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dc.contributor.authorFeilke, Thorben
dc.contributor.authorZimmer, Katrin
dc.contributor.authorFromm, Jana
dc.contributor.authorLarnøy, Erik
dc.date.accessioned2020-08-20T08:08:09Z
dc.date.available2020-08-20T08:08:09Z
dc.date.created2017-10-17T15:32:14Z
dc.date.issued2011
dc.identifier.isbn9788231101390
dc.identifier.urihttps://hdl.handle.net/11250/2673119
dc.description.abstractWood as a hygroscopic material gains or loses moisture with changes in climate of the surrounding air. The moisture content influences strength properties, hardness, durability and machinability. Therefore the hygroscopicity is a very important property, last but not least for economic factors. Below fibre saturation, a change in moisture content causes shrinkage or swelling and anisotropic behaviour can be seen in the different growth directions. For a better understanding of the sorption behaviour of Scots pine (Pinus sylvestris L.) the variation between different adsorption and desorption curves has been investigated. Trees from 25 different sites in Northern Europe were collected and 3651 samples (1510 heartwood- and 2141 sapwood-samples) measuring 5 (T) x 10 (R) x 30 (L) mm were obtained. The sorption isotherms for all specimens were measured at 25 °C at relative humidities of 15, 35, 55, 75 and 95 % for both desorption and adsorption. The aim of this study is to investigate the influence of raw material variability on the sorption behaviour of Scots pine. Due to the different growing conditions, densities and wooden material (heart or sapwood) variations within the sample groups have been found. Correlations between moisture and density respectively latitude were investigated.
dc.language.isoeng
dc.relation.ispartofProceedings of the 7th meeting of the NORDIC-BALTIC NETWORK IN WOOD MATERIAL SCIENCE & ENGINEERING (WSE)
dc.titleSorption behaviour of Scots pine in Northern Europe
dc.typeChapter
dc.description.versionpublishedVersion
dc.source.pagenumber131-136
dc.identifier.cristin1505296
cristin.ispublishedtrue
cristin.fulltextoriginal


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