scholarly journals POSSIBLE CAUSES OF CHANGE IN THE DIRECTION OF EARTH'S MAGNETIC FIELD

2016 ◽  
Vol 7 (2) ◽  
Author(s):  
Dragana Malivuk Gak ◽  
Saša Nježić ◽  
Enes Škrgić ◽  
Zoran Rajilić

The study of the magnetic properties of materials have attracted the interest of scientists for ages. Knowing the magnetic properties of materials do their best possible use in industry and technology, as well as better understanding of some yet unexplained phenomena in nature related to the Earth's magnetic field. Several models that describe the given phenomenon are known, such as the domino model, two-dimensional Ising model and model of inversion magnetic Earth's field. In computer experiments whose results are presented in this paper, it is used a simplified two-dimensional Ising model, one version of the model related spins. Computer experiments (simulations) are made in the mathematical software Maple. It has been observed reversing the direction of magnetization in a small change of inhomogeneity energy interactions. Consideration of this issue could be of importance for the study of ferromagnetic material.

2006 ◽  
Vol 182 (2) ◽  
pp. 343-347 ◽  
Author(s):  
Jeremy N. Robinson ◽  
Andrew Coy ◽  
Robin Dykstra ◽  
Craig D. Eccles ◽  
Mark W. Hunter ◽  
...  

Geophysics ◽  
1940 ◽  
Vol 5 (3) ◽  
pp. 295-306 ◽  
Author(s):  
Harold H. Pentz

Curves and formulas for the interpretation of the two‐dimensional “dike” and “step” are given because they offer an easy, rapid method of solving all cases to which they apply. Horizontal and vertical polarization of the bodies are considered. This method applies to torsion balance surveys, and to magnetic surveys where the horizontal and vertical components of the earth’s magnetic field are measured. Two curves for the interpretation of an anomaly in terms of a point pole (or a point mass) are given. The depth to the two‐dimensional structures is considered, with formulas and curves.


1996 ◽  
Vol 17 (2) ◽  
pp. 225-228
Author(s):  
Kenneth L. Verosub ◽  
Elbridge Gerry Puckett ◽  
Igor Aleninov ◽  
David J. Barsky ◽  
Janko Gravnor ◽  
...  

2010 ◽  
Vol 54 (4) ◽  
pp. 575-593 ◽  
Author(s):  
Modesto Pineda Duran ◽  
Avto Goguitchaichvili ◽  
Juan Morales ◽  
Bertha Aguilar Reyes ◽  
Luis M. Alva Valdivia ◽  
...  

Author(s):  
A. Soloviev ◽  
A. Khokhlov ◽  
E. Jalkovsky ◽  
A. Berezko ◽  
A. Lebedev ◽  
...  

2011 ◽  
Vol 12 (2) ◽  
pp. 1-9
Author(s):  
A. E. Berezko ◽  
A. V. Khokhlov ◽  
A. A. Soloviev ◽  
A. D. Gvishiani ◽  
E. A. Zhalkovsky ◽  
...  

1967 ◽  
Vol 20 (1) ◽  
pp. 101 ◽  
Author(s):  
KJW Lynn ◽  
J Crouchley

Results of a study at Brisbane of individual night-time sferics of known origin are described. A propagation attenuation minimum was observed in the 3-6 kHz range. The geographic distribution of sferic types was also examined. Apparent propagation asynunetries were observed, since sferics were detected at greater ranges to the west than to the east at 10 kHz, whilst the number of tweek-sferics arising from the east was about four times that arising from the west. Comparison with European studies suggest that these asymmetries are general. These results are then " interpreted in terms of an ionospheric reflection cgefficient which is a function of the effective angle of incidence of the wave on the ionosphere and of orientation with respect to the Earth's magnetic field within the ionosphere.


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