Modeling of magnetic hysteresis parameters in foraminiferal shells of the Mid-Atlantic Ridge

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Resumo

The composition and magnetic properties of foraminifers from bottom sediments of the Mid-Atlantic Ridge and their artificial analogues obtained by hydrothermal synthesis have been studied. The presence of magnetic hysteresis and theoretical modeling of hysteresis characteristics made it possible to assume the presence of grains of nonstoichiometric magnetite in single and low-domain states.

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Sobre autores

E. Sergienko

Saint Petersburg University

Email: kggareev@etu.ru
Rússia, St. Petersburg, 199034

S. Janson

Saint Petersburg University

Email: kggareev@etu.ru
Rússia, St. Petersburg, 199034

K. Gareev

Saint Petersburg Electrotechnical University “LETI”

Autor responsável pela correspondência
Email: kggareev@etu.ru
Rússia, St. Petersburg, 197022

P. Kharitonskii

Ioffe Institute

Email: kggareev@etu.ru
Rússia, St. Petersburg, 194021

A. Ralin

Far Eastern Federal University

Email: kggareev@etu.ru
Rússia, Vladivostok, 690922

T. Sheidaev

Saint Petersburg Electrotechnical University “LETI”

Email: kggareev@etu.ru
Rússia, St. Petersburg, 197022

E. Setrov

Saint Petersburg Electrotechnical University “LETI”

Email: kggareev@etu.ru
Rússia, St. Petersburg, 197022

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2. Fig. 1. Optical images of foraminifera samples: F1 – Globorotalia menardii (a), F2 – Orbulina universa (b), Fs1 – Globorotalia menardii (c), Fs2 – Orbulina universa (d), Fs3 – Globigerinoides conglobatus (d), Fart – Orbulina universa (e).

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3. Fig. 2. Hysteresis loops in a field less than 1 T and demagnetization curves by a reverse field: sample F1 (a), F2 (b), Fs1 (c), Fs2 (d), Fs3 (d), Fart (e). The saturation magnetization values ​​obtained in a field of 7 T are given in Table 3.

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