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Article

Modelling the Material Resistance of Wood—Part 1: Utilizing Durability Test Data Based on Different Reference Wood Species

1
Norwegian Institute of Bioeconomy Research (NIBIO), Division of Forestry and Forest Resources, Wood Technology, Høgskoleveien 8, NO-1433 Ås, Norway
2
Wood Biology and Wood Products, University of Goettingen, D-37077 Goettingen, Germany
3
Department of Wood Science and Technology, Biotechnical Faculty, University of Ljubljana, SI-1000 Ljubljana, Slovenia
*
Author to whom correspondence should be addressed.
Forests 2021, 12(5), 558; https://doi.org/10.3390/f12050558
Submission received: 30 March 2021 / Revised: 23 April 2021 / Accepted: 23 April 2021 / Published: 29 April 2021
(This article belongs to the Special Issue Modeling the Performance of Wood and Wood Products)

Abstract

:
To evaluate the performance of new wood-based products, reference wood species with known performances are included in laboratory and field trials. However, different wood species vary in their durability performance, and there will also be a within-species variation. The primary aim of this paper was to compare the material resistance against decay fungi and moisture performance of three European reference wood species, i.e., Scots pine sapwood (Pinus sylvestris), Norway spruce (Picea abies), and European beech (Fagus sylvatica). Wood material was collected from 43 locations all over Europe and exposed to brown rot (Rhodonia placenta), white rot (Trametes versicolor) or soft rot fungi. In addition, five different moisture performance characteristics were analyzed. The main results were the two factors accounting for the wetting ability (kwa) and the inherent protective properties of wood (kinh), factors for conversion between Norway spruce vs. Scots pine sapwood or European beech for the three decay types and four moisture tests, and material resistance dose (DRd) per wood species. The data illustrate that the differences between the three European reference wood species were minor, both with regard to decay and moisture performance. The results also highlight the importance of defined boundaries for density and annual ring width when comparing materials within and between experiments. It was concluded that with the factors obtained, existing, and future test data, where only one or two of the mentioned reference species were used, can be transferred to models and prediction tools that use another of the reference species.

1. Introduction

Robust integrated performance classification of wood products and structures is based on the whole set of external parameters—the foundation established for decay, material and integrity aspects, aesthetic limits and performance, and termite/insect performance aspects. The European ForestValue research project CLICKdesign brings together into a unique single software tool diverse models and performance databases associated with decay and integrity, aesthetic function, and termite performance [1]. The basis for predicting service life and decay of wood is a set of dose-response models accounting for exposure and resistance, both expressed as dosage [2] and following well-established engineering principles [3], Equation (1):
E x p o s u r e   d o s e   D E d   R e s i s t a n c e   d o s e   D R d
For predicting the field performance of wood-based materials, the material resistance dose (DRd) needs to be determined to verify the design condition according to Equation (1). The resistance dose DRd is considered to be the product of a critical dose (Dcrit) and two modifying factors considering the wetting ability of wood (kwa) and its inherent durability (kinh). The approach to do this is, according to [4], Equation (2):
D R d = D c r i t × k w a × k i n h   [ d ]
where:
  • DRd is the material resistance dose [d];
  • Dcrit is the critical dose [d] corresponding to decay rating 1 (EN 252 [5]);
  • kwa is a factor accounting for the wetting ability of the material [-] relative to a reference wood species;
  • kinh is a factor accounting for the inherent protective properties of the material against decay [-] relative to a reference wood species.
The critical dose Dcrit was evaluated for Scots pine sapwood (Pinus sylvestris) and Douglas-fir heartwood (Pseudotsuga menziesii) according to [4] based on long-term field tests using horizontal above-ground, double-layer set-ups, which had been exposed and monitored at 25 different locations in Europe [6]. It was found that Dcrit corresponding to decay rating 1, i.e., ‘slight decay’, can be seen as more or less independent from the wood species. Instead, differences between species and/or treatments can be accounted for by defining differences in moisture uptake and decay inhibiting properties. For the two wood species, Dcrit was found to be around 325 days with favorable conditions for fungal decay [4].
Meyer-Veltrup et al. [7] further developed and optimized this model considering the resistance of wood against brown, white and soft rot, as well as relevant types of water uptake and release. They determined factors kwa and kinh for a wide variety of different wood species and modified wood. Furthermore, the model was validated using data from laboratory and field tests [7,8,9]. Norway spruce was chosen as reference material, having low amounts of extractives and low durability, but is frequently used outdoors all over Europe.
The approach for modelling the material resistance based on moisture performance and material-intrinsic properties is promising and has been validated for a wide range of different wood species. However, robust data are lacking, especially for preservative-treated wood. Additionally, data on modified, water repellant-treated, and coated wood are sparse. The lack of data is caused by the variety of non-durable reference species used in the standard tests and the different prediction models. This variety also causes statistical uncertainty when analyzing existing data from previous durability tests. Prediction models often used Norway spruce, but the standard reference species in European test protocols, e.g., [5,10] are Scots pine sapwood for softwoods and European beech (Fagus sylvatica) for hardwoods. In Australia and New Zealand, the AWPC protocol [11] is quite open regarding reference species “The timber species shall be softwood or hardwood and representative of the country or region of proposed end-use”. Radiata pine (Pinus radiata) is a commonly used softwood, Tasmanian oak (a species mix of Eucalyptus regnans, Eucalyptus obliqua or Eucalyptus delegatensis) is a commonly used hardwood. For laboratory testing in New Zealand, Radiata pine is used as reference species against brown rot fungi and European beech against white rot fungi. In Australia, low durability sapwood references in laboratory tests include Southern pine sapwood (e.g., Pinus elliottii, Pinus caribaea, P. elliottii x P. caribaea hybrid) or Radiata pine sapwood. In the US, the field in-ground tests for stakes [12] and posts [13] use sapwood of Southern pine (Pinus elliottii, P. echinata, P. palustris, P. taeda, P. serotina, P. virginiana, P. glabra) as a reference while the above-ground L-joint test [14] uses sapwood of Ponderosa pine (Pinus ponderosa) and the horizontal lap-joint method [15] uses sapwood of Pinus spp. or “other softwood species shall be used and defined”. The laboratory soil-block test [16] lists non-durable softwood such as Southern pine (Pinus spp.) for softwood, and sapwood from a non-durable, medium-density hardwood such as Sweetgum (Liquidambar styraciflua) or Yellow-poplar (Liriodendron tulipifera) for hardwood test blocks. However, neither of these species is easy to treat and are sometimes substituted with Aspen. The standard for evaluation of natural decay resistance using laboratory decay tests [17] lists as references “Pine sapwood (Pinus sp.) (…)or some other softwood of comparably low resistance should be prepared if a softwood species or product is being tested. Other materials include sapwood of fir, (Abies sp.), spruce (Picea sp.) or hemlock (Tsuga sp.). If broadleaf species (hardwoods) are evaluated (…) sapwood of sweetgum (Liquidambar sp.) or other low durability species shall be prepared. Potential hardwood species include beech (Fagus sp.), birch (Betula sp.) or maple (Acer sp.)”. In the laboratory soil bed test [18], Birch (Betula papyrifera) is the preferred hardwood species, and Southern pine (Pinus spp.) or Ponderosa pine (Pinus ponderosa) are the preferred softwood species. In Thailand, rubberwood (Hevea brasiliensis) and Red gum (Eucalyptus camaldulensis) are used as a reference in laboratory tests. According to Japanese Industrial Standards (JIS), the sapwood of the softwood Sugi (Cryptomeria japonica) is the standard reference species for both field trials and fungal laboratory tests with brown rot (Fomitopsis palustris) and white rot (Trametes versicolor), as well as termites (Coptotermes formosanus). Some, but not all, of the standards listed above provide guidance regarding the range of annual ring width for test specimens. The European standards recommend 2.5–8 rings per 10 mm, e.g., [5,10] while the American standards tend to have a narrower range, 2–4 rings per 10 mm e.g., [12,16].
In this study, the aims were to: 1. compare the material resistance and moisture performance of the three European reference wood species (Norway spruce, European beech and Scots pine sapwood) with conversion factors as the primary output (this paper), 2. collecting data from durability tests for validating and optimizing the ‘Meyer-Veltrup model’ for material-resistance [7] and Part 2 of this publication [19], and 3. surveying wood durability test data, utilize them for implementation in a material resistance model, and generate a database for service life prediction of wood products in above and in-ground situations, Part 3 of this publication [20].

