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This article is cited in 2 scientific papers (total in 2 papers)
Day plots of bacterial magnetite from sediments of Shira lake (Khakassia, Russia)
Sergey V. Semenovab, Dmitry A. Balaevab, Kirill A. Shaykhutdinovb, Denis Yu. Rogozinca a Siberian Federal University, Svobodny, 79, Krasnoyarsk, 660041,
Russia
b Kirensky Institute of Physics SB RAS,
Akademgorodok, 50/38, Krasnoyarsk, 660036, Russia
c Institute of Biophysics SB RAS, Akademgorodok, 50/50, Krasnoyarsk, 660036, Russia
Abstract:
The domain state of magnetite detected in sediments of Shira lake (Khakassia, Russia) was examined by means of magnetic hysteresis. Analysis of experimental data obtained on samples from different parts of bottom sediment cores in terms of Day plots allowed us to conclude that magnetite particles are in the pseudo-single-domain state. This indicates respectively small size of magnetite particles ($< 100$ nm) and reveals their bacterial origin. Biogenic magnetite buried in the bottom sediments can indicate the climatic changes in the Shira lake level in the Late Holocene.
Keywords:
nanoparticles, magnetic hysteresis, bacterial magnetite.
Received: 10.08.2016 Received in revised form: 10.11.2016 Accepted: 20.01.2017
Citation:
Sergey V. Semenov, Dmitry A. Balaev, Kirill A. Shaykhutdinov, Denis Yu. Rogozin, “Day plots of bacterial magnetite from sediments of Shira lake (Khakassia, Russia)”, J. Sib. Fed. Univ. Math. Phys., 10:2 (2017), 252–256
Linking options:
https://www.mathnet.ru/eng/jsfu548 https://www.mathnet.ru/eng/jsfu/v10/i2/p252
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