From Nano to Micro: Evolution of Magnetic Domain Structures in Multidomain Magnetite
From Nano to Micro: Evolution of Magnetic Domain Structures in Multidomain Magnetite
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DOI:
10.1029/2019gc008319
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发表时间:
2019-06-01
影响因子:
3.5
通讯作者:
Muxworthy, Adrian R.
中科院分区:
文献类型:
--
作者:
Nagy, Lesleis;Williams, Wyn;Muxworthy, Adrian R.
Reliability of magnetic recordings of the ancient magnetic field is strongly dependent on the magnetic mineralogy of natural samples. Theoretical estimates of long-term stability of remanence were restricted to single-domain (SD) states, but micromagnetic models have recently demonstrated that the so-called single-vortex (SV) domain structure can have even higher stability that SD grains. In larger grains ( ?10 mu m in magnetite) the multidomain (MD) state dominates, so that large uniform magnetic domains are separated by narrow domain walls. In this paper we use a parallelized micromagnetic finite element model to provide resolutions of many millions of elements allowing us, for the first time, to examine the evolution of magnetic structure from a uniform state, through the SV state up to the development of the domain walls indicative of MD states. For a cuboctahedral grain of magnetite, we identify clear domain walls in grains as small as similar to 3 mu m with domain wall widths equal to that expected in large MD grains; we therefore put the SV to MD transition at similar to 3 mu m for magnetite and expect well-defined, and stable, SV structures to be present until at least similar to 1 mu m when reducing the grain size. Reducing the size further shows critical dependence on the history of domain structures, particularly with SV states that transition through a so-called unstable zone leading to the recently observed hard-aligned SV states that proceed to unwind to SD yet remain hard aligned.