2019
DOI: 10.3390/su11195342
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Hygrothermal Properties of Raw Earth Materials: A Literature Review

Abstract: Raw earth historic and contemporary architectures are renowned for their good environmental properties of recyclability and low embodied energy along the production process. Earth massive walls are universally known to be able to regulate indoor thermal and hygroscopic conditions containing energy consumptions, creating comfortable interior spaces with a low carbon footprint. Therefore, earth buildings are de facto green buildings. As a result of this, some earthen technologies have been rediscovered and imple… Show more

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Cited by 79 publications
(47 citation statements)
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“…It can be also seen in Figure 12b that moisture is kept around the beam end for a longer period of time after it penetrates through the surface. It happens due to a high value of the hygroscopic moisture content of the wood (0.0342 m 3 •m −3 , see Table 1), which makes it more capable to absorb and retain moisture. Fungi colonization, mold growth, and wood decay might then appear, especially when the relative humidity is kept above 81% and 90%, respectively [53].…”
Section: Resultsmentioning
confidence: 99%
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“…It can be also seen in Figure 12b that moisture is kept around the beam end for a longer period of time after it penetrates through the surface. It happens due to a high value of the hygroscopic moisture content of the wood (0.0342 m 3 •m −3 , see Table 1), which makes it more capable to absorb and retain moisture. Fungi colonization, mold growth, and wood decay might then appear, especially when the relative humidity is kept above 81% and 90%, respectively [53].…”
Section: Resultsmentioning
confidence: 99%
“…where ρw (kg•m −3 ) is the water density, w (m 3 •m −3 ) is the water content, pv (Pa) is the partial pressure of water vapor in the air, t (s) is the time, Dw (m 2 •s −1 ) is the moisture diffusivity, δp (s) is the water vapor permeability, H (J•m −3 ) is the enthalpy density, T (K) is the temperature, λ (W•m −1 •K −1 ) is the thermal conductivity, Lv (J•kg −1 ) is the latent heat of evaporation of water, and A, B ϵ <0;1> are transition coefficients between the liquid and gaseous phases of water, which give the weight to each phase according to the current moisture content. The model was developed, calibrated, and validated based on experimental results obtained using a laboratory semi-scale experiment.…”
Section: Mathematical Modelmentioning
confidence: 99%
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