HVAC Systems Encyclopedia

A comprehensive encyclopedia of heating, ventilation, and air conditioning systems

Moisture Storage Capacity

Moisture storage capacity quantifies a material’s ability to absorb and retain water vapor and liquid water as a function of relative humidity and temperature. This property determines transient moisture behavior in building assemblies, influencing condensation risk, drying potential, and indoor humidity stability.

Moisture Storage Mechanisms

Building materials store moisture through two distinct physical mechanisms that operate across different relative humidity ranges.

Hygroscopic Moisture Storage

Hygroscopic storage occurs when water vapor molecules adsorb onto material surfaces and absorb into the material structure at relative humidities below saturation. This mechanism dominates in the hygroscopic range (0-95% RH).

Molecular Processes:

  • Monolayer adsorption: Water molecules form a single layer on hydrophilic surface sites at low RH (0-30%)
  • Multilayer adsorption: Additional water layers build on the initial monolayer at moderate RH (30-70%)
  • Capillary condensation: Water condenses in small pores (<0.1 μm) at high RH (70-95%)
  • Absorption: Water penetrates the molecular structure of hygroscopic materials (wood, cellulose)

The hygroscopic moisture content increases non-linearly with relative humidity, described by sorption isotherms.

Capillary Moisture Storage

Capillary storage occurs when liquid water fills pore spaces through surface tension forces. This mechanism activates at relative humidities above 95% or when liquid water contacts the material.

Physical Characteristics:

  • Governed by capillary pressure: Pc = 2σcosθ/r
  • Where σ = surface tension (0.0728 N/m at 20°C), θ = contact angle, r = pore radius
  • Smaller pores generate higher capillary suction
  • Moisture content increases dramatically near saturation
  • Hysteresis between wetting and drying curves

Sorption Isotherms

The moisture storage function (sorption isotherm) relates equilibrium moisture content to relative humidity at constant temperature.

Isotherm Characteristics

RH RangeStorage MechanismMoisture Increase RateTypical Materials
0-30%Monolayer adsorptionLow, nearly linearAll porous materials
30-70%Multilayer adsorptionModerate, curvilinearHygroscopic materials
70-95%Capillary condensationHigh, exponentialFine-pored materials
95-100%Capillary saturationExtreme, asymptoticAll porous materials

Mathematical Models

BET Model (Low RH):

w = (w_m × C × φ) / [(1-φ)(1-φ+C×φ)]

Where:

  • w = moisture content (kg/m³)
  • w_m = monolayer moisture content
  • C = BET constant (energy parameter)
  • φ = relative humidity (0-1)

Modified Oswin Model (Full Range):

w = A × [φ/(1-φ)]^B + C×φ^D

Where A, B, C, D are material-specific fitting parameters.

Hysteresis Effects

Moisture storage exhibits hysteresis—different isotherms for adsorption (increasing RH) and desorption (decreasing RH). The desorption curve lies above the adsorption curve, meaning materials retain more moisture during drying than they contain at the same RH during wetting.

Hysteresis Ratio:

  • Typical hysteresis: 20-40% difference in moisture content
  • Maximum difference occurs at 40-60% RH
  • Important for accurate transient moisture modeling

Material-Specific Storage Functions

Different building materials exhibit characteristic moisture storage behaviors based on their pore structure and surface chemistry.

Organic Materials

Wood and Wood Products:

  • Fiber saturation point: 25-30% moisture content by mass (approximately 95% RH)
  • Below FSP: Hygroscopic storage in cell walls
  • Above FSP: Free water in cell lumens
  • Strong temperature dependence: -0.02% MC per °C
  • Species variation: Dense hardwoods store less than softwoods
MaterialDensity (kg/m³)Moisture Content at 80% RH (kg/m³)Saturation (kg/m³)
Spruce/pine45065600
Oak70085750
Plywood55070650
OSB65095800
Particleboard700120900

Cellulose Insulation:

  • High hygroscopic capacity: 15-18% by mass at 80% RH
  • Excellent moisture buffering performance
  • Minimal impact on thermal performance until >20% moisture content
  • Reversible storage in normal building conditions

Mineral Materials

Brick and Masonry:

  • Wide pore size distribution creates gradual isotherm
  • Fired clay brick: 2-4% by volume at 80% RH
  • Calcium silicate brick: 5-8% by volume at 80% RH
  • Capillary active—significant liquid water transport
MaterialPorosity (%)w80 (kg/m³)w_sat (kg/m³)Capillary Absorption (kg/m²·h^0.5)
Fired clay brick30402800.15
Calcium silicate brick401204500.40
Concrete block (lightweight)55855500.25
Concrete (normal weight)15201500.05

