2011
DOI: 10.1016/j.conbuildmat.2010.06.069
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Water vapor properties of two hemp wools manufactured with different treatments

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Cited by 44 publications
(22 citation statements)
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“…Moisture flow is a function of hygroscopic capacity, vapour permeability and rate of air flow. Since the vapour permeability of both insulations is similar, as also observed by Collet et al [30], and the cooler sides of the insulations were airtight, the managed response of Hemp insulation can mainly be attributed to its higher moisture adsorption capacity and to a limited extent to its relatively lower air permeability.…”
Section: Fig 7 Internal Surface Temperatures Of the Acrylic And Thesupporting
confidence: 75%
“…Moisture flow is a function of hygroscopic capacity, vapour permeability and rate of air flow. Since the vapour permeability of both insulations is similar, as also observed by Collet et al [30], and the cooler sides of the insulations were airtight, the managed response of Hemp insulation can mainly be attributed to its higher moisture adsorption capacity and to a limited extent to its relatively lower air permeability.…”
Section: Fig 7 Internal Surface Temperatures Of the Acrylic And Thesupporting
confidence: 75%
“…At lower relative humidity, 0-15% according to Hill, Norton and Newman [6] and 5-35% according to Collet et al [7], water molecules are adsorbed in a monolayer (solid solution) on to the internal surfaces of the cell wall. Multi-molecular layers of water are formed on the cell wall micro-capillaries at a relative humidity varying between 15% and 70%, while capillary condensation occurs at further higher relative humidity ranges.…”
Section: Adsorption-desorption Isothermmentioning
confidence: 99%
“…The GAB equation has been chosen for its higher coverage of activity range for monolayer sorption values (0.05<φ<0.8-0.9) [7] compared to that of BET equation…”
Section: Analysis Of Adsorption-desorption Isothermmentioning
confidence: 99%
“…Hygrothermal materials include natural fibres (Collet et al 2011), timber (Ku¨nzel et al 2004), earth and clays (D'Orazio andQuagliarini 2009, Hall and, natural and synthetic zeolites (Feng and Peng 2005), silica gels (La et al 2010) and molecular sieves (Dieng and Wang 2001). The limitations of these materials are that they have predefined microstructural characteristics resulting in set levels of heat and moisture uptake and storage.…”
Section: Introductionmentioning
confidence: 98%