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


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.

SUBMITTER: Shiozawa H 

PROVIDER: S-EPMC3653141 | biostudies-literature | 2013

REPOSITORIES: biostudies-literature

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

Shiozawa Hidetsugu H   Bachmatiuk Alicja A   Stangl Andreas A   Cox David C DC   Silva S Ravi P SR   Rümmeli Mark H MH   Pichler Thomas T  

Scientific reports 20130101


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 a  ...[more]

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