2. Materials and Methods

2.1. Wood Specimens

Small clear specimens (free from defects such as cracks, decay, and discoloration) from Norway spruce (Picea abies), Scots pine (Pinus sylvestris) sapwood, and European beech (Fagus sylvatica) were used for fungal decay tests and moisture performance tests. The sample dimensions used in the different tests are referred to in the respective Section 2.2, Section 2.3 and Section 2.4. The wood materials were provided by different research institutions and industry partners, plus frozen Scots pine sapwood material from Zimmer et al. [21]. The material included 43 locations in 11 different European countries, as summarized in Table 1. Due to logistic issues, less material was exposed to capillary water uptake (CWU) than to 24 h water uptake and release tests (W24) and cell wall saturation (EMC~100%RH).
Annual ring width (ARW), initial oven-dry mass, and volume were recorded for specimens used in the fungal decay tests, and initial oven-dry density (ρ0) was calculated.

2.2. Decay Tests with Pure Basidiomycete Cultures

Laboratory decay resistance tests were conducted according to a modified EN 113-2 [10] protocol as follows: in total, 1543 specimens (Table 1), 15 × 25 × 50 (ax.) mm3, were oven-dried at 103 ± 2 °C for 48 h, weighed to the nearest 0.001 g, and afterwards conditioned at 20 °C/65% relative humidity (RH) until constant mass. After sterilization in an autoclave at 121 °C and 0.24 MPa for 20 min, two specimens of the same species were placed on fungal mycelium in a Kolle flask. To avoid direct contact between wood and overgrown malt agar (4%), stainless steel washers were used. The incubation time was 16 weeks. Rhodonia placenta (Fr.) Niemelä, K.H. Larss. and Schigel (strain FPRL 280) and Trametes versicolor (L.) Lloyd (strain CTB 863A) were used as test fungi. After incubation, the specimens were cleaned from adhering mycelium, weighed to the nearest 0.001 g, and oven-dry mass loss (MLf) was calculated according to Equation (3):
M L f = m 0 , i m 0 , f m 0 , i   ×   100   [ % ]
where:
  • m0,i is the oven-dry mass before incubation (g);
  • m0,f is the oven-dry mass after incubation (g).

2.3. Decay Tests in Terrestrial Microcosms (TMCs)

Terrestrial microcosms (TMCs), in accordance with CEN/TS 15083-2 [22], were utilized in semi-field experiments. The soil moisture content (MCsoil) was equal to 95% of the soil-water holding capacity (WHCsoil), and the test was conducted in a dark, climate-controlled room set to a temperature of 27 °C and 65% RH. Wood specimens of 5 × 10 × 100 (ax.) mm3, a total of 1028, were buried 4/5 of their length into the soil substrate with 58 specimens per TMC box. The incubation time was 16 weeks. The MLf was calculated according to Equation (3). Details about the soil preparation are provided below.

2.3.1. Soil Substrates

The basis of the substrate was a horticultural compost produced at the forest botanical garden at the University of Göttingen’s North Campus. The compost comprised of fallen leaves and cuttings from grass and trees. Soil was passed through a sieve with nominal aperture size of 8.5 mm. WHCsoil was then determined according to the ‘cylinder sand bath method’ according to ISO 11268-2 [23]. Silica sand (0–0.2 mm grain size) was added to lower the WHCsoil of the pure compost substrate and deliver a soil mixture with WHCsoil of 60%.

2.3.2. Determination of the Soil Moisture Content (MCsoil)

Soil samples of 50–90 g (depending on the soil density) were taken for determining the MCsoil. Three replicate samples were taken, weighed to the nearest 0.01 g, oven-dried at 103 °C for 24 h, and weighed again. MCsoil was calculated according to Equation (4):
M C s o i l = m w m 0 m 0   ×   100
where:
  • M C s o i l is the soil moisture content (%);
  • m w is the wet soil mass (g);
  • m 0 is the oven-dry soil mass (g).

2.3.3. Determination of the Soil-Water Holding Capacity (WHCsoil)

Soil was inserted into hollow polyethylene cylinders 10 cm long with 4 cm diameter. The bottoms of the cylinders were covered with a fine polymer grid and filter paper (MN 640 W 70 mm). All cylinders were filled with soil to a height of 5–7 cm and saturated in an 8 cm high water bath for 3 h. After the saturation period, the cylinders were placed on a water saturated sand bath for 2 h to allow unbound water within the soil-filled cylinders to drain to reach the equivalent of field capacity. The soil samples were then weighed wet, as well as after oven-drying at 103 ± 2 °C for 24 h. WHCsoil (%) was calculated according to Equation (5):
W H C s o i l = m s m 0 m 0   ×   100
where:
  • W H C s o i l is the soil water-holding capacity (%);
  • m s is the saturated soil mass (g);
  • m 0 is the oven-dry soil mass (g).

2.3.4. Preparation of Mixed Soil Substrate

To mix the different soil substrates of compost and sand to the predetermined WHCsoil of 60%, the WHCsoil of soils mixed in incremental ratios based on oven-dry mass was first determined.
Table 2 below shows the incremental soil mixtures used to establish a WHCsoil regression equation for the substrates sand and compost. To prepare mixed soil substrates for testing WHCsoil, Equation (6) below was used.
m x , w e t =   m t o t a l , d r y   ×   x 100   ×   1 +   M C x 100
where:
  • m x ,   w e t is the mass of the wet substrate x (g);
  • m t o t a l ,   d r y is the oven-dry mass of the total soil mixture (g);
  • x is the fraction of the substrate (sand or compost) in the total soil mixture m t o t a l ,   d r y based on oven-dry mass (%);
  • M C x is the moisture content of the soil substrate x (%).
A regression between the incremental mixing ratios of the two substrates sand and compost and their resulting WHCsoil was determined. Equation (7) below shows the regression relationship for WHCsoil of the two substrates used to define the mixture percentages to attain a mixed soil substrate with WHCsoil 60%. Table 2 below shows the output from computations using Equation (7).
W H C s o i l = 0.7 x + 30
where:
  • W H C s o i l is the target water-holding capacity of the soil mixture (%);
  • x is the fraction of pure compost substrate in the total soil mixture based on oven-dry mass (%).

2.3.5. Preparation of Mixed Soil to Reach Target Soil Moisture Content (MCsoil,target)

A soil mixture with WHCsoil of 60% was attained in a ratio of 43% compost to 57% silica sand, weighing a total of 8500 g (based on oven-dry mass). Then, in accordance with CEN/TS 15083-2 [22], distilled water was added to the soil mixture to reach MCsoil equal to 95%WHCsoil, shown here as the target soil moisture content (MCsoil,target) of 57%. Equation (8) below was used to calculate the mass (g) of distilled water required to add to the soil mixture to reach MCsoil,target of 57%. To account for losses in MCsoil resulting from fungal activity and evaporation, rewetting to MCsoil,target occurred once per week throughout the 16-week incubation period.
m w a t e r = M C s o i l , t a r g e t M C s o i l , c u r r e n t 100   ×   m t o t a l ,   d r y
where:
  • m w a t e r is the mass of distilled water to add to the soil mixture (g);
  • M C s o i l , t a r g e t is the target soil moisture content (%);
  • M C s o i l , c u r r e n t is the current moisture content of the soil mixture before adding additional water (%);
  • m t o t a l ,   d r y is the oven-dry mass of the total soil mixture (g).

2.4. W24-Tests (24 h Water Uptake and Release Tests)

For all three W24-tests (Section 2.4.1, Section 2.4.2 and Section 2.4.3), the same specimens, a total of 672 (Table 1), were used. The specimen dimension was 5 × 10 × 100 (ax.) mm3.

