One-Dimensional Liesegang Phenomena under the Influence of Electric and Magnetic Fields

1971 ◽  
Vol 31 (1) ◽  
pp. 39-43 ◽  
Author(s):  
Shouji Shinohara
Keyword(s):  
Magnetic Fields ◽  
One Dimensional ◽  
Electric And Magnetic Fields

Quantisation of the conductance in units of e2/2h in a ballistic quasi-one-dimensional channel, produced by strong electric and magnetic fields

1992 ◽  
Vol 11 (2) ◽  
pp. 233-235 ◽  
Author(s):  
N.K. Patel ◽  
L. Martín-Moreno ◽  
J.T. Nicholls ◽  
M. Pepper ◽  
J.E.F. Frost ◽  
...  
Keyword(s):  
Magnetic Fields ◽  
One Dimensional ◽  
Electric And Magnetic Fields

scholarly journals Eindimensionale Plasmaströmung in gekreuzten elektrischen und magnetischen Feldern

1965 ◽  
Vol 20 (8) ◽  
pp. 1019-1026 ◽  
Author(s):  
E. Rebhan
Keyword(s):  
Magnetic Field ◽  
Magnetic Fields ◽  
Field Strength ◽  
Shock Front ◽  
Magnetic Field Strength ◽  
Plasma Flow ◽  
One Dimensional ◽  
Electric And Magnetic Fields ◽  
The Magnetic Field ◽  
Steady Shock

An investigation was made of a steady, one-dimensional plasma flow in crossed electric and magnetic fields. The interaction between the flow and the fields causes various flow types. In general, the flow is either supersonic or subsonic in the entire channel. Under certain circumstances, however, a transsonic flow may develop. Finally, flows exist with a steady shock front, the position and strength of which depend on the magnetic field strength and the pressure at the end of the tube.

Magnetotelluric data analysis: removal of bias

Geophysics ◽  
1978 ◽  
Vol 43 (6) ◽  
pp. 1157-1166 ◽  
Author(s):  
Wolfgang M. Goubau ◽  
Thomas D. Gamble ◽  
John Clarke
Keyword(s):  
Magnetic Fields ◽  
Reference Signal ◽  
Impedance Tensor ◽  
Magnetotelluric Data ◽  
New Techniques ◽  
One Dimensional ◽  
Strike Direction ◽  
Electric And Magnetic Fields ◽  
A Site ◽  
Correlated Noises

Two new techniques for analyzing 4‐channel magnetotelluric (MT) data are described. These techniques produce estimates of the elements [Formula: see text] of the impedance tensor that are unbiased by noise in the autopowers of the electric and magnetic fields. Effectively, each technique uses one field channel as a reference signal that can be correlated with the other three channels. Method 1 obtains estimates for the [Formula: see text] in terms of crosspowers of the Fourier components of the electric and magnetic fields [Formula: see text], [Formula: see text], [Formula: see text], and [Formula: see text]. Method 2 is a generalization of method 1, and obtains estimates for [Formula: see text] in terms of weighted crosspowers. Both methods fail when the geology is one‐dimensional, or two‐dimensional with one electrode oriented along the strike direction. To obtain results that are stable for any geology and that are unbiased by autopower noise, at least five channels of data are required. To also minimize bias by correlated noises, one needs six channels of data, two channels of which are for fields measured at a site that is remote from the base MT station. The analysis of MT data using a remote magnetometer as a reference is discussed.

49. Evaluation of Electric and Magnetic Fields Around an Induction Cap Sealer

1999 ◽  
Author(s):  
F. Rosenthal ◽  
M. Carter ◽  
S. Hampton ◽  
T. Mays
Keyword(s):  
Magnetic Fields ◽  
Electric And Magnetic Fields

Electric and magnetic fields at power frequencies

2010 ◽  
Vol 29 (Supplement 1) ◽  
pp. 69-83
Author(s):  
Anthony B. Miller ◽  
Lois M. Green
Keyword(s):  
Magnetic Fields ◽  
Electric And Magnetic Fields
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