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Role of Dy on the magnetic properties of orthorhombic <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mi>DyFeO</mml:mi><mml:mn>3</mml:mn></mml:msub></mml:math>

Role of Dy on the magnetic properties of orthorhombic <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mi>DyFeO</mml:mi><mml:mn>3</mml:mn></mml:msub></mml:math>

Orthoferrites are a class of magnetic materials with a magnetic ordering temperature above 600 K, predominant $G$-type antiferromagnetic ordering of the Fe-spin system and, depending on the rare-earth ion, a spin reorientation of the Fe spin taking place at lower temperatures. ${\mathrm{DyFeO}}_{3}$ is of particular interest since the spin reorientation …