2.4.1. Liquid Water Uptake by Submersion (LWU)

The specimens were oven-dried at 103 °C until constant mass. The oven-dry mass was determined to the nearest 0.001 g. Oven-dry specimens were submerged in a sealed plastic container with demineralized water and placed in a climate chamber at 20 °C/65% RH. Specimens were separated from each other by square-shaped stainless steel meshes. The specimens were weighed again after 24 h submersion. The liquid water uptake (LWU) of the specimens was determined according to Equation (9):
L W U = m s u b m 0 m 0   ×   100   [ % ]
where:
  • LWU is the liquid water uptake during 24 h submersion (%);
  • m0 is the oven-dry mass before submersion (g);
  • msub is the mass after 24 h submersion (g).

2.4.2. Water Vapor Uptake in Water-Saturated Atmosphere (VU)

The specimens were oven-dried at 103 °C until constant mass. The oven-dry mass was determined to the nearest 0.001 g. The bottom of a miniature climate chamber (sealed plastic container with stainless steel perforated plates) was filled with 5 L of demineralized water. Specimens were placed with approx. 5 mm distance between each other on stainless-steel plates above the water. The containers were stored in a climate chamber (20 °C/65% RH), and specimens weighed again after 24 h. The water vapor uptake (VU) of the specimens was determined according to Equation (10):
V U = m 100 % R H m 0 m 0   ×   100   [ % ]
where:
  • VU is the water vapor uptake during 24 h exposure above water (%);
  • m0 is the oven-dry mass before submersion (g);
  • m100%RH is the mass after 24 h exposure above water (g).

2.4.3. Desorption (VR)

Specimens were stored in sealed containers above water at 20 °C (approximately 100% RH) until constant mass. The mass at approximate cell wall saturation (EMC~100%RH) was determined to the nearest 0.001 g. Specimens were exposed directly on freshly activated silica gel in sealed boxes (0% RH) and weighed again after 24 h. The water vapor release (desorption) of the specimens during 24 h was determined and expressed as a relative value of the mass at EMC~100%RH (Equation (11)):
V R = E M C ~ 100 % R H m 0 % R H E M C ~ 100 % R H     ×   100 [ % ]
where:
  • VR is the water vapor release during 24 h exposure at 0% RH (%)
  • EMC~100%RH is the mass at cell wall saturation (g)
  • m0%RH is the mass after 24 h exposure to 0% RH (g)

2.4.4. Capillary Water Uptake (CWU)

Short-term water absorption was measured using a Krüss Processor Tensiometer K100MK2 (Krüss GmbH, Hamburg, Germany). A total of 508 specimens (Table 1) with the dimensions 60 (ax.) × 10 × 5 mm3 (wood material from Germany), 100 (ax.) × 10 × 5 mm3 (Scots pine sapwood from [21]) or 30 (ax.) × 10 × 5 mm3 (wood material from the remaining locations) were stored at 20 °C/65% RH until a constant mass was reached (m65%RH). For the capillary water uptake tests, the axial specimen surfaces (10 × 5 mm2) were fixed in the tensiometer and positioned to be in contact with water (end-grain uptake). The specimen’s mass was recorded after 200 s. The CWU was determined over time and related to the cross-sectional area of the specimens (Equation (12):
C W U = m 200 s m 65 % R H A   [ g / cm 2 ]
where:
  • CWU is the capillary water uptake during 200 s (g/cm2);
  • m200s is the mass after 200 s in contact with water (g);
  • m65%RH is the mass at 20 °C/65% RH (g);
  • A = axial specimen surface.

2.5. Statistical Analyses

The Tukey–Kramer HSD (honestly significant difference) test was used to compare means (JMP Pro 14, SAS Institute Inc., Cary, NC, USA) on a 5% level of significance, due to the unequal sample sizes. Linear regression models (Equation (13)) were used to study the influence of initial oven-dry density (ρ0), annual ring width, and an interaction term of the latter on different combinations of wood species and decay fungus (Equations (13a)–(13d)). Variables with p-values < 5% were considered significant.
Y i = f X i , β + e i
where:
  • Y i is the response;
  • f is the function;
  • X i is the independent variable;
  • β are the unknown parameters;
  • e i are the error terms.
(13a) M o d e l   1 M L f = β 0 + β 1 ρ 0 + e 1 (13b) M o d e l   2 M L f = β 0 + β 1 A R W + e 1 (13c) M o d e l   3 M L f = β 0 + β 1 ρ 0 + β 2 A R W + e 1 (13d) M o d e l   4 M L f = β 0 + β 1 ρ 0 + β 2 A R W + β 3 ρ 0 × A R W + e 1
where:
  • MLf (mass loss) is the response;
  • β 0 is the population intercept;
  • β i is the population slope coefficient;
  • ρ0 is the initial oven-dry density;
  • ARW is the annual ring width;
  • e 1 are the error terms.

3. Results and Discussion

3.1. Wood Species Level

The total mean mass loss (MLf) for the three fungal decay tests and the characteristics for the four moisture performance tests (LWU, VU VR, CWU) are summarized in Table 3.
Table 3 also provides the main findings of this study, i.e.,: (1) the factors kinh and kwa, (2) factors for conversion between Norway spruce vs. Scots pine sapwood or European beech for the three decay types and four moisture tests, and (3) the material resistance dose DRd per wood species. The results illustrate that the difference in performance between the three reference wood species is small.
When comparing mean MLf between decay fungi for each wood species, Tukey–Kramer HSD showed significant differences caused by R. placenta, T. versicolor and TMC when exposed to the same wood species (i.e., Norway spruce, Scots pine sapwood, or European beech). Hence, this confirms why the performance of a wood species must be compared using the same test organisms.
When comparing mean MLf between wood species exposed to the same test organisms (i.e., R. placenta, T. versicolor or TMC), the three wood species showed significant differences in mean MLf after exposure to only T. versicolor and R. placenta. After exposure to TMC, however, no significant difference in the mean MLf between the three wood species was found.
According to Stirling et al. [24] “Field tests have been performed around the world for many decades, but unfortunately, most of the data are not available in a form that can be utilised for service life models”. This includes the use of different reference species. The first step in comparing global field test performance data (source: IRG Durability Database, https://www.irg-wp.com/durability/index.html (accessed on 1 February 2016)) for non-durable reference species was provided by Stirling et al. [24]. They noted that Norway spruce, Scots pine sapwood and European beech were all suitable for use as reference species, however, slow-grown spruce should be avoided. With this paper, the factor provided in Table 3 takes a big step further for future utilization and comparison of test performance data.

3.2. Location Level-Decay

Table 4 provides an overview of the mean MLf values for the fungal decay tests for each of the three wood species from every location included in the dataset. Table 4, Table 5 and Table 6 provide Tukey–Kramer HSD comparisons of mean MLf per wood species, between locations. The data strongly indicate that location alone is not a main influencing factor for the durability performance of Norway spruce against the two tested basidiomycetes and soft rot. Therefore, the variation needs to be investigated on a stand or tree level.
In Table 5, Tukey–Kramer HSD comparison of means illustrate that MLf (R.p.) of Norway spruce was highest for material from Hobøl stand 1 (NO), Slovenia, and Breisgau (DE). The lowest MLf (R.p.), were found for the Ribnica stand (SI) and Hobøl stand 3 (NO). Hence, the largest variation in means was found between stands within the same property and municipality in Norway. The highest MLf (T.v.) for Norway spruce was found for Hobøl stand 1 (NO), and lowest for the Ribnica stand (SI), and Rippoldsau (DE). The highest MLf (TMC) was again for Hobøl stand 1 (NO) and the lowest for Ribnica stand (SI), and Hobøl stand 3 (NO).
The main influencing factor of variations in decay performance did not seem to be location, but rather tree or stand level factors. In Table 6, Tukey–Kramer HSD comparison of means illustrate that MLf (R.p.) of Scots pine sapwood varied greatly between locations, the highest MLf (R.p.) was found for material from Nordern Zealand (DK), and the lowest from Raseborg stand 5 in Finland. For MLf (T.v.) the variation between locations was much lower and the significant highest means were found for Kongsberg stand 9 (NO), Berkåk stand 2 (NO), Alves (GB), Raseborg stand 4 (FI), Borås stand 5 (SE), Pudasjärvi stand 1 (FI), Harads stand 4 (SE), Tartu stand 1 (EE), Rognan stand 1 (NO), and Northern Spain.
The material from Denmark and Oerrel (DE) had the significantly highest MLf (TMC), while Munlochy Stand 2 (GB) had the lowest. As for Norway spruce (Table 5), material from different stands at the same location varied significantly.
The southern European beech material tended to be slightly less resistant against the two tested basidiomycetes and soft rot compared to the more northern material. In Table 7, Tukey–Kramer HSD comparison of means illustrates that for MLf (R.p.) of European beech, three distinct groups were found. The highest MLf (R.p.) was recorded for Haute Saône (FR) and northern Spain, similar MLf (R.p.) for Slovenia, Switzerland and Denmark, and lowest for Reinhausen (DE). The mass loss MLf (T.v.) of European beech from northern Spain, Haute Saône (FR) and Switzerland were higher than the material from Slovenia and Denmark. European beech from Reinhausen (DE) had significantly higher MLf (TMC) than the material from Slovenia, Switzerland and Denmark.

