Тип публикации: статья из журнала

Год издания: 2007

Идентификатор DOI: 10.1134/S0020168507060155

Аннотация: Mossbauer measurements reveal four inequivalent Fe sites in ferrihydrite produced by Klebsiella oxytoca. The origin of these sites can be understood in terms of two nanosized structural regions in the bacterium and a certain ordering of bilayers and single layers of Fe-occupied octahedra.

Журнал: INORGANIC MATERIALS

Выпуск журнала: Vol. 43, Is. 6

Номера страниц: 638-641

ISSN журнала: 00201685

Место издания: NEW YORK

Издатель: MAIK NAUKA/INTERPERIODICA/SPRINGER

• Stolyar S.V. (Krasnoyarsk State University)
• Bayukov O.A. (Kirensky Institute of Physics,Siberian Division,Russian Academy of Sciences)
• Iskhakov R.S. (Kirensky Institute of Physics,Siberian Division,Russian Academy of Sciences)
• Gurevich Yu.L. (Institute of Biophysics,Siberian Division,Russian Academy of Sciences)
• Ladygina V.P. (Institute of Biophysics,Siberian Division,Russian Academy of Sciences)
• Pustoshilov P.P. (Institute of Biophysics,Siberian Division,Russian Academy of Sciences)

• Web of Science Core Collection
• Scopus
• Ядро РИНЦ (eLIBRARY.RU)
• Список ВАК