First‐order reversal curve (FORC) diagrams are constructed from a class of partial magnetic
hysteresis loops known as first‐order reversal curves and are used to understand …

The magnetic domain state of a material determines its magnetic recording capability and
magnetic properties. Constraining the domain state of magnetic components within …

High-resolution first-order reversal curve (FORC) diagrams are increasingly employed to
characterize magnetic minerals in sediments, and especially as a magnetofossil detection …

The term “pseudo‐single domain”(PSD) has been used to describe the transitional state in
rock magnetism that spans the particle size range between the single domain (SD) and …

Electric field control of magnetism provides a promising route towards ultralow power
information storage and sensor technologies. The effects of magneto-ionic motion have …

The magnetic characterization technique of hysteretic materials based on the measurement
of the first-order reversal curves (FORC) is one of the most appealing methods recently …

To develop a full understanding of interactions in nanomagnet arrays is a persistent
challenge, critically impacting their technological acceptance. This paper reports the …

Since their introduction in Earth sciences in 1990, first-order reversal curve (FORC)
measurements have become an important tool for characterizing geologic materials. The …

Remanence magnetization plots (eg, Henkel or δM plots) have been extensively used as a
straightforward way to determine the presence and intensity of dipolar and exchange …

We present an exploration of a family of compositionally complex cubic spinel ferrites
featuring combinations of Mg, Fe, Co, Ni, Cu, Mn, and Zn cations, systematically …