity in $\text{BTU/hr}$
- $\text{CFM}$ = Volumetric airflow rate in cubic feet per minute
- $\Delta T$ = Temperature differential between entering return air and leaving supply air ($T_{\text{return}} - T_{\text{supply}}$ in $^\circ\text{F}$)
- Derivation of Constant 1.08:
2. Latent Heat Formula
- $Q_l$ = Latent heat capacity in $\text{BTU/hr}$
- $\Delta W_{\text{grains}}$ = Humidity ratio difference between entering return air and leaving supply air in grains of moisture per pound of dry air ($W_{\text{return}} - W_{\text{supply}}$)
- Derivation of Constant 0.68:
3. Total Heat Formula (The Enthalpy Method)
- $Q_t$ = Total heat capacity (sensible + latent) in $\text{BTU/hr}$
- $\Delta h$ = Enthalpy difference between entering return air and leaving supply air in $\text{BTU per pound of dry air}$ ($h_{\text{return}} - h_{\text{supply}}$)
- Derivation of Constant 4.5:
Note that by the law of conservation of energy: $Q_{\text{total}} = Q_{\text{sensible}} + Q_{\text{latent}}$.
Coil Bypass Factor ($BF$) & Apparatus Dew Point ($ADP$)
When moist air passes through a cooling coil, not all air molecules make physical contact with the cold metal fins and tubes:
- Apparatus Dew Point (ADP): The effective average surface temperature of the cooling coil tubes and fins.
- Coil Bypass Factor ($BF$): The fraction of total airflow that passes through the coil without contacting the cooling surface, exiting completely unaltered at entering conditions. For modern residential multi-row coils, $BF$ ranges between $0.05\text{ and }0.15$ (meaning 5% to 15% of air bypasses the surface).
- Contact Factor ($CF$): The fraction of air that makes direct contact with the coil surface:
A coil with deeper rows (e.g., 4 rows vs. 2 rows) and higher fin density (e.g., 14 fins per inch vs. 10 fins per inch) reduces the bypass factor, forcing more air into direct contact with the surface and maximizing dehumidification.
Supply Air Temperature Split ($\Delta T$) Field Diagnostics
Measuring the temperature drop across the indoor evaporator coil—termed the Supply Air Temperature Split—is an essential field diagnostic:
- Target Baseline: Under standard indoor design conditions ($75^\circ\text{F}\text{ DB}$, $63^\circ\text{F}\text{ WB}$, $\sim 50%\text{ RH}$) and $400\text{ CFM/ton}$ airflow, the normal temperature split across a residential evaporator coil is $18^\circ\text{F} \text{ to } 22^\circ\text{F}$.
Diagnostic Interpretation of Off-Target Temperature Splits
- Low Temperature Split ($\Delta T < 16^\circ\text{F}$):
- Cause 1: Inadequate System Capacity: Low refrigerant charge, defective compressor valves, worn scroll wraps, or restricted metering device.
- Cause 2: Excessive Airflow: Blower running too fast ($> 450\text{ CFM/ton}$), duct static bypass dampers stuck open.
- Cause 3: High Latent Load: Extremely humid return air. When entering return air has high moisture content ($> 65%\text{ RH}$), the cooling coil expends a large percentage of its total capacity condensing water vapor (latent heat) rather than lowering the dry-bulb temperature (sensible heat). A $15^\circ\text{F}$ split in a very humid home may represent normal total capacity, but with a depressed sensible split.
- High Temperature Split ($\Delta T > 24^\circ\text{F}$):
- Cause 1: Restricted Airflow (Most Common): Severely loaded or clogged air filters, closed supply registers, collapsed or undersized flex ducts, dirty evaporator coil fins, or blower wheel caked with dirt.
- Cause 2: Low Entering Return Air Wet-Bulb: In very dry indoor air (low latent load), nearly 100% of coil capacity converts to sensible cooling, driving the dry-bulb temperature split up to $24^\circ\text{F} - 26^\circ\text{F}$.
An air conditioning system circulates 1,600 CFM of air across an evaporator coil. Entering return air conditions are 76°F dry-bulb and 64°F wet-bulb (enthalpy = 29.3 BTU/lb, humidity ratio = 68 grains/lb). Leaving supply air conditions are 56°F dry-bulb and 54°F wet-bulb (enthalpy = 22.6 BTU/lb, humidity ratio = 56 grains/lb). Using standard air formulas, what are the sensible heat removal (Q_s), latent heat removal (Q_l), and total cooling capacity (Q_t)?
In Alabama's humid climate, a homeowner complains that a newly installed 4-ton heat pump cools the house to the 72°F thermostat setpoint very quickly, but the indoor air feels uncomfortably damp and clammy, with indoor relative humidity hovering at 68%. What is the most effective engineering adjustment to remediate this issue?
A technician measures the return air dry-bulb temperature at 75°F and supply air dry-bulb temperature at 48°F across an active evaporator coil operating with normal indoor humidity (50% RH). The resulting temperature split (delta T) is 27°F. What does this abnormally high temperature split indicate?