Concrete and Mortar:

  • Cement paste: High initial moisture content (50-60% by volume when cast)
  • Drying progresses over months to years
  • Equilibrium moisture at 80% RH: 4-6% by volume
  • Carbonation reduces moisture storage capacity over time

Gypsum-Based Materials

Gypsum Board:

  • Moderate hygroscopic capacity: 1-2% by mass at 80% RH
  • Sharp increase above 90% RH due to gypsum dissolution risk
  • Temperature sensitivity: Factor of 1.5-2 between 5°C and 30°C
  • Paper facings contribute additional hygroscopic storage
MaterialDensity (kg/m³)Sorption at 50% RH (kg/m³)Sorption at 80% RH (kg/m³)
Standard gypsum board650513
Type X gypsum board750615
Gypsum plaster1100822
Clay plaster14001850

Insulation Materials

Fibrous Insulation:

  • Glass fiber: Minimal hygroscopic storage (<0.5% by mass)
  • Mineral wool: Low storage (1-2% by mass at 80% RH)
  • Cellulose: High storage (15-18% by mass at 80% RH)
  • Moisture affects thermal conductivity: +3-5% per 1% moisture content increase

Foam Insulation:

  • Closed-cell foams: Negligible moisture storage
  • Open-cell spray foam: Moderate storage (3-5% by volume at 80% RH)
  • EPS: Minimal hygroscopic storage, can hold condensed water in voids
  • XPS: Lowest moisture storage among foam products

Moisture Buffering in Buildings

Moisture storage capacity enables materials to buffer indoor humidity fluctuations, improving occupant comfort and reducing mechanical dehumidification loads.

Moisture Buffering Value (MBV)

The practical moisture buffering value quantifies a material’s ability to moderate humidity changes:

MBV = Δm / (A × Δφ)  [g/(m²·%RH)]

Where:

  • Δm = mass of moisture absorbed/desorbed (g)
  • A = exposed surface area (m²)
  • Δφ = relative humidity variation (%)

Classification:

  • Negligible: MBV < 0.2 g/(m²·%RH) - Sealed surfaces, vapor barriers
  • Limited: MBV = 0.2-0.5 - Gypsum board, concrete
  • Moderate: MBV = 0.5-1.0 - Uncoated wood, clay plaster
  • Good: MBV = 1.0-2.0 - Exposed cellulose, thick wood panels
  • Excellent: MBV > 2.0 - Hygroscopic finishes, natural fiber panels

Penetration Depth

Moisture buffering is limited by the effective penetration depth during daily humidity cycles:

d_p = √(δ_v / (ρ × ∂w/∂φ × 1/τ))

Where:

  • δ_v = vapor permeability (kg/m·s·Pa)
  • ρ = material density (kg/m³)
  • ∂w/∂φ = slope of sorption isotherm
  • τ = period of humidity cycle (86400 s for daily)

Typical penetration depths for 24-hour cycles: 5-15 mm for most building materials.

Building Assembly Buffering

Total moisture buffering depends on:

  • Surface area exposure: Higher surface-to-volume ratios increase buffering
  • Material accessibility: Paint and coatings reduce buffering by 50-90%
  • Air change rate: Higher ventilation reduces the impact of material buffering
  • Internal moisture generation: Occupant activities, cooking, bathing

Hygrothermal Simulation Parameters

Accurate modeling of moisture storage in WUFI, DELPHIN, and other hygrothermal software requires proper characterization.

WUFI Input Requirements

ParameterUnitsMeasurement MethodTypical Range
Moisture storage functionkg/m³Sorption balance, DVSMaterial-dependent
Free water saturationkg/m³Vacuum saturation100-900 kg/m³
Moisture-dependent thermal conductivityW/m·KGuarded hot plate at various MCFactor of 1.2-3
Moisture-dependent vapor permeabilitykg/m·s·PaCup tests at various RH1-2 orders of magnitude

Typical Storage Function Data

Wood-Based Materials (Spruce, 500 kg/m³):

  • 30% RH: 30 kg/m³
  • 50% RH: 50 kg/m³
  • 65% RH: 65 kg/m³
  • 80% RH: 95 kg/m³
  • 95% RH: 200 kg/m³
  • 100% RH (free saturation): 600 kg/m³

Gypsum Board (650 kg/m³):

  • 30% RH: 3 kg/m³
  • 50% RH: 5 kg/m³
  • 65% RH: 7 kg/m³
  • 80% RH: 13 kg/m³
  • 95% RH: 40 kg/m³
  • 100% RH: 100 kg/m³

Critical Modeling Considerations

Temperature Dependence: Moisture storage decreases with increasing temperature. Correction factor:

w(T) = w(T_ref) × exp[-0.02 × (T - T_ref)]

Where T_ref = 20°C, temperatures in °C.