3.3. Location Level-Moisture

Table 8 provides an overview of mean values for the moisture tests for each of the three wood species at every location included in the dataset. Table 9, Table 10 and Table 11 provide Tukey–Kramer HSD comparisons of mean values for the moisture tests per wood species between locations.
Location was not the main influencing factor for Norway spruce LWU, VU, VR and CWU. According to the Tukey–Kramer HSD comparison of moisture data for Norway spruce between locations (Table 9), LWU was highest for the material from Hobøl stand 1 (NO) and Slovenia (SI). For the three stands on the same property in Hobøl (NO), LWU was significantly different between the stands. The lowest LWU values were found for the two German locations (Rippoldsau and Breisgau), and Eastern Finland. EMC~100%RH showed no significant variation between stands.
In Table 10, Tukey–Kramer HSD comparison of means illustrates that for Scots pine sapwood it was a general tendency between the tests that the Baltic and Nordic Scots pine sapwood material, with the exception of Denmark, tended to group together. For LWU, the highest mean was reached by the material from Denmark and Germany, the lowest from Finland and the Baltics. For W24100% no clear pattern was found for locations/countries, the highest values were found for the material from Norway, Sweden, Scotland, Finland and the Baltics. W240% data from one of the Scottish locations together with material from Finland, the Baltics and Sweden formed one group with low W240%, the Norwegian material grouped in the middle and the remaining materials had statistically similar W240%. CWU generally followed the same trends as LWU while no clear pattern between locations was found for EMC~100%RH.
In Table 11, three distinct groups were found using Tukey–Kramer HSD comparison of means for European beech analysed by LWU, the highest mean being Reinhausen (DE). Statistically similar means were found for Denmark and Slovenia, and lowest mean for Switzerland. No significant difference was found for VU. For VR Reinhausen (DE) and Slovenia had the highest values, and Switzerland the lowest. CWU was highest for Slovenia and northern Spain, lowest for Reinhausen (DE). The only difference in EMC~100%RH was found between Slovenia and Switzerland.

3.4. Correlation Matrix Wood—Effect of Density and Annual Ring Width

In order to examine the effect of initial oven-dry density (ρ0) and annual ring width (ARW), four regression models (Equation (13a–d)) were provided (Table 12).
Model 1 (ρ0) shows significant coefficient effects of ρ0 for all decay fungi/wood species combinations. R2 show that the model explained some of the data variation for R. placenta vs. Norway spruce (R2 = 0.43) and vs. Scots pine sapwood (R2 = 0.24), and soft rot vs. Norway spruce (R2 = 0.33), while for T. versicolor, none of the variations in the different decay fungi/wood species combinations was explained by the model.
Model 2 (ARW) shows significant coefficient effects of annual ring width for: R. placenta vs. Norway spruce and Scots pine sapwood, soft rot vs. Norway spruce and European beech. No significant effects were found for T. versicolor. R2 was low, i.e., the variation in the data was not explained, for any of decay fungi/wood species combinations in this model.
Model 3 (ρ0 + ARW) included ρ0 and annual ring width. ρ0 was significant for all decay fungi and wood species combinations, while ARW was significant for: R. placenta vs. Norway spruce, Scots pine sapwood and European beech, T. versicolor vs. Scots pine, soft rot vs. European beech. R2 show that the model explained roughly half of the data variation for R. placenta vs. Norway spruce (R2 = 0.53) and some of the variation for soft rot (R2 = 0.328).
Model 4 (ρ0 + ARW + ρ0 × ARW) included ρ0, ARW plus the ρ0-ARW interactions for the fungus/material combinations. Again, ρ0 was significant for all decay fungi and wood species combinations, ARW was significant for: R. placenta vs. Scots pine sapwood, T. versicolor vs. Scots pine sapwood and European beech. The ρ0-ARW interactions were significant for: R. placenta vs. Norway spruce and Scots pine sapwood, soft rot vs. Norway spruce, Scots pine sapwood and European beech. R2 show that the model explained roughly half of the data variation for Norway spruce vs. R. placenta vs. (R2 = 0.54) and some of the variation for soft rot (R2 = 0.36). For Scots pine sapwood, one-third of the variation was explained by R. placenta (R2 = 0.30).
This model approach illustrates that ρ0 and the combination of ρ0 and ARW is an influencing factor for R. placenta decay of the softwoods. For soft rot, the effect of ρ0 and the combination of ρ0 and ARW was strongest for Norway spruce. With the model used here, no effect of ρ0 and/or ARW was found for T. versicolor. For practical purposes, this implies that especially for decay tests with R. placenta the recommendations in standards regarding density and annual ring width are of great importance.
Stirling et al. [24] noted that “Greater attention should be given to characterisation and reporting of material quality, e.g., density, annual year ring width, and ideally also water sorption properties of individual test specimens”. This study confirms this. In order to ensure reproducability and comparability of experiments it is recommended to: (1) follow the specifications for annual ring width in standards, and (2) preferably report the ring width and density for individual specimens. Sandberg and Salin [25] performed adsorption tests on Norway spruce and found differences in liquid water absorption between sapwood and heartwood as well as between trees from different growth conditions. According to Stirling et al. [24] species with the greatest absorption and retention of water decayed most rapidly. Latewood content and growth conditions influenced the treatability of Scots pine sapwood significantly [21] and in this context, latewood content was shown to be more important than density due to the open pathways provided by the unaspirated bordered pits in the dried wood. These pathways could also be beneficial in the initial wetting of the wood prior to fungal infestation. Position in the stem, tree origin, and latewood content are therefore factors, which could add to some of the unexplained variations in the models.

4. Conclusions

The variation of the examined durability and moisture performance indicators was surprisingly low within and between the three reference wood species usually considered for wood durability testing in Europe. Therefore, in Part 2 of this series [18], the obtained conversion factors will further be used to utilize existing durability tests for validating and optimizing the ‘Meyer-Veltrup model’ for material-resistance [7]. Additionally, Part 3 of this publication [19] will survey wood durability test data, utilize them for implementation in a material resistance model and generate a database for service life prediction of wood products in above and in-ground situations.
Nevertheless, annual ring width and oven-dry density turned out to be decisive parameters and can explain the variation of reference species’ properties to a great extent. Hence, carefully selecting wood material from reference species with respect to these parameters is recommended to assure high accuracy and reproducibility of both durability and moisture performance tests.

Author Contributions

G.A. and C.B. were mainly responsible for the conceptualization, methodology used, data evaluation, data validation, and formal analysis; Ka.Z. contributed significantly to the latter; investigations and data curation were conducted by G.A., C.B., M.H., R.F.A.S., Ka.Z. and B.N.M.; the original draft of this article was prepared by C.B. and G.A., who were also responsible for the review and editing process of this article. All authors have read and agreed to the published version of the manuscript.

