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磁铁矿对微波的吸收:一种将非热辐射水平与生物系统耦合的可能机制。

Microwave absorption by magnetite: a possible mechanism for coupling nonthermal levels of radiation to biological systems.

作者信息

Kirschvink J L

机构信息

Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, USA.

出版信息

Bioelectromagnetics. 1996;17(3):187-94. doi: 10.1002/(SICI)1521-186X(1996)17:3<187::AID-BEM4>3.0.CO;2-#.

Abstract

The presence of trace amounts of biogenic magnetite (Fe3O4) in animal and human tissues and the observation that ferromagnetic particles are ubiquitous in laboratory materials (including tissue culture media) provide a physical mechanism through which microwave radiation might produce or appear to produce biological effects. Magnetite is an excellent absorber of microwave radiation at frequencies between 0.5 and 10.0 GHz through the process of ferromagnetic resonance, where the magnetic vector of the incident field causes precession of Bohr magnetons around the internal demagnetizing field of the crystal. Energy absorbed by this process is first transduced into acoustic vibrations at the microwave carrier frequency within the crystal lattice via the magnetoacoustic effect; then, the energy should be dissipated in cellular structures in close proximity to the magnetite crystals. Several possible methods for testing this hypothesis experimentally are discussed. Studies of microwave dosimetry at the cellular level should consider effects of biogenic magnetite.

摘要

动物和人体组织中存在痕量的生物源磁铁矿(Fe3O4),以及在实验室材料(包括组织培养基)中普遍存在铁磁性颗粒这一现象,提供了一种物理机制,通过该机制微波辐射可能产生或看似产生生物学效应。磁铁矿通过铁磁共振过程,在0.5至10.0 GHz频率范围内是微波辐射的优良吸收体,在此过程中,入射场的磁矢量会导致玻尔磁子围绕晶体的内部退磁场做进动。此过程吸收的能量首先通过磁声效应在晶格内以微波载波频率转换为声振动;然后,能量应在紧邻磁铁矿晶体的细胞结构中耗散。文中讨论了几种通过实验检验该假设的可能方法。细胞水平的微波剂量学研究应考虑生物源磁铁矿的影响。

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