Abstract

The magnetic susceptibility and magnetic resonance spectroscopy of coals doped with Ni have been measured as a function of heat treatment temperature (HTT). Both the susceptibilities and magnetic resonance signals began increasing at HTT of 300 to 500°C by a factor of 10 2 to 10 3. The HTT corresponding to this steep increase shifted to higher temperatures with coal rank; 300°C for brown coal, 400°C for bituminous coal and 500°C for anthracite. With the changes in the magnetic properties, the state of aggregation of Ni particles in coals changed. From the parameters of magnetic resonance spectroscopy combined with x-ray diffraction data, it is presumed that ultrafine Ni particles (<100 Å) showing superparamagnetic behavior were formed in the brown coal, whereas relatively larger Ni particles (>100 Å) were produced in the bituminous coal and anthracite.

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