1. Introduction
The ratification of the Paris Agreement [
1] entails an obligation for industrialized countries to reduce greenhouse gas emissions. One contribution to meeting this requirement could be the utilization of wood instead of greenhouse gas-intensive building materials. This would result in an increase in demand for wooden construction materials.
In Germany, however, the availability of spruce structural timber from own domestic forests is expected to decline in the long term due to current forest policy. In order to balance various forest interests, the Forest Strategy 2020 [
2] proposes, among other things, the establishment of near-natural mixed forests from native tree species appropriate to the location. Consequently, it can be assumed that the timber industry and the construction industry will adapt to hardwood-based materials.
While the use of solid beech wood in particular poses challenges for the construction industry due to its growth form and high anisotropy, structural wood materials such as laminated veneer lumber (LVL), for which an attenuated anisotropic behavior is promised, could be a promising alternative. The Pollmeier Massivholz GmbH & Co. KG (Creuzburg, Germany) recognized this connection and has been producing LVL from beech (BauBuche). However, comprehensive knowledge of material properties is needed to use laminated beech veneer lumber and other such innovative wood products that present a new class of material in the building sector.
For construction planning, materials need to fulfill minimum requirements, e.g., in terms of structural-physical characteristic values, which are stated in standards. In addition to surpassing these thresholds, the variability of the construction materials plays a crucial part. In this respect, engineered wood products are superior compared to solid wood, due to the homogenization of natural raw material variability. This homogenization is achieved by generating specially designed wood cuttings that are systematically re-connected using synthetic resins [
3]. This decrease in variability is especially beneficial for beech, due to its high anisotropy and large dimensional changes caused by typical moisture changes in buildings.
Technical strength properties for structural calculations are known and given for the commercial product called “BauBuche” (“ConstructionBeech”) within the declarations of product performance (e.g., “PM-005-2018”). Basic behavior in terms of humidity absorption and desorption are to be found in the product data sheets “Structural physics”. Here it is stated that the equilibrium moisture content of BauBuche does not differ significantly from that of other wood species.
Dimensional changes in terms of wood moisture content changes are denoted as the ratio between the rate of change in dimension and the rate of change in wood moisture content. In this context, it is pointed out that the wood moisture content of BauBuche is 6% (±2%) ex works and the material tends to swell and shrink as the wood moisture content changes below the fiber saturation level (approx. 35% wood moisture content). However, details of the moisture-induced dimensional changes are missing. It is unclear, for example, whether the material behaves like solid wood or whether the manufacturing process leads to specific swelling and shrinkage behavior when absorbing and releasing moisture, with effects on the strength properties in extreme cases.
Therefore, it was the intention of the present study to investigate the behavior of LVL made from beech in terms of humidity absorption and desorption. This was done by applying a manual testing procedure (climatic chamber, balance and caliper) as well as with a dynamic vapor sorption analyzer equipped with a camera. Finally, on the basis of the results, practical advice on the proper use of BauBuche in the building sector is given.
3. Results
According to the set rules (IQR method), extreme outliers in moisture content and dimensional change were found for the data of the manual test method: eight for test specimens of cubic dimensions within the Adsorption Sequence, one for test specimens of flat dimensions within the adsorption sequence. More detailed information is to be found in the attached files (
Supplementary Information).
Table 1 lists the mean value and the coefficient of variation for moisture content and dimensional change of the flat and cubic test specimens after application of the manual test method for each climatic condition of the Absorption Sequence and the Desorption Sequence. Although no differences were found between the flat and cubic test specimens when simply viewing the data in
Table 1; the statistical mean value comparison shows that a large number (6 of 20 Ad. Sq, 8 of 20 De. Sq.) of significant differences were found. This means that the two types of specimens cannot be combined into one data set. Therefore, only the flat test specimens are considered in the following, since a more reliable conditioning can be assumed due to the smaller dimensions, and thus, shorter distances for moisture to enter the test specimen. This assumption is supported by the fact that the initial moisture content (at 20 °C and 65% r. h.) in the Desorption Sequence of the cubic test specimens (9.7%) is (significantly) lower than that of the flat test specimens (10.7%). Irrespective of the results of the statistical investigation, all data points in the plot would have matched well, except for the initial moisture content of the desorption sequence.
