Microscopic insight into the bilateral formation of carbon spirals from a symmetric iron core

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Abstract

Mirrored carbon-spirals have been produced from pressured ferrocene via the bilateral extrusion of the spiral pairs from an iron core. A parametric plot of the surface geometry displays the fractal growth of the conical helix made with the logarithmic spiral. Electron microscopy studies show the core is a crystalline cementite which grows and transforms its shape from spherical to biconical as it extrudes two spiralling carbon arms. In a cross section along the arms we observe graphitic flakes arranged in a herringbone structure, normal to which defects propagate. Local-wave-pattern analysis reveals nanoscale defect patterns of two-fold symmetry around the core. The data suggest that the bilateral growth originates from a globular cementite crystal with molten surfaces and the nano-defects shape emerging hexagonal carbon into a fractal structure. Understanding and knowledge obtained provide a basis for the controlled production of advanced carbon materials with designed geometries.

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Shiozawa, H., Bachmatiuk, A., Stangl, A., Cox, D. C., Silva, S. R. P., Rümmeli, M. H., & Pichler, T. (2013). Microscopic insight into the bilateral formation of carbon spirals from a symmetric iron core. Scientific Reports, 3. https://doi.org/10.1038/srep01840

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