An analytic counterexample to the KAM theorem by Bessi U.

By Bessi U.

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P. Lariviere, and J. W. Hamilton (2001). Arsenic alters the function of the glucocorticoid receptor as a transcription factor. Environ. , 109:245–251. , R. Kipfer, O. A. Cirpka, C. F. Harvey, M. S. Brennwald, K. N. Ashfaque, A. B. M. Badruzzaman, S. J. Hug, and D. M. Imboden (2006). Groundwater dynamics and arsenic mobilization in Bangladesh assessed using noble gases and tritium. Environ. Sci. , 40:243–250. Knowles, F. , and A. A. Benson (1983). The biochemistry of arsenic. Trends Biochem. , 8:178–180.

Analyst , 120: 917–924. , G. Samanata, B. K. Mandal, T. R. Chowdhury, C. R. Chanda, P. P. Chowdhury, G. K. Basu, and D. Chakraborti (1996). Arsenic in groundwater in six districts of West Bengal, India. Environ. Geochem. Health, 18:5–15. , and J. G. Hering (2003). Comparison of arsenic(V) and arsenic(III) sorption onto iron oxide minerals: implications for arsenic mobility. Environ. Sci. , 37:4182–4189. Dowdle, P. , A. M. Laverman, and R. S. Oremland (1996). Bacterial dissimilatory reduction of arsenic(V) to arsenic(III) in anoxic sediments.

Sulfurreducens: (A) ESEM image of biogenic vivianite; (B) EDS spectrum of vivianite; (C) identification of vivianite by XRD. , 1983). In our experiments the phosphate was present as a constituent of the growth medium, which reacted with biogenic ferrous iron, leading to the formation of a new mineral phase with the potential to sorb arsenic. The microbial precipitation of ferrihydrite is widespread in nature. , 1994). Iron mineralization has commonly been divided into two modes: biologically controlled mineralization and biologically facilitated mineralization (Konhauser, 1997): as, for example, magnetite formation by magnetotactic bacteria, representing biologically controlled mineralization in which the particles are formed inside bacterial cells templated by a specific internal membrane (Blakemore, 1991).

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