Funding

The authors received funding in the frame of the research project CLICKdesign, which is supported under the umbrella of ERA-NET Cofund ForestValue by the Ministry of Education, Science and Sport (MIZS)—Slovenia; The Ministry of the Environment (YM)—Finland; The Forestry Commissioners (FC)—UK; Research Council of Norway (RCN, 297899)—Norway; The French Environment and Energy Management Agency (ADEME) and The French National Research Agency (ANR)—France; The Swedish Research Council for Environment, Agricultural Sciences and Spatial Planning (FORMAS), Swedish Energy Agency (SWEA), Swedish Governmental Agency for Innovation Systems (Vinnova)—Sweden; Federal Ministry of Food and Agriculture (BMEL) and Agency for Renewable Resources (FNR)—Germany. ForestValue has received funding from the European Union’s Horizon 2020 research and innovation program under grant agreement N° 773324.

Data Availability Statement

All mean values, standard deviations and number of replicates per wood material, fungi and location for the dataset are presented in this paper. The entire set of raw data presented in this study is available on request from the corresponding author.

Acknowledgments

Stefania Fortino VTT FI, StoraEnso FI, Morten Klamer DTI DK, Magdalena Kutnik FCBA, David Lorenzo University of Santiago de Compostela ES, Jakub Sandak InnoRenew SI, Boštjan Lesar University of Ljubljana SI, Ed Suttie BRE GB and James Jones & Sons Ltd. GB are acknowledged for providing wood test material. Andreas Buschalsky and Philip B. Van Niekerk University of Göttingen, and Sigrun Kolstad NIBIO are acknowledged for their support with the different decay tests, and Andreja Žagar University of Ljubljana for tensiometer measurements. Further, we want to acknowledge the following for helping out with the overview of reference species around the world: Charunee Vongkaluang Royal Forest Department TH, Tripti Singh Scion NZ, Lesley Francis Dep. of Agriculture, Fisheries and Forestry AU, Hiroshi Matsunaga Forestry and Forest Products Research Institute JP, Jeff J. Morrell University of the Sunshine Coast AU, Jeff D. Lloyd Nisus US and Adam Taylor University of Tennessee US.

Conflicts of Interest

The authors declare no conflict of interest. The funders had no role in the design of the study; in the collection, analyses, or interpretation of data; in the writing of the manuscript, or in the decision to publish the results.

