Author/Authors :
Franc¸ois Prud’hommeb، نويسنده , , Maurice Morencya، نويسنده , , b، نويسنده , , U، نويسنده , , Klaus Freyerd، نويسنده , ,
Holger Weissc، نويسنده , , James Bourneb، نويسنده , , Brigit Dausc، نويسنده , , Denise Fontaineb، نويسنده , ,
Jurgen Mattuschc، نويسنده , , Raymond Mineaub، نويسنده , , Michel Pr´edab، نويسنده , , Hanns-Christian Treutler، نويسنده , , Reiner Wennrichd، نويسنده ,
Abstract :
When characterizing multi-phase materials, several authors have recommended separating the material into
various fractions consisting of a reduced number of minerals. However, the common separation techniques are of
limited value when treating ultra-fine-grained materials. We present in this paper a separation technique using
tensio-active solutions which break up any particle agglomerates which may be present and facilitates sedimentation
of component particles according to grain size. These fractions have a distinctive mineralogy and chemistry. The
technique has been applied to two selected samples from two mining residue sites in Germany. Results from Bielatal,
a tin residue, show that a large proportion of the arsenic and heavy metals are concentrated in a suspension fraction,
which consists of clay minerals and amorphous iron oxyhydroxides. Silicates such as a micas and feldspar settle out
quite rapidly, whereas, other minerals, such as hematite take longer. In the case of D¨ankritz, a uranium mine waste,
the same technique was applied and similar results were obtained for the heavy metals distribution. Additional study
indicated that radium is with barite and other radio-isotopes were associated with the fine suspension fraction.