4.1. Basic Moisture Transfer Mechanisms and Approximations
The simple models developed here approximate the moisture transfer in the wall assembly without accounting for all the complexity of the three-dimensional time-dependent moisture transport that occurs as water moves through the thickness of the OSB under the wetting system, away from the wetting site, into the cavity air, and diffuses through the OSB and lumber studs into the laboratory. The focus was on the drying portion of this moisture transfer, which occurred after several days of injection, because we were seeking to quantify wall drying. During the injection period, the OSB under the paper towel was charged with liquid water while water also evaporated into the cavity air, increasing the relative humidity and hence further distributing the initial water injected. Primary drying occurred at the outer surface of the OSB as water vapor left the assembly. In most experiments, there was also diffusion through the lumber studs. This diffusion was modeled using the standard one-dimensional steady state diffusion mass flow relationship of Fick’s law [
26], driven by a vapor pressure difference.
Here, Q is the rate of water vapor diffusion (g h−1), A is the surface area (m2), R is the resistance to water vapor diffusion (m2 h Pa g−1), and p is water vapor pressure (Pa). The time units are in hours (h) since the process is slow and the data were acquired on an hourly basis. Values of Q were calculated each hour based on the values of p. Each material was represented by a single vapor resistance value; the typical dependence on relative humidity for hygroscopic materials such as lumber and OSB is not included in the model. The model includes additional effective resistance due to the air layers (Rair) on the inside and outside of the OSB. When exterior insulation was added over the outside of the OSB, this further increased the total resistance to moisture flow by Rxps.
This diffusive flow was modeled as three components, one (Qwet) coming from the wetted area of the OSB directly under the paper towel (Awet) and the second (Qnw) from the rest of the area (Anw) of the rectangular piece of OSB. In the majority of the OSB area (Anw), the vapor driving force is the difference between the vapor pressure in the wall cavity (pcav) and the laboratory (plab). The third flow (Qwood) is constituted by diffusion through the lumber studs, driven by the same pressure difference but with different resistance factors, including wood thickness (Rwood) and, in some experiments, a paint layer (Rpnt).
However, validation of Fick’s law was not our objective. This first simple diffusive model was needed in order to account for water leaving the system. However, the moisture pins respond both to the water leaving the system and to moisture redistribution. Our goal was to provide a simple characterization of this moisture redistribution, suitable for use in a one-dimensional hygrothermal model. We did not use a simple linear model, such as in Fick’s law, to model redistribution away from the wetting area. This transfer presumably includes lateral movement inside the OSB, through both diffusion and capillary action and redistribution inside the cavity through the fiberglass insulation. Instead of directly modeling these flows, an empirical near-exponential decay was used to characterize redistribution, with the starting mass value,
k, set equal to half the initial water mass measured by the moisture pins. This initial mass depends on the wetted area, fixed at 0.157 m
2 to roughly match the rectangular paper towel area. The area of the initially wet OSB is not well defined so the area of the wetted portion was chosen to approximate the paper towel area. Similarly, the moisture content of this area varies by location and is arbitrarily assumed to be represented by the average of moisture pins 1 and 3, which are in the field of the wetted paper towel. The initial water mass used to calculate
k also depends on the density of the OSB, which was measured as 540 kg/m
3. The assumption of near-exponential decay to describe the mass of injected water subject to moisture redistribution will be explored later by comparing other possible simple models, including pure exponential decay. The near exponential function
f(
t) is described in more detail by Whitehead et al. [
27] and is shown in Equation (5) below, with
k as the scale factor (g),
c a dimensionless shape parameter,
τmrd the time constant (h), and
t the time (h).
Both c and τmrd were used as fit parameters in the moisture balance described below to allow the predicted MC inside the wetted region to track the measured values over time. The c value, which must be above 0, determines this function’s proximity to pure exponential decay.
In addition, because the laboratory conditions were not always constant, it was sometimes necessary to model the moisture sorption in the OSB and lumber studs, as the OSB bulk MC and lumber bulk MC changed to reach equilibrium with the room. A simplified method of calculating the moisture transfer from sorption was used by TenWolde [
28] and Boardman and Glass [
29] to model whole building moisture transfer. The model assumes that the material effectively equilibrates with the average relative humidity over its recent past. Here, it is based on the vapor pressure (
plab), but the same exponentially weighted average was used:
where
τsorp is a time constant for sorption (set to 100 h) and
w is a function that applies exponential weighting over the previous 400 h:
so that the rate of moisture transfer from sorption each hour is represented by:
Here,
Rsorp represents the resistance to diffusion in combination with sorption and is another fitting parameter in the moisture balance described in the next section. The full model uses two
Qsorp terms, one for the OSB and the other for the lumber, which have different resistance terms related to paint on the lumber or exterior insulation sometimes covering the OSB, as well as different areas. The time values used for averaging and the sorption time constant are discussed in
Appendix B.
4.2. Moisture Transfer Model for the Whole Wall and for the Water Injection Site
The predicted mass of injected water remaining in the wall assembly,
m, can be compared to the total measured mass at each hour. The predicted total mass at time
ti was based on the mass at the previous hour (
ti−1) and the moisture flows
Q from diffusion and sorption (Equation (8)) for a time step Δ
t set to 1 h:
Similarly, the predicted moisture content for the wetted area,
u, can be compared to the measured moisture content at each hour. This again was based on the previous hour and the moisture flows from outward diffusion (
Qwet), inward diffusion into the insulated cavity (
Qin), redistribution (
Qmrd) within the OSB or the cavity away from the injection site, and sorption (
Qsorp) scaled by the ratio of wetted area to total area (
Awet/
Aosb):
where
ρd,osb is the dry density of OSB (540 kg m
−3) and
Losb is its thickness (11 mm).
The moisture redistribution (Qmrd) is strongly dependent on Equation (5) modeling the mass of water moving out of the wetted area into the surrounding OSB, as well as further net transfer due to redistribution in the air. In those cases where external insulation was added to the OSB, the additional term Rxps was added to Equations (8), (10), and (11).
This model was implemented in a spreadsheet with hourly time steps. The drying simulation began after the final injection, when the MC readings in the OSB reached their maximum; this time was assigned t = 0. The initial moisture content, u(t0), was set to the peak MC measured by the moisture pins. However, the initial value of total mass, m(t0), was allowed to vary somewhat from initial measured mass. When the peak MC was reached and the simulation started, the mass flow was still far from steady state, so there was little chance of matching the predicted and measured m. It took an additional day or two for the mass flows to stabilize, so the starting value, m(t0), was adjusted to minimize the difference between predicted and measured values after the system was closer to steady state. Furthermore, it was not possible to use the mass corresponding to the MC reading because an unknown amount of injected water had already moved outside the wetted area before the model even began, given that the injections happened over multiple days.