LiGa5O8中Co2+的光学检测核磁共振

R. Wannemacher, S. Magnien, W. Grill
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引用次数: 0

摘要

光谱烧孔已被证明是探测稀土离子基态和光激发态下超精细[1]和超精细[2]相互作用的一种有价值的工具。如果空穴燃烧机制是在电子基态的超精细或超精细水平上的居群存储,则应用与分裂共振的射频磁场改变光谱空穴的深度,可以在吸收或荧光[3]中监测。这种双共振技术,通常被称为“光学检测磁共振”,ODMR(稀土离子的应用概述见[1]),原则上能够分别检测基态和激发态的超细和超细[4]分裂。此外,该技术的分辨率是由核磁共振的线宽决定的,而不是由激光线宽决定的,激光线宽只需要小于分裂,就可以实现光谱烧孔。
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Optically Detected Nuclear Magnetic Resonance of Co2+ in LiGa5O8
Optical spectral hole-burning has proven to be a valuable tool for the detection of hyperfine [1] as well as superhyperfine [2] interactions in ground and optically excited states of rare earth ions. In cases where the hole-burning mechanism is population storage in hyperfine or superhyperfine levels of the electronic ground state, the application of an rf-magnetic field resonant with the splittings changes the depth of the spectral hole, which can be monitored either in absorption or in fluorescence [3]. This double resonance technique, commonly termed 'Optically Detected Magnetic Resonance', ODMR (for an overview of applications to rare earth ions see [1]), is in principle able to detect hyperfine as well as superhyperfine [4] splittings of ground and excited [5] states separately. Moreover, the resolution of this technique is determined by the linewidth of the nuclear magnetic resonance and not by the laser linewidth, which only needs to be smaller than the splittings in order to enable spectral hole-burning.
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