The interlamellar organic layer plays a key role in establishing the tensile mechanical response of nacre, while changing the compressive response in only a marginal manner. We conduct observations on the epithelial layer of the abalone foot in direct contact with the extrapallial layer where the deposition process takes place and identify cilia, microvilli, and secretory cells which determine the deposition of chitin to form the interlamellar organic layer. On the basis of these observations we propose a mechanism for the deposition of interlamellar organic layers. We show that the fraction of pores, as well as their diameter, grow rapidly as the interlamellar layer is extended uniaxially or biaxially, and compare these calculations with the observed values. In the calculations we assume a Poisson's ratio equal to zero in the plane of the lamellae. This assumption is justified by the thickness of the organic layer (20-50 nm) being equal to twice the diameter of the chitin fibrils; consequently the expansion of the membrane occurs at a constant thickness. As an illustration of this effect, an externally applied strain of 0.5 increases the initial pore diameter (typically equal to 20-50 nm) to a value of ten times (0.2-0.5 μm). These calculations explain the observations of large pores reported in the literature and interpret them as the result of externally applied loads.
Keywords: Abalone; Modeling; Nacre.
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