Abstract
We investigated the surface and interior magnetic domains by using magnetic force microscopy for two types of Tb <sub xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">0.3</sub> Dy <sub xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">0.7 </sub> Fe <sub xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">1.95</sub> crystal growing along the lang110rang direction: 1) crystals annealed at 673 K for 2 h in higher vacuum (5times10 <sup xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">-5</sup> Pa) and 2) crystals annealed at 723 K for 2 h in lower vacuum (5times10 <sup xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">-3</sup> Pa). For the former, we observed fine stripe-like domains at the surface. For the latter, we observed the interior domains of the specimen; these were also stripe-like, but with larger average width than the surface domains. X-ray diffraction patterns indicate the formation of a thin iron layer in the surface of the specimens annealed in the lower vacuum. The iron layer, as a "capping" layer, actually acts as a shielding layer for the stray fields emerging from the interior domains underneath, resulting in the wide interior domains
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