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Table 1. Number of replicates used in this study. R.p. = Rhodonia placenta, T.v. = Trametes versicolor, TMC = terrestrial microcosm, soft rot test, W24 = 24 h water uptake and release tests, EMC~100%RH = cell wall saturation, CWU = capillary water uptake. NA = not available.
Table 1. Number of replicates used in this study. R.p. = Rhodonia placenta, T.v. = Trametes versicolor, TMC = terrestrial microcosm, soft rot test, W24 = 24 h water uptake and release tests, EMC~100%RH = cell wall saturation, CWU = capillary water uptake. NA = not available.
DecayMoisture
LocationR.p.T.v.TMCW24, EMC~100%RHCWU
Norway spruceRippoldsau, DE151515109
Breisgau, DE1515151010
Eastern Finland, FI2525505050
Haute Loire, FR151530109
Slovenia, SI2021453012
Ribnica, SI333389404
Hobøl, stand 1, NO55101010
Hobøl, stand 2, NO3030606060
Hobøl, stand 3, NO3535707069
Total Norway spruce:193194384290233
Scots pine sapwoodNorthern Zealand, DK1515301010
Tartu, stand 1, EE2525NA105
Tartu, stand 2, EE1010NA42
Pudasjärvi, stand 1, FI1515NA63
Heinävesi, stand 3, FI55NA21
Raseborg, stand 4, FI1515NA43
Raseborg, stand 5, FI1010NA42
Eastern Finland, FI2525505050
St Chély d’apcher, FR1515301010
Oerrel, DE1515151010
Halberstadt, DE1515151010
Unterfranken, DE1514151010
Klaipeda, stand 1, LT4040NA168
Rognan, stand 1, NO55NA00
Berkåk, stand 2, NO55NA00
Åkrestrømmen, stand 4, NO55NA20
Kongsberg, stand 5, NO1515NA63
Kongsberg, stand 9, NO55NA21
Bergen, stand 7, NO55NA21
Bergen, stand 8, NO55NA21
Harads, stand 4, SE1515NA63
Borås, stand 5, SE2020NA64
Borås, stand 6, SE1010NA42
Forres, stand 1, Scotland, GB1010NA42
Munlochy, stand 2, Scotland, GB3030NA126
Alves, Scotland, GB60601204036
Slovenia, SI212245308
Northern Spain, ES151569108
Total Scots pine sapwood:446446389272199
European beechHaute Saône, FR1515301010
Reinhausen, DE1515151010
Slovenia, SI212145308
Switzerland, CH212175308
Northern Spain, ES1515NA010
Denmark, DK4545903030
Total beech:13213225511076
Total specimens per test:7717721028672508
Table 2. Mixing ratios of soil substrates for WHCsoil of mixed soil substrates. Percentage is based on the oven-dry soil mass (g).
Table 2. Mixing ratios of soil substrates for WHCsoil of mixed soil substrates. Percentage is based on the oven-dry soil mass (g).
Resultant WHCsoil (%)
Equation (7)10093867972655851443730
Percentage compost (%)1009080706050403020100
Percentage sand (%)0102030405060708090100
Table 3. Summary of the main findings, factors (in bold) for: the inherent protective properties of wood (kinh), wetting ability (kwa), and conversion from Norway spruce vs. Scots pine sapwood or European beech, and material resistance dose (DRd) per wood species. sw = sapwood.
Table 3. Summary of the main findings, factors (in bold) for: the inherent protective properties of wood (kinh), wetting ability (kwa), and conversion from Norway spruce vs. Scots pine sapwood or European beech, and material resistance dose (DRd) per wood species. sw = sapwood.
Norway SpruceScots Pine swEuropean Beech
MLf
(%)
kinh
(-)
MLf
(%)
kinh
(-)
MLf
(%)
kinh
(-)
fspruce/pine swfspruce/beech
kinhR. placenta27.171.0030.660.8924.821.091.130.91
T. versicolor21.411.0024.940.8629.670.721.161.39
TMC19.101.0018.531.0318.871.010.970.99
kinh all 1.00 0.95 0.961.051.04
W24
(%)
kwa
(-)
W24
(%)
kwa
(-)
W24
(%)
kwa
(-)
kwaliquid uptake61.311.0060.551.0153.701.140.990.88
vapor uptake12.171.0013.970.8710.481.161.150.86
vapor release16.271.0013.540.8315.990.981.201.02
CWU
(g/cm2)
kwa
(-)
CWU
(g/cm2)
kwa
(-)
CWU
(g/cm2)
kwa
(-)
kwacapillary uptake0.301.000.291.030.211.430.970.70
kwaall 1.00 0.94 1.181.070.85
DRd 325 290 328
Table 4. Mean mass loss (MLf) and standard deviation from all decay tests at each location. R.p. = Rhodonia placenta, T.v. = Trametes versicolor, TMC = terrestrial microcosm, soft rot test, NA = not available, s. = stand.
Table 4. Mean mass loss (MLf) and standard deviation from all decay tests at each location. R.p. = Rhodonia placenta, T.v. = Trametes versicolor, TMC = terrestrial microcosm, soft rot test, NA = not available, s. = stand.
LocationMLf (R.p.) [%]MLf (T.v.) [%]MLf (TMC) [%]
Norway spruceRippoldsau DE27.64 ± 1.2416.91 ± 4.0418.82 ± 4.80
Breisgau DE30.45 ± 2.0524.71 ± 1.3912.78 ± 3.89
E. Finland FI26.85 ± 2.7122.39 ± 3.3918.05 ± 6.42
Haute Loire FR27.50 ± 1.8121.85 ± 2.6124.49 ± 5.09
Slovenia SI30.95 ± 4.1222.33 ± 2.9020.35 ± 5.80
Ribnica SI24.39 ± 1.6416.08 ± 1.1916.48 ± 4.19
Hobøl s.1 NO31.28 ± 1.0027.36 ± 3.7430.57 ±9.64
Hobøl s.2 NO28.53 ± 3.0823.88 ± 4.0622.36 ± 6.45
Hobøl s.3 NO24.35 ± 2.2822.53 ± 3.4917.04 ± 4.11
Total mean:27.17 ± 3.4621.41 ± 4.3419.10 ± 6.31
N. Zealand DK39.24 ± 1.0323.79 ± 4.6126.55 ± 4.99
Scots pine sapwoodTartu s.1 EE28.51 ± 2.0526.16 ± 2.58NA
Tartu s.2 EE31.95 ± 3.2123.38 ± 1.99NA
Pudasjärvi s.1 FI29.96 ± 1.4126.85 ± 3.37NA
Heinävesi s.3 FI29.90 ± 1.1626.80 ± 1.45NA
Raseborg s.4 FI30.93 ± 2.6127.02 ± 2.00NA
Raseborg s.5 FI26.26 ± 1.1325.20 ± 1.82NA
E. Finland FI30.45 ± 1.7024.66 ± 2.8914.46 ± 4.34
St Chély d’a. FR29.78 ± 2.2327.12 ± 3.5416.35 ± 3.75
Oerrel DE35.07 ± 1.8125.38 ± 1.9425.17 ± 3.17
Halberstadt DE34.25 ± 1.1424.58 ± 2.0219.22 ± 4.11
Unterfranken DE30.79 ± 0.7824.92 ± 1.4121.40 ± 5.87
Klaipeda s.1 LT30.01 ± 2.2422.11 ± 4.50NA
Rognan s.1 NO26.94 ± 1.9328.56 ± 3.52NA
Berkåk s.2 NO32.31 ± 1.8129.75 ± 6.72NA
Åkrestr. s.4 NO27.07 ± 1.9125.51 ± 1.67NA
Kongsb. s.5 NO30.77 ± 0.9825.20 ± 3.73NA
Kongsb. s.9 NO34.21 ± 2.0228.41 ± 2.35NA
Bergen s.7 NO26.86 ± 1.5724.62 ± 3.16NA
Bergen s.8 NO30.82 ± 1.1823.37 ± 0.87NA
Harads s.4 SE29.62 ± 2.2926.70 ± 3.24NA
Borås s.5 SE30.25 ± 1.9125.71 ± 5.16NA
Borås s.6 SE31.50 ± 1.4826.60 ± 2.12NA
Forres s.1 GB28.85 ± 0.9326.20 ± 2.46NA
Munlochy S.2 GB27.49 ± 1.7319.86 ± 2.60NA
Alves GB31.05 ± 1.6824.73 ± 4.5118.32 ± 4.92
Slovenia SI34.34 ± 2.5825.01 ± 1.7217.80 ± 5.76
N. Spain ES26.87 ± 1.7628.38 ± 2.4017.58 ± 3.93
Total mean:30.66 ± 3.2024.94 ± 3.9018.53 ± 5.58
European beechHaute Saône FR30.86 ± 1.1232.55 ± 2.6322.86 ± 4.08
Reinhausen DE14.91 ± 9.4628.39 ± 1.5825.38 ± 4.88
Slovenia SI26.09 ± 1.8828.35 ± 4.7916.97 ± 3.41
Switzerland CH25.17 ± 2.6131.91 ± 5.8018.14 ± 4.26
N. Spain ES30.70 ± 3.0433.48 ± 3.22NA
Denmark DK23.40 ± 4.0727.44 ± 3.6618.01 ± 4.18
Total mean:24.82 ± 6.1829.67 ± 4.5618.87 ± 4.70
Table 5. Norway spruce, Tukey–Kramer HSD (T–K) comparison of mean percent mass loss. Materials not sharing the same letter have statistically significant differences in mean mass loss (MLf). R.p. = Rhodonia placenta, T.v. = Trametes versicolor, TMC = terrestrial microcosm, soft rot test, s. = stand.