The data of the gravimetric vapor sorption analyzer are displayed in
Table 2. Due to the test setup, only single measured values are given here, i.e., without indication of the variance, since only one test specimen per material was finally examined. The results are in good agreement with the study of Nopens et al. [
5].
Figure 3 shows the course of wood moisture development over the relative humidity at constant temperature (20 °C) when passing through the absorption and desorption sequences. In partial figure a, the course of wood moisture development of the flat test specimens in manual test procedure is graphically evaluated by plotting against the relative humidity separately for the Absorption Sequence and the Desorption Sequence.
Figure 3b shows the course of the wood moisture development of the LVL and solid wood test specimens in the gravimetric vapor sorption analyzer with at first decreasing, and then increasing, humidity. For both the manual test procedure and the gravimetric vapor sorption analyzer examination, roughly seen the typical sigmoidal form of the isotherms can be recognized and a hysteresis is to be observed between moisture absorption and desorption. In particular, it can be seen from
Figure 3a that in the case of the LVL test specimens, these are scanning isotherms, as will be explained later in the discussion. At the beginning of both, the Absorption Sequence and the Desorption Sequence is located at 65% r. h. and thus lies undefined within the absorption or desorption process. This can be seen from the fact that the starting point is below the end point of the Absorption Sequence and above the end point of the Desorption Sequence. The lack of water saturation in the case of the LVL test specimen at gravimetric vapor sorption analyzer test procedure can be seen from the lower wood moisture content compared to the solid wood test specimen measured at the first climate stage (20 °C and 85% r. h.). Apart from this, the course of the wood moisture corresponds largely to that of the solid wood test specimen.
Figure 4 shows the course of dimensional change development over the relative humidity at constant temperature (20 °C) when passing through the absorption and desorption sequences. In partial figures a and c, the course of dimensional change development is shown for the flat test specimens at manual test procedure by plotting against the relative humidity separately for the Absorption Sequence and the Desorption Sequence.
Figure 4a shows the course of development in radial direction,
Figure 4c shows the tangential direction.
Figure 4b,c show the same topics for the test specimens at gravimetric vapor sortion analyzer test procedure. For both the manual test procedure and the gravimetric vapor sorption analyzer examination, roughly seen the typical sigmoidal form of the isotherms can be recognized and a hysteresis is to be observed between moisture absorption and desorption.
While the swelling isotherms are similar in principal, the results from dimensional change in radial direction of manual test procedure show in detail a clear difference to all others. The first moisture increase over the state at the end of production (started recording after initial conditioning at 20 °C and 65% r. h.) causes a strong increase of the radial dimension. It is noticeable in this context that the dimension after re-drying in the initial climate (20 °C and 65% r. h.) is considerably higher than the initial dimension, even taking into account the expected hysteresis. On the one hand, this can be seen from the clearly lower starting point (and the following one) of the Absorption Sequence in
Figure 4a compared to that of the dimensional change in tangential direction in
Figure 4c. In numbers, this can be traced in
Table 1 for both, flat and cubic test specimens, comparing the initial value
dcrad (0.4% or 1.8%) with the final (4.7%) respectively. In actual dimensions of the flat test pieces, this means a difference of nominal 2.5 mm (50.5 mm [±0%], initial vs. 52.7 mm [±1%], final), while in the tangential direction the initial dimension (20.2 mm [±1%]) barely deviates from the final dimension (20.4 mm [±1%]). In conclusion, this means that during first moisture increase over the state at the end of production, an irreversible dimensional increase occurs in radial direction.