Initial Conditions:

  • Built-in construction moisture: 1-5% by volume in concrete, masonry
  • Manufacturing moisture: 8-12% in wood products
  • Hygroscopic equilibrium: Assume 50% RH for initial simulations
  • Verify initial moisture content with field measurements

Boundary Conditions:

  • Interior: ASHRAE 160 profiles or measured data
  • Exterior: Climate files with driving rain load
  • Ground contact: Capillary rise and soil moisture potential

Design Applications

Understanding moisture storage capacity informs multiple design decisions.

Condensation Risk Assessment

High moisture storage capacity reduces condensation risk by:

  • Absorbing moisture before liquid water forms
  • Distributing moisture over larger volume
  • Enabling redistribution during drying periods

Critical for:

  • Cold climate wall assemblies
  • Roof assemblies with interior humidity loads
  • Assemblies with seasonal moisture accumulation

Drying Reserve

Materials with high storage capacity provide drying reserve—the ability to safely absorb and later release construction moisture or occasional wetting events.

Calculation:

Drying Reserve = (w_80% - w_50%) × Volume

Adequate drying reserve: >2 kg/m² of assembly cross-section for typical climates.

Material Selection Criteria

Prefer high storage capacity when:

  • Indoor humidity control is important
  • Building has high occupant density
  • Mechanical ventilation rates are low
  • Climate has daily or seasonal humidity variations

Prefer low storage capacity when:

  • Rapid drying is essential
  • Moisture sources are continuous
  • Materials are exposed to weather
  • Freeze-thaw damage is a concern

Measurement Methods

Laboratory Techniques

Desiccator Method (ASTM C1498):

  • Equilibrate specimens over saturated salt solutions
  • Each salt provides specific RH at controlled temperature
  • Measure mass at equilibrium (2-4 weeks per RH step)
  • Generate full sorption isotherm with 8-12 RH points

Dynamic Vapor Sorption (DVS):

  • Automated microbalance with RH control
  • Continuous mass measurement during RH ramping
  • Complete isotherm in 3-5 days
  • Provides both adsorption and desorption curves

Pressure Plate Method (High RH/Capillary Range):

  • Apply controlled suction to saturated specimens
  • Measure moisture content at equilibrium
  • Characterizes capillary moisture storage >95% RH
  • Essential for modeling liquid water transport

Field Assessment

Non-destructive moisture content measurement enables validation of hygrothermal models:

  • Pin-type resistance meters: 7-30% MC in wood
  • Capacitance meters: Qualitative indication in various materials
  • Microwave reflection: Research-grade quantitative measurement
  • Neutron probe: Concrete moisture profiling

Practical Design Values

For preliminary design and rule-of-thumb assessments:

Material CategoryMoisture Storage at 80% RHMoisture Buffering Value
Dense materials (concrete, brick)2-4% by volumeLimited (0.2-0.5)
Medium density (gypsum, plaster)1-2% by massLimited to Moderate
Wood and wood products12-18% by massModerate to Good
Hygroscopic insulation15-20% by massGood to Excellent
Paint/coatings on substrate80-95% reductionNegligible

These values guide assembly design and inform expectations for moisture buffering performance in occupied buildings.


References:

  • ASHRAE Handbook—Fundamentals, Chapter 26: Heat, Air, and Moisture Control in Building Assemblies
  • ISO 12571: Hygrothermal Performance of Building Materials and Products
  • ASHRAE 160: Criteria for Moisture-Control Design Analysis in Buildings
  • Künzel, H.M.: Simultaneous Heat and Moisture Transport in Building Components

Sections

Hygroscopic Materials

Hygroscopic material characteristics in building envelopes including moisture sorption mechanisms, adsorption and absorption processes, equilibrium moisture content, and material-specific hygroscopic behavior.

Buffering Capacity

Moisture buffering capacity in building materials including RH fluctuation dampening, moisture buffer value, effective penetration depth, diurnal and seasonal buffering, and hygric inertia effects.

Sorption Isotherms

Sorption isotherm characteristics in building materials including adsorption and desorption curves, hysteresis effects, temperature dependence, and material-specific moisture storage relationships.