Table 5. Norway spruce, Tukey–Kramer HSD (T–K) comparison of mean percent mass loss. Materials not sharing the same letter have statistically significant differences in mean mass loss (MLf). R.p. = Rhodonia placenta, T.v. = Trametes versicolor, TMC = terrestrial microcosm, soft rot test, s. = stand.
MLf (R.p.) MLf (T.v.) MLf (TMC)
LocationT–KMeanT–KMeanT–KMean
Hobøl s.1 NOABC 31.28A 27.36A 30.57
Slovenia SIA 30.95 B 22.33 CD 20.35
Breisgau DEAB 30.45AB 24.71 F12.78
Hobøl s.2 NO BCD 28.53AB 23.88 BC 22.36
Rippoldsau DE BCD 27.64 C16.91 CDEF18.82
Haute Loire FR CD 27.50 B 21.85AB 24.49
E. Finland FI D 26.85 B 22.39 DE 18.05
Ribnica SI E24.39 C16.08 EF16.48
Hobøl s.3 NO E24.35 B 22.53 EF17.04
Table 6. Scots pine sapwood, Tukey–Kramer HSD (T–K) comparison of mean percent mass loss. Materials not sharing the same letter have statistically significant differences in mean mass loss (MLf). R.p. = Rhodonia placenta, T.v. = Trametes versicolor, TMC = terrestrial microcosm, soft rot test, NA = not available, s. = stand.
Table 6. Scots pine sapwood, Tukey–Kramer HSD (T–K) comparison of mean percent mass loss. Materials not sharing the same letter have statistically significant differences in mean mass loss (MLf). R.p. = Rhodonia placenta, T.v. = Trametes versicolor, TMC = terrestrial microcosm, soft rot test, NA = not available, s. = stand.
MLf (R.p.) MLf (T.v.) MLf (TMC)
LocationT–KMeanT–KMeanT–KMean
N. Zealand DKA 39.24A BC23.79A 26.55
Oerrel DE B 35.07AB 25.38AB 25.17
Slovenia SI BC 34.34AB 25.01 CD 17.80
Halberstadt DE BCD 34.25AB 24.58 CD 19.22
Kongsb. s.9 NO BCDE 34.21A 28.41NA
Berkåk s.2 NO BCDEF 32.31A 29.75NA
Tartu s.2 EE CDEF 31.95ABC23.38NA
Borås s.6 SE DEF 31.50AB 26.60NA
Alves GB EF 31.05A 24.73 CD 18.32
Raseborg s.4 FI EF 30.93A 27.02NA
Bergen s.8 NO DEFGHIJ 30.82ABC23.37NA
Unterfranken DE EF 30.79AB 24.92 BC 20.40
Kongsb. s.5 NO EFG 30.77AB 25.20NA
E. Finland FI FG I 30.45AB 24.66 E14.46
Borås s.5 SE FG IJ 30.25A 25.71NA
Klaipeda s.1 LT FG IJ 30.01 BC22.11NA
Pudasjärvi s.1 FI FG IJ 29.96A 26.85NA
Heinävesi s.3 FI EFGHIJK29.90AB 26.80NA
St Chély d’a. FR FG IJ 29.78A 27.12 DE16.35
Harads s.4 SE FGHIJ 29.62A 26.70NA
Forres s.1 GB FGHIJK28.85AB 26.20NA
Tartu s.1 EE GHIJK28.51A 26.16NA
Munloc. s.2 GB H K27.49 C19.86NA
Åkrestr. s.4 NO HIJK27.07ABC25.51NA
Rognan s.1 NO H JK26.94A 28.56NA
N. Spain ES K26.87A 28.38 CD 17.58
Bergen s.7 NO H JK26.86ABC24.62NA
Raseborg s.5 FI K26.26AB 25.20NA
Table 7. European beech, Tukey–Kramer HSD (T–K) comparison of mean percent mass loss. Materials not sharing the same letter have statistically significant differences in mean mass loss (MLf). R.p. = Rhodonia placenta, T.v. = Trametes versicolor, TMC = terrestrial microcosm, soft rot test, NA = not available, s. = stand.
Table 7. European beech, Tukey–Kramer HSD (T–K) comparison of mean percent mass loss. Materials not sharing the same letter have statistically significant differences in mean mass loss (MLf). R.p. = Rhodonia placenta, T.v. = Trametes versicolor, TMC = terrestrial microcosm, soft rot test, NA = not available, s. = stand.
MLf (R.p.) MLf (T.v.) MLf (TMC)
LocationT–KMeanT–KMeanT–KMean
Haute Saône FRA 30.86AB 32.55A 22.86
N. Spain ESA 30.70A 33.48NA
Slovenia SI B 26.09 C28.35 B16.97
Switzerland CH B 25.17AB 31.91 B18.14
Denmark DK B 23.40 C27.44 B18.01
Reinhausen DE C14.91 BC28.39A 25.38
Table 8. Means and standard deviation from all moisture tests. NA = not available; s. = stand.
Table 8. Means and standard deviation from all moisture tests. NA = not available; s. = stand.
LocationVU [%]VR [%]LWU [%]CWU [g/cm2]EMC~100%RH
Norway spruceRippoldsau DE13.87 ± 3.0115.02 ± 1.0556.97 ± 5.530.29 ± 0.0428.45 ± 6.44
Breisgau DE11.89 ± 1.0614.03 ± 1.6852.72 ± 6.070.21 ± 0.0727.37 ± 2.84
E. Finland FI12.28 ± 1.7116.53 ± 1.4753.13 ± 7.780.29 ± 0.0528.47 ± 2.02
Haute Loire FR14.08 ± 1.2818.01 ± 1.0263.27 ± 7.980.22 ± 0.0529.92 ± 1.89
Slovenia SI13.69 ± 2.3915.75 ± 1.8171.92 ± 9.270.35 ± 0.0529.40 ± 2.59
Ribnica SI11.27 ± 2.0515.49 ± 0.6959.49 ± 6.660.42 ± 0.0629.40 ± 0.79
Hobøl s.1 NO13.58 ± 1.3817.85 ± 1.7187.45 ± 9.180.51 ± 0.1430.53 ± 2.61
Hobøl s.2 NO12.41 ± 1.9117.18 ± 1.0565.68 ± 9.740.33 ± 0.1229.37 ± 1.80
Hobøl s.3 NO11.06 ± 1.7816.00 ± 1.8457.74 ± 5.010.28 ± 0.1028.39 ± 3.12
Total mean:12.17 ± 2.1316.27 ± 1.6761.31 ± 10.710.30 ± 0.1128.94 ± 2.59
Scots pine sapwoodN. Zealand DK12.67 ± 1.4516.25 ± 0.8386.68 ± 4.610.55 ± 0.0530.31 ± 1.42
Tartu s.1 EE17.49 ± 1.257.14 ± 0.6653.47 ± 2.970.14 ± 0.0331.62 ± 1.31
Tartu s.2 EE18.01 ± 0.207.92 ± 0.7058.38 ± 0.690.20 ± 0.1029.64 ± 0.47
Pudasjärvi s.1 FI18.15 ± 0.225.95 ± 0.7255.70 ± 1.540.11 ± 0.0428.21 ± 0.18
Heinävesi s.3 FI19.69-6.84-54.77-0.14-33.75-
Raseborg s.4 FI19.32 ± 1.269.50 ± 0.0250.28 ± 5.520.13 ± 0.0141.33 ± 2.18
Raseborg s.5 FI16.86 ± 0.957.78 ± 0.0848.20 ± 5.360.12 ± 0.0230.11 ± 0.31
E. Finland FI10.26 ± 1.7715.80 ± 2.4149.93 ± 5.100.23 ± 0.0728.43 ± 2.88
St Chély d’a. FR12.28 ± 1.4616.00 ± 2.4859.71 ± 6.390.24 ± 0.0328.07 ± 3.79
Oerrel DE12.89 ± 1.0816.75 ± 3.8570.34 ± 4.530.41 ± 0.0428.43 ± 5.42
Halberstadt DE10.81 ± 1.0317.41 ± 2.1068.60 ± 4.740.41 ± 0.0430.55 ± 3.04
Unterfranken DE14.10 ± 4.7116.48 ± 3.6577.65 ± 14.380.48 ± 0.0630.52 ± 6.32
Klaipeda s.1 LT17.80 ± 0.586.57 ± 1.5253.16 ± 3.670.15 ± 0.0228.86 ± 0.86
Rognan s.1 NONANANANANA
Berkåk s.2 NONANANANANA
Åkrestr. s.4 NO20.62-14.31-51.71-NA37.90-
Kongsb. s.5 NO21.19 ± 2.2014.55 ± 4.2767.68 ± 17.260.14 ± 0.0634.64 ± 6.24
Kongsb. s.9 NO21.58-8.32-65.00-0.14-25.52-
Bergen s.7 NO20.98-7.26-54.82-0.18-29.60-
Bergen s.8 NO21.30-8.36-57.84-0.11-29.51-
Harads s.4 SE20,15 ± 0.535.26 ± 0.8956.84 ± 2.300.14 ± 0.0330.52 ± 1.28
Borås s.5 SE17.94 ± 0.826.04 ± 1.0756.18 ± 2.410.13 ± 0.0128.50 ± 0.64
Borås s.6 SE18.29 ± 0.086.89 ± 0.7256.84 ± 4.540.15 ± 0.0128.80 ± 0.41
Forres s.1 GB19.64 ± 0.218.48 ± 0.8361.89 ± 0.480.13 ± 0.0433.54 ± 0.83
Munloc. s.2 GB18.06 ± 1.308.13 ± 4.7452.80 ± 4.550.12 ± 0.0534.13 ± 5.62
Alves GB11.84 ± 1.7615.48 ± 0.9064.49 ± 3.670.31 ± 0.0829.52 ± 1.47
Slovenia SI11.93 ± 2.1615.30 ± 0.7667.14 ± 9.660.45 ± 0.0628.95 ± 0.75
N. Spain ES10.99 ± 1.4915.68 ± 1.7064.08 ± 4.210.46 ± 0.1529.72 ± 2.55
Total mean:13.97 ± 3.9313.13 ± 4.5460.55 ± 11.040.29 ± 0.1429.90 ± 3.56
European beechHaute Saône FR10.89 ± 1.2217.59 ± 0.9557.72 ± 3.360.19 ± 0.0330.54 ± 1.11
Reinhausen DE11.70 ± 3.9016.83 ± 0.7764.90 ± 1.640.15 ± 0.0430.74 ± 1.45
Slovenia SI9.54 ± 1.5316.27 ± 1.5254.21 ± 3.280.31 ± 0.0531.02 ± 2.40
Switzerland CH10.78 ± 2.0615.08 ± 0.8846.51 ± 6.240.19 ± 0.0329.07 ± 1.55
N. Spain ESNANANA0.27 ± 0.06NA
Denmark DK10.56 ± 2.8415.82 ± 0.9955.32 ± 6.760.20 ± 0.0329.83 ± 1.89