Due to the different test setup of the gravimetric vapor sortion analyzer test procedure, it can be seen in
Figure 4b,d that the LVL test specimen behaves similarly to natural solid wood (or LVL in tangential direction,
Figure 4c) after the irreversible dimensional increase has taken place also in radial direction. The untypical appearance of the desorption isotherm at the beginning of its course (crossing with the absorption isotherm) is due to incomplete water saturation before the start of the experiment.
Figure 4b,d also shows that the swelling anisotropy typical of solid wood is almost non-existent for LVL. Although the swelling of LVL in the radial direction is slightly above that of solid wood, the swelling in tangential direction is considerably below that of solid wood. Both, the swelling of LVL in radial direction and that in tangential direction are approximately equal. This means that the material has been improved compared to solid wood.
Figure 5 shows the course of dimensional change development over the wood moisture content when passing through the absorption and desorption sequences. In partial figures a and c, the course of dimensional change development is shown for the flat test specimens in manual test procedure by plotting against the wood moisture content separately for the Absorption Sequence and the Desorption Sequence.
Figure 5a shows the course of development in radial direction,
Figure 5c shows the course of development in tangential direction.
Figure 5b,c shows the same topics for the test specimens at gravimetric vapor sortion analyzer test procedure (LVL and solid wood both).
Except for the Absorption Sequence in
Figure 5a, absorption and desorption is linear (lines are close together), independent of method (manual test procedure, gravimetric vapor sorption analyzer) and material (LVL, solid wood). The different behavior of the LVL in the absorption sequence clearly reflects the irreversible swelling during first moisture increase over the state of that at the end of production as described above. Furthermore,
Figure 5 clearly shows that, regardless of the direction, LVL remains the same as solid wood in the radial direction.
Table 3 lists the initial data and the results of the calculation of differential swelling determined by the manual test procedure according to the approach proposed in DIN 52184. In radial direction, the differential swelling accounts for 0.41%/%, in tangential direction for a range of 0.38 to 0.47%/% (mean 0.44%/%) and in longitudinal direction for 0.01%/%. In the course of calculating the differential swelling in the form of the slope of the regression line, the following values were obtained: 0.42%/% (radial), 0.47%/% (tangential), and 0.01%/% (longitudinal). The corresponding measures of determination were 1.00 (radial and tangential) and 0.95 (longitudinal).
Table 4 lists the results of the calculation of differential swelling at the first moisture increase over the state at the end of production according to the approach proposed in DIN 52184. In radial direction, the differential swelling accounts to a value range of 0.59 to 0.60%/% (mean 0.59%/%).
4. Discussion
When plotting the test specimen wood moisture content or dimensional change against the relative air humidity at constant temperature, a sorption or swelling isotherm is obtained. However, since only the solid wood test specimen had been immersed in distilled water before the experiment was started (fully saturated with water), so that a real isotherm was obtained, the other graphs were scanning isotherms according to Fredriksson and Thybring [
7]. This can be seen prominently by crossing desorption and absorption isotherms in
Figure 5b,d for LVL samples. The beginning of the experiment was made within the hysteresis, and the real course of the isotherm is only described in the course of the re-moistening after passing through the dry stage. The begin of the isotherms within the hysteresis becomes obvious in
Figure 3a where both the Adsorption Sequence and the Desorption Sequence start for 65% relative air humidity, and thus, the starting point is located between re-desorption and re-adsorption scanning isotherms. Apart from the described limitations due to the use of test specimens without prior water storage, the sorption isotherms follow in principal the typical sigmoidal shape with hysteresis between sorption and desorption. With the gravimetric sorption analyzer, only one sample was measured for beech and LVL respectively. The general deviation of the measuring principle is low [
5]. Values for beech are in close agreement with the first presented data [
5]. However, every natural material, as well as compound materials like LVL exhibit deviations within the structure. Therefore the presented values are a strong indication for the general swelling and shrinking behavior related to relative humidity and moisture content. Especially as they agree well with the manual test procedure. However, further investigations with more samples cut at different positions within the raw material (beech and Baubuche) could improve and strengthen the significance of the presented research in the future.
