Magnetic properties of hydrothermally synthesized greigite (F3S4) -: II.: High- and low-temperature characteristics

被引:116
作者
Dekkers, MJ
Passier, HF
Schoonen, MAA
机构
[1] Univ Utrecht, Inst Earth Sci, Palaeomagnet Lab Ft Hoofddijk, NL-3584 CD Utrecht, Netherlands
[2] SUNY Stony Brook, Dept Geosci, Stony Brook, NY 11794 USA
关键词
alteration; greigite; hydrothermal synthesis; magnetic properties;
D O I
10.1046/j.1365-246x.2000.00129.x
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
The magnetic behaviour of hydrothermally synthesized greigite was analysed in the temperature range from 4 K to 700 degrees C. Below room temperature, hysteresis parameters were determined as a function of temperature, with emphasis on the temperature range below 50 K. Saturation magnetization and initial susceptibility were studied above room temperature, along with X-ray diffraction analysis of material heated to various temperatures. The magnetic behaviour of synthetic greigite on heating is determined by chemical alteration rather than by magnetic unblocking. Heating in air yields more discriminative behaviour than heating in argon. When heated in air, the amount of oxygen available for reaction with greigite determines the products and magnetic behaviour. In systems open to contact with air, haematite is the final reaction product. When the contact with air is restricted, magnetite is the final reaction product. When air is excluded, pyrrhotite and magnetite are the final reaction products; the amount of magnetite formed is determined by the purity of the starting greigite and the degree of its surficial oxidation. The saturation magnetization of synthetic greigite is virtually independent of temperature from room temperature down to 4 K. The saturation remanent magnetization increases slowly by 20-30 per cent on cooling from room temperature to 4 K. A broad maximum is observed at similar to 10 It which may be diagnostic of greigite. The coercive and remanent coercive force both increase smoothly with decreasing temperature to 4 K. The coercive force increases from similar to 50 mT at room temperature to approximately 100-120 mT at 4 K, and the remanent coercive force increases from approximately 50-80 mT at room temperature to approximately 110-180 mT at 4 K.
引用
收藏
页码:809 / 819
页数:11
相关论文
共 58 条
[1]  
[Anonymous], 1999, Quaternary climates, environments, and magnetism, DOI DOI 10.1017/CB09780511535635.007
[2]  
[Anonymous], 1992, J PALEOLIMNOL, DOI DOI 10.1007/BF00181713
[3]   INFLUENCE OF NONSTOICHIOMETRY ON THE VERWEY TRANSITION [J].
ARAGON, R ;
BUTTREY, DJ ;
SHEPHERD, JP ;
HONIG, JM .
PHYSICAL REVIEW B, 1985, 31 (01) :430-436
[4]  
Banerjee S. K., 1995, ROCK PHYS PHASE RELA, V3, P189, DOI [10.1029/RF003p0189, DOI 10.1029/RF003P0189]
[5]   THERMODYNAMIC STABILITY OF SEDIMENTARY IRON SULFIDES [J].
BERNER, RA .
AMERICAN JOURNAL OF SCIENCE, 1967, 265 (09) :773-&
[6]  
BUCKLEY AN, 1985, APPL SURF SC, V22-3, P280, DOI 10.1016/0378-5963(85)90061-3
[7]   THE SURFACE OXIDATION OF PYRITE [J].
BUCKLEY, AN ;
WOODS, R .
APPLIED SURFACE SCIENCE, 1987, 27 (04) :437-452
[8]   MAGNETIC STRUCTURE OF SPINEL FE3S4 [J].
COEY, JMD ;
SPENDER, MR ;
MORRISH, AH .
SOLID STATE COMMUNICATIONS, 1970, 8 (20) :1605-&
[9]  
Collinson D.W., 1983, METHODS ROCK MAGNETI
[10]   Magnetic properties of hydrothermally synthesized greigite (Fe3S4) .1. Rock magnetic parameters at room temperature [J].
Dekkers, MJ ;
Schoonen, MAA .
GEOPHYSICAL JOURNAL INTERNATIONAL, 1996, 126 (02) :360-+