Introduction
Wood may be idealized as a fiber-reinforced polymer, with the microfibrils of cellulose acting as fibers and reinforcing the wood in longitudinal direction, and the polymeric hemicellulose and lignin acting as a matrix material embedding the cellulose fibers (Holzer et al.
1989; Hofstetter et al.
2005; Bader et al.
2011). This matrix additionally contains distinct porous structures. As many other polymers, wood—especially the amorphous phases hemicellulose and lignin (Kelley et al.
1987)—shows a pronounced time-dependent behavior (Navi and Stanzl-Tschegg
2009). In this regard, one needs to distinguish between transport-induced, load-induced, and pseudo (shrinkage and swelling) viscoelastic phenomena, respectively (Hunt
1999).
It is well documented that relative humidity changes during a creep test accelerate creep, disregarding whether humidity increases or decreases (Armstrong and Kingston
1960; Ranta-Maunus
1975; Bažant and Meiri
1985; Mukudai and Yata
1986; Mohager and Toratti
1992). This phenomenon is commonly denoted as mechano-sorptive creep. Bažant (
1985) identified mechano-sorptive creep as a transport-induced phenomenon taking place in the porous structure of wood, roughly idealized as a network consisting of micro- and macropores. On the one hand, macropores are responsible for water transport throughout the meso-structure of wood. At least for moderate loading rates, water contained in those pores cannot withstand any external stresses. On the other hand, structured water molecules within micropores can act against the external stresses, and, hence, can transmit external loads, c.f. Bažant (
1985). Although those micropores are not involved in any global water transport, however, water molecules are transported within this microporous structures in the scope of local diffusion processes caused by moisture gradients. This molecular transport causes breakage and reforming of hydrogen bonds in the wood microfibrils, which is identified as the source of mechano-sorptive creep in wood. It is important to note that in the case of constant overall moisture content, no water transport through the macropores and no diffusion processes within micropores, respectively, occur. Hence, mechano-sorptive creep is deactivated. A similar effect is observed for cement-based materials, the so-called Pickett-effect (Pickett
1942; Acker and Ulm
2001), which is explained on the one hand by microcracking and on the other hand by a gradient in the moisture content causing molecular water transport within gel pores and hence breakage and reformation of H-bonds (similar to creep in wood), c.f. Bažant and Xi (
1993) and Altoubat and Lange (
2002).
As a second source of time-dependent behavior, load-induced (or viscoelastic) creep is observed in wood, occurring at constant moisture content within the wood. The molecular mechanism of viscoelastic creep, the breaking and reformation of H-bonds, is similar to mechano-sorptive creep (Bodig and Jayne
1982). An increased moisture content leads to augmented H-bond breakage and therefore to increased creep rates (Hering and Niemz
2012); similarly, higher temperatures increase the creep rate of wood (Jiang et al.
2009), probably due to the higher thermal motion of water molecules and therefore again due to an increase in hydrogen bond breakage. Due to the longitudinal alignment of cellulose fibers, the elastic and viscoelastic behavior of wood is apparently strongly anisotropic, which was investigated by Schniewind and Barrett (
1972) and Ozyhar et al. (
2013), where the latter authors distinguished between tension and compression.
Pseudo-creep (shrinkage and swelling), in contrast to mechano-sorptive and viscoelastic creep, is a fully reversible process (Hunt
1999; Hunt and Shelton
1988). The underlying physical process for swelling (shrinkage) is the absorption (desorption) of water in the cell walls (Nakano
2008). Shrinkage and swelling take place at moisture contents between oven-dry conditions and the fiber-saturation point and its magnitude is a function of the moisture content (Stamm
1935). Additionally, the microstructure plays a fundamental role in the amount of shrinkage and swelling (Schroeder
1972).
As regards models for describing viscoelastic behavior, several classical models were compared by Haque et al. (
2000), finding that the Kelvin–Voigt model and the Burgers model are best suited to describe creep of
Pinus radiata at different levels of moisture content. Hering and Niemz (
2012) used a Kelvin–Voigt model to describe the moisture content-dependent creep of beech wood. Mukudai (
1983) used a Maxwell model and three Kelvin–Voigt models connected in series to model the viscoelastic behavior of Japanese cypress, whereas Hunt (
2004) used a generalized Kelvin–Voigt model to estimate the creep curves of wood. Clouser (
1959), Schniewind and Barrett (
1972) and Hoyle et al. (
1985) employed power-law models to model creep behavior of timber beams. Eitelberger et al. (
2012) modeled the viscoelastic behavior of the lignin-hemicellulose matrix with a power-law model, whereas the macroscopic wood behavior was predicted to follow a fractional Zener model. King (
1961) observed that the creep deformation of wood is proportional to time and hence introduced a logarithmic creep model to consider the viscoelastic behavior of wood, whereas Bach and Pentoney (
1968) introduced a modified logarithmic creep law. In geology, a logarithmic creep model, the so-called Lomnitz model, has been introduced by Lomnitz (
1956,
1957,
1962). So far it has been applied to model cement-based materials (e.g., in Bažant and Prasannan
1989; Bažant et al.
1997; Acker and Ulm
2001; Pichler et al.
2008; Pichler and Lackner
2009), polyurethane foams (Pichler et al.
2018) and metals (Nabarro
2001a,
b).
For wood, on the other hand, logarithmic models have been introduced by King (
1961) and Bach and Pentoney (
1968), but have not been applied to the thermo-hygro-mechanical analysis of wood and wood structures. That may be (i) due to the missing expression for the relaxation function, which cannot be obtained in a straightforward manner and has only been derived recently by Mainardi and Spada (
2012), and (ii) due to the lack of a physical interpretation of logarithmic creep laws, which has been given only recently by Pandey and Holm (
2016) by linking time-dependent Newtonian viscosity to the parameters of the Lomnitz model. With these recent developments, the Lomnitz model has become much more attractive, also on account of the smaller number of model parameters, as compared to other models (e.g., the generalized Kelvin–Voigt or the generalized Maxwell model), necessary for representation of test data.
Therefore, the present paper readopts the logarithmic Lomnitz model for wood and considers, in addition to King (
1961) and Bach and Pentoney (
1968), the influence of temperature (Morlier
1994; Bekhta and Niemz
2003) and moisture content (Schänzlin
2010), as those parameters are commonly known to majorly influence the time-dependent behavior. For this purpose, the viscoelastic behavior of clear (knot-free) wood specimens of spruce at the 10 mm scale of observation is determined, disabling mechano-sorptive creep as well as shrinkage and swelling. Half-hour long creep tests were performed at different (constant) levels of temperature and moisture content.
Publisher’s Note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations