On the role of moisture in triggering out-of-plane displacement in paper: from the network level to the macroscopic scale

TL;DR

This paper investigates how moisture causes out-of-plane deformations in paper by developing multi-scale models that connect fiber-level interactions to macroscopic sheet behavior, supported by experimental validation.

Contribution

It introduces a macroscopic hygro-mechanical model for predicting moisture-induced deformations and a meso-structural fiber network model explaining the origin of anisotropic hygro-expansion.

Findings

The anisotropic sheet-level hygro-expansion significantly influences instability phenomena.

The fiber network model shows inter-fiber bonding expansion drives macroscopic deformation.

Experimental comparisons provide semi-quantitative validation of the models.

Abstract

The response of paper to humidity variations is a complex multi-scale problem. The hygroscopic swelling of individual fibres and their interactions within the fibrous network govern the macroscopic response. At this scale, moisture induced instabilities and out-of-plane deformations may occur. This work focuses on several aspects of this issue. A macroscopic phenomenological hygro-mechanical model is first proposed, which aims at predicting moisture induced out-of-plane deformations in paper sheets. The constitutive model is based on the relation between these deformations and typical irreversible phenomena associated to the history of paper manufacturing, i.e. the release of dried-in strains. The model is used to describe bending induced by moisture gradients through the thickness of the sheet as well as buckling due to moisture variation in the presence of mechanical constraints. The results of the model show that the anisotropic sheet-level hygro-expansion has a strong influence on the instability phenomena. Moreover, a comparison with experiments provides adequate semi-quantitative estimates. An additional step is made towards the multi-scale understanding of paper hygro-mechanics. The fundamental mechanisms governing the macroscopic moisture induced response are investigated on the basis of the underlying fibrous network. To this aim, a meso-structural model is developed which consists of a network of fibres randomly positioned in a planar region according to an orientation probability density function. A series of network simulations reveals that upon moisture content variations the expansion of the inter-fibre bonding regions drives the overall deformation. Particularly in the case of anisotropic fibre orientation, this explains the origin of the macro-scale anisotropic hygro-expansion, which is essential for the observed sheet-level instability phenomena.