The sorption isotherm of the solid wood test specimen examined in the gravimetric vapor sorption analyzer follows that reported in literature [
8] and found within previous investigations [
5]. Although the desorption of the LVL test specimen in the gravimetric vapor sorption analyzer was started in an unsaturated state, both the desorption and adsorption curves correspond to those of solid beech wood. Results of the manual test procedure are within the hysteresis region of the gravimetric vapor sorption analyzer data. Therefore, both methods support each other in the presented results and prove the results for both materials in general.
The swelling isotherms of the solid wood test specimen examined in the gravimetric vapor sorption analyzer follow that reported in literature [
8] and found within previous investigations [
5]. In general, the swelling isotherms from manual test procedure are similar to that of gravimetric vapor sorption analyzer examination, though in detail they show differences. The reason for this is presumably the different pre-states of climate between both methods. At manual test procedure, the test specimens were investigated within an absorption and desorption sequence, both started at 65% relative humidity and dried or remoistened respectively after running through the sequence. In contrast, in the case of the gravimetric vapor sorption analyzer examination, the tests were started at 85% relative air humidity and water saturated samples were used in the case of solid wood samples. Absorption was performed after reaching zero percent relative humidity. A direct comparison of the results of both methods is therefore not possible. Comparing the swelling isotherms of LVL and solid wood determined using the gravimetric vapor sorption analyzer, it is noticeable that the radial swelling of LVL exceeds that of solid wood. For the tangential direction, the behavior is reversed. A material-related peculiarity for the examined LVL can be observed when considering the swelling isotherm in radial direction for the manual test procedure. The swelling state at the beginning of the absorption sequence is significantly below that which can be expected on the basis of the data of the desorption sequence. The reason for this could be a densification of the wood substance in the radial material direction during the manufacturing process. During the production of the material, the veneer layers are coated with phenolic adhesive, which is then cured under pressure in a hot press. The wood compaction that takes place during this process is released in the course of subsequent swelling and can be observed as a spring back effect, i.e., irreversible swelling. While calculation methods lead to nominally low swelling in the radial direction at the beginning of the absorption sequence, it becomes clear that an unusually strong swelling of the material occurs here due to the irreversible spring back of the material (nominally approx. 2 mm per 50 mm, i.e., 4%) and the method of swelling calculation (dividing the measured data by the respective dimension after final oven drying). This could be illustrated if the curve of the absorption sequence were shifted in parallel in such a way that the starting point of the absorption sequence coincides with the end point of the desorption sequence. This approach makes clear why unusually high swelling of the material is observed during the absorption sequence. After release of the production-related compaction stored in the material, a normal swelling and shrinkage behavior of the material can be assumed. Furthermore, the swelling in the radial direction after release of the production-related compression equals the swelling in the tangential direction. Regardless of spring back, LVL shows a lower swelling anisotropy than solid wood. The radial and tangential swelling of LVL are in a similar range and are more similar to the radial swelling of solid wood.
From the results of the present study, the following recommendations can be made for the practical application of LVL in the construction sector. If BauBuche is installed in the factory condition (moisture content of 6% ± 2%), strong radial swelling must be expected during initial moisture absorption due to the spring back effect. In order to avoid this strong initial swelling in the installed state, it would be advisable to carry out initial moistening and subsequent conditioning during the production process. Ideally, after primary swelling, the LVL should be conditioned to the equilibrium moisture content expected in the area of application. In this state, LVL shows a lower swelling anisotropy than solid wood and is therefore more suitable for use in the construction sector. However, initial moistening and subsequent conditioning in the LVL production process would be very time-consuming and require large storage capacities. Consequently, it might be more realistic to take into account the strong initial radial swelling in component planning and dimensioning in order to avoid damage to building structures.