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Chapter 4 - Jacobs University

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<strong>Chapter</strong> 4<br />

16-Iron Metal Center Nanocluster<br />

4.6 References<br />

(1) a) This refers in a general sense to scenarios where “materials” grow with preferred<br />

orientations on surfaces influenced/directed by the surfaces’ geometry: Henrich, V. E.;<br />

Cox, P. A, The Surface Science of Metal Oxides, Cambridge <strong>University</strong> Press,<br />

Cambridge 1994, p. 384. b) The process is quite common in the geosphere. This leads to<br />

situations where spaces with larger scale sizes (bulk condition comparable), but also up to<br />

smaller scales, are filled with minerals or water; the well-known geodes are objects of<br />

that type (see textbooks of mineralogy). The confinement induced changes in the water<br />

structure and dynamics, which are commonly substrate specific, play a key-role in the<br />

geosphere regarding the reactivity of mineral surfaces (see Wang, J.; Kalinichev, A. G.;<br />

Kirkpatrick, R. J. J. Phys. Chem. B 2005, 109, 14308). Important information about that<br />

topic can be obtained from POM chemistry(see : Oleinikova, A.; Nrtner, H. W.; Chaplin,<br />

M.; Diemann, E.; Bögge, H.; Müller, A. Chem Phys Chem. 2007, 8, 646).<br />

(2 ) Phospholipid vesicles are for instance the reaction vessels for many biomineralisation<br />

processes: in the spatially confined environments the biological systems can control the<br />

reaction conditions to achieve extraordinary morphologies (Douglas, T. in Biomimetic<br />

Materials Chemistry (Ed.: S. Mann), VCH, Weinheim, 1996, p. 91).<br />

(3) Mann, S. Biomineralisation: Principles and Concepts in Bioinorganic Materials<br />

Chemistry, Oxford <strong>University</strong> Press, Oxford, 2001.<br />

(4) a) Kaim, W.; Schwederski, B. Bioinorganic Chemistry: Inorganic Elements in the<br />

Chemistry of Life, Wiley, Chichester, 1994; see also Essen, L.-O.; Offermann, S.;<br />

Oesterhelt, D.; Zeth, K. in Biomineralisation: Progress in Biology, Molecular Biology<br />

and Application (Ed.: E. Baeuerlein), Wiley-VCH, Weinheim, 2004, p. 119; in this<br />

context the authors refer to the toxicity of Fe 2+ for aerobic organisms in the sense that it<br />

-<br />

reduces O 2 to the reactive superoxide anion O 2 and reacts with the peroxide in the<br />

Fenton reaction to form the highly reactive OH· radical. b) Schemberg, J.; Schneider, K.;<br />

Demmer, U.; Warkentin, E.; Müller, A.; Ermler, U. Angew. Chem. 2007, 119, 2460;<br />

Angew. Chem. Int. Ed. 2007, 46, 2408. c) Müller, A.; Shah, S. Q. N.; Bögge, H.;<br />

Schmidtmann, M.; Nature 1999, 397, 48.<br />

88

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