Theory of Stable Multidomain Thermoviscous Remanence Based on Repeated Domain Wall Jumps

被引:7
作者
Berndt, Thomas A. [1 ]
Chang, Liao [1 ,2 ]
机构
[1] Peking Univ, Sch Earth & Space Sci, Lab Orogen Belts & Crustal Evolut, Beijing, Peoples R China
[2] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao, Peoples R China
关键词
multidomain grains; thermoremanent magnetization; viscous remanent magnetization; magnetic domain state; rock and mineral magnetism; FIELD PARTIAL THERMOREMANENCE; PSEUDO-SINGLE; FERROMAGNETIC GRAINS; 1ST-ORDER SYMMETRY; MAGNETIZATION; TEMPERATURE; MAGNETITE; MODEL; PALEOMAGNETISM; ACQUISITION;
D O I
10.1029/2018JB016816
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We developed a theory of multidomain (MD) thermoviscous remanence that can be solved analytically to yield an expression relating the blocking temperature of a MD grain to its relaxation time. This expression is analogous to Neel's widely used theory of single-domain (SD) thermoviscous remanence but yields a different time-temperature relationship. The theory is based on a two-domain model with a domain wall (DW) that can jump between different pinning sites. In contrast to previous theories of this kind, our theory considers repeated DW jumps rather than a single jump in isolation. It is shown that while SD remanence behavior is fully described by the two quantities (V,H-K0), that is, volume and microscopic coercivity, MD particle remanence depends on three quantities: volume, Barkhausen volume, and DW pinning field, denoted (V,V-Bark,H-K0). Pullaiah nomograms of this new theory show that while small MD grains behave almost identically to SD grains, larger grains show different slopes depending on the above quantities. The theory predicts that MD grains can be highly stable remanence carriers, in particular showing a high thermal stability. Grains with weak pinning fields, however, while thermally stable, are highly unstable under alternating field (AF) demagnetization, being demagnetized under fields of a few millitesla. Our theory also explains (1) why samples dominated by MD grains show curved vector demagnetization plots for both thermal and AF demagnetization, as well as (2) why MD grains affect thermal demagnetization plots even at high temperatures, while their remanence is completely removed within the first few AF demagnetization steps.
引用
收藏
页码:10399 / 10417
页数:19
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