Abstract
The relative Fe2+ ion concentrations in three flux‐grown crystals of YIG(Si), containing up to 0.3 Si4+ ion per formula unit, have been determined by optical techniques. The Fe2+ ion concentration appears to reach a maximum or saturation value at Si4+ ion content of 0.1 per formula unit. The Si4+ ions not compensated by Fe2+ or Pb2+ ions, the sum of which is less than the Si4+ ion content, must be compensated by cation vacancies.