| Literature DB >> 35564259 |
Mohammad Soleimani1, Sten J J van den Broek2, Rick R M Joosten1, Laura S van Hazendonk1, Sai P Maddala1, Lambert C A van Breemen2, Rolf A T M van Benthem1,3, Heiner Friedrich1,4.
Abstract
Investigating and understanding the intrinsic material properties of biogenic materials, which have evolved over millions of years into admirable structures with difficult to mimic hierarchical levels, holds the potential of replacing trial-and-error-based materials optimization in our efforts to make synthetic materials of similarly advanced complexity and properties. An excellent example is biogenic silica which is found in the exoskeleton of unicellular photosynthetic algae termed diatoms. Because of the complex micro- and nanostructures found in their exoskeleton, determining the intrinsic mechanical properties of biosilica in diatoms has only partly been accomplished. Here, a general method is presented in which a combination of in situ deformation tests inside an SEM with a realistic 3D model of the frustule of diatom Craspedostauros sp. (C. sp.) obtained by electron tomography, alongside finite element method (FEM) simulations, enables quantification of the Young's modulus (E = 2.3 ± 0.1 GPa) of this biogenic hierarchical silica. The workflow presented can be readily extended to other diatom species, biominerals, or even synthetic hierarchical materials.Entities:
Keywords: diatom frustule; electron tomography; hierarchical materials; in situ mechanical testing
Year: 2022 PMID: 35564259 PMCID: PMC9102398 DOI: 10.3390/nano12091549
Source DB: PubMed Journal: Nanomaterials (Basel) ISSN: 2079-4991 Impact factor: 5.719
Figure 1Morphology and elemental composition of the frustule of diatom C. sp. (a–d) SEM images of frustule of C. sp. (a) intact frustule of C. sp.; (b) an isolated valve deposited on its concave orientation showing the interior surface of the valve (RA = raphe; CN = central nodule); (c) porous area of the valve (TR = transapical rib; CE = cross extension; AR = areola); (d) overlapping girdle bands (GB); (e–g) EDS elemental mapping of the intact frustule; green = silicon, blue = oxygen, red = carbon; (h) FTIR spectra of frustule of C. sp.
Figure 2SEM images of different orientations of intact frustule and isolated valves of C. sp. for in situ deformation tests: (a) intact frustule standing upright; (b) intact frustule standing on girdle bands; (c) intact frustule laying on the girdle bands; (d,e) deformation test at different locations of an isolated valve laying flat; (f) deformation test on isolated valve standing on its side.
Figure 3Mechanical manipulation of an isolated valve of diatom C. sp. (a–f) SEM image sequence acquired during repositioning of an isolated valve from its flat orientation to standing on its side.
Figure 4Overall workflow to quantify Young’s modulus of biosilica in the valve: (a) SEM images of an isolated valve at different stages during the in situ deformation test; (b) load–displacement curves for three valves obtained from one culture; (c) crack formed by deformation of the valve; (d) from left to right: STEM image of the valve, a slice of the reconstructed 3D intensity map of the valve, and 3D surface views of the valve; (e) initial undeformed (I) and final deformed (II) stages of the realistic valve model in FEM simulations and a comparison between experimental and simulated load–displacement curves.