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On the Determination of Rock‐Magnetic Parameters by Differential Thermal Analysis *
Author(s) -
Vollstädt H.
Publication year - 1968
Publication title -
geophysical journal of the royal astronomical society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0016-8009
DOI - 10.1111/j.1365-246x.1968.tb07136.x
Subject(s) - curie temperature , curie , differential thermal analysis , thermal , differential (mechanical device) , heat capacity , point (geometry) , thermodynamics , specific heat , range (aeronautics) , geology , materials science , geophysics , physics , mathematics , condensed matter physics , geometry , ferromagnetism , optics , diffraction , composite material
Thermodynamic considerations suggest the Curie temperature can be represented by means of differential thermal analysis. For this purpose, the heat capacity is used as parameter for the Curie‐point range; the basic theoretical connections for this are reported. In passing, an account is given of some experimental results as well as of tests made to use magnetic substances with certain characteristic features instead of the usual inert ones.

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