Total mean:10.48 ± 2.3915.99 ± 1.3353.70 ± 7.390.21 ± 0.0630.10 ± 2.00
Table 9. Norway spruce, Tukey–Kramer HSD (T–K) comparison of mean moisture data. Materials not sharing the same letter have statistically significant differences in mean moisture parameters. Moisture data from Berkåk s.2 (NO) and Rognan s.1 (NO) not available; s. = stand.
Table 9. Norway spruce, Tukey–Kramer HSD (T–K) comparison of mean moisture data. Materials not sharing the same letter have statistically significant differences in mean moisture parameters. Moisture data from Berkåk s.2 (NO) and Rognan s.1 (NO) not available; s. = stand.
LWUVUVRCWUEMC~100%RH
LocationT-KMeanT–KMeanT–KMeanT–KMeanT–KMean
Hobøl s.1 NOA 87.45AB 13.58A 17.85A 0.51A30.52
Slovenia SI B 71.92A 13.69 BC 15.75 BC 0.35A29.40
Breisgau DE C 65.68ABC 12.41A 17.18 B 0.33A29.37
Hobøl s.2 NO BCD 63.27AB 14.08A 18.01 CD0.22A29.92
Rippoldsau DE D 59.49 CD11.27 CD15.49AB 0.42A29.40
Haute Loire FR D 57.74 D11.06 BC 16.00 BCD0.28A28.39
E. Finland FI DE56.97AB 13.87 BCD15.02 BCD0.29A28.45
Ribnica SI E53.13 BC 12.28AB 16.53 BCD0.29A28.47
Hobøl s.3 NO DE52.72ABCD11.89 D14.03 D0.21A27.37
Table 10. Scots pine sapwood, Tukey–Kramer HSD (T–K) comparison of mean moisture data. Materials not sharing the same letter have statistically significant differences in mean moisture parameter. Material collected by Zimmer et al. [21], marked with *, was merged at country level, since only very few measurements were taken per stand; s. = stand.
Table 10. Scots pine sapwood, Tukey–Kramer HSD (T–K) comparison of mean moisture data. Materials not sharing the same letter have statistically significant differences in mean moisture parameter. Material collected by Zimmer et al. [21], marked with *, was merged at country level, since only very few measurements were taken per stand; s. = stand.
LWUVUVRCWUEMC~100%RH
LocationT-KMeanT–KMeanT–KMeanT–KMeanT–KMean
N. Zealand DKA 86.68 CD 12.67A 16.25A 0.55ABCD30.31
Unterfrank. DEAB 77.65 C 14.10A 16.48AB 0.48ABCD30.52
Oerrel DE BC 70.34 CD 12.89A 16.75 B 0.41 BCD28.43
Halberstadt DE BCD 68.60 DE10.81A 17.41 B 0.41ABCD30.55
Slovenia SI CD 67.14 CD 11.93A 15.30 B 0.45 CD28.95
Alves GB CD 64.49 D 11.84A 15.48 C 0.31 BCD29.52
N. Spain ES CDE 64.08 DE10.99A 15.68AB 0.46ABCD29.72
Norway * CDEF 61.77A 21.15 B 11.70 DEF0.14ABC 32.35
St Chély FR DEFG 59.71 CDE12.28A 16.00 CDE 0.24 CD28.07
Sweden * EFG 56.59 B 18.86 C5.96 F0.14 BCD29.33
Scotland GB * FGH55.07 B 18.46 C8.22 F0.12A 33.98
Baltics * GH53.96 B 17.73 C6.94 EF0.15 BCD29.88
Finland * GH52.35 B 18.31 C7.41 F0.12AB 32.66
E. Finland FI H49.93 E10.26A 15.80 D 0.23 D28.43
Table 11. European beech, Tukey–Kramer HSD (T–K) comparison of mean moisture data. Materials not sharing the same letter have statistically significant differences in mean moisture parameters. NA = not available.
Table 11. European beech, Tukey–Kramer HSD (T–K) comparison of mean moisture data. Materials not sharing the same letter have statistically significant differences in mean moisture parameters. NA = not available.
LWUVUW240%RHCWUEMC~100%RH
LocationT–KMeanT–KMeanT–KMeanT–KMeanT–KMean
Reinhausen DEA 64.90A11.70A 16.83 C0.15AB30.74
Haute Saône FR B 57.72A10.89A 17.59 BC0.19AB30.54
Denmark DK B 55.32A10.56 BC15.82 B 0.20AB29.83
Slovenia SI B 54.21A9.54 B 16.27A 0.31A 31.02
Switzerland CH C46.51A10.78 C15.08 BC0.19 B29.07
N. Spain ESNANANAA 0.27NA
Table 12. Overview on model statistics, giving the coefficient of determination for four different models Model 1–Model 4, for Norway spruce, European beech and Scots pine sapwood and the respective decay fungi Rhodonia placenta (R.p.), Trametes versicolor (T.v.) and TMC. For β 0 (population intercept) and β i (population slope coefficient), the respective p-values are noted, where a * indicates statistical significance. ρ0 = initial oven-dry density, ARW = annual ring width.
Table 12. Overview on model statistics, giving the coefficient of determination for four different models Model 1–Model 4, for Norway spruce, European beech and Scots pine sapwood and the respective decay fungi Rhodonia placenta (R.p.), Trametes versicolor (T.v.) and TMC. For β 0 (population intercept) and β i (population slope coefficient), the respective p-values are noted, where a * indicates statistical significance. ρ0 = initial oven-dry density, ARW = annual ring width.
Model 1 (ρ0)Model 2 (ARW)
ρ0 ARW
R2 β 0 β 1 R2 β 0 β 1
Norway spruce
R.p.0.439<0.0001 *<0.0001 * 0.093<0.0001 *<0.0001 *
T.v.0.040<0.0001 *0.0052 * 0.0001<0.0001 *0.8774
TMC0.325<0.0001 *<0.0001 * 0.014<0.0001 *0.0218 *
Scots pine sapwood
R.p.0.236<0.0001 *<0.0001 * 0.085<0.0001 *<0.0001 *
T.v.0.037<0.0001 *<0.0001 * 0.004<0.0001 *0.1665
TMC0.171<0.0001 *<0.0001 * 0.005<0.0001 *0.1780
European beech
R.p.0.030<0.0001 *0.0459 * 0.026<0.0001 *0.067
T.v.0.097<0.0001 *0.0003 * 0.0003<0.0001 *0.8415
TMC0.220<0.0001 *<0.0001 * 0.013<0.0001 *0.0687
Model 3 (ρ0 + ARW)Model 4 (ρ0 + ARW + ρ0 x ARW)
ρ0ARW ρ0ARWρ0 x ARW
R2 β 0 β 1 β 2 R2 β 0 β 1 β 2 β 3
Norway spruce
R.p.0.532<0.0001 *<0.0001 *<0.0001 *0.544<0.0001 *<0.0001 *0.09790.0235 *
T.v.0.078<0.0001 *<0.0001 *0.00580.078<0.0001 *0.0006 *0.09560.7714
TMC0.328<0.0001 *<0.0001 *0.18270.362<0.0001 *<0.0001 *0.1297<0.0001 *
Scots pine sapwood
R.p.0.263<0.0001 *<0.0001 *<0.0001 *0.300<0.0001 *<0.0001 *<0.0001 *<0.0001 *
T.v.0.075<0.0001 *<0.0001 *<0.0001 *0.079<0.0001 *<0.0001 *<0.0001 *0.1534
TMC0.173<0.0001 *<0.0001 *0.37840.203<0.0001 *<0.0001 *0.1572<0.0001 *
European beech
R.p.0.059<0.0001 *0.0342 *0.0498 *0.059<0.0001 *0.0395 *0.06010.8178
T.v.0.098<0.0001 *<0.0003 *0.87620.123<0.0001 *<0.0011 *0.60420.0543
TMC0.235<0.0001 *<0.0001 *0.0238 *0.241<0.0001 *<0.0001 *0.02780.1897
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Alfredsen, G.; Brischke, C.; Marais, B.N.; Stein, R.F.A.; Zimmer, K.; Humar, M. Modelling the Material Resistance of Wood—Part 1: Utilizing Durability Test Data Based on Different Reference Wood Species. Forests 2021, 12, 558. https://doi.org/10.3390/f12050558

AMA Style

Alfredsen G, Brischke C, Marais BN, Stein RFA, Zimmer K, Humar M. Modelling the Material Resistance of Wood—Part 1: Utilizing Durability Test Data Based on Different Reference Wood Species. Forests. 2021; 12(5):558. https://doi.org/10.3390/f12050558

Chicago/Turabian Style

Alfredsen, Gry, Christian Brischke, Brendan N. Marais, Robert F. A. Stein, Katrin Zimmer, and Miha Humar. 2021. "Modelling the Material Resistance of Wood—Part 1: Utilizing Durability Test Data Based on Different Reference Wood Species" Forests 12, no. 5: 558. https://doi.org/10.3390/f12050558

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