金红石与石榴石浮选分离及调整剂作用机理

为了实现金红石与主要脉石矿物石榴石在无污染条件下的有效分离,采用浮选方法研究了金红石和石榴石的分离,并采用红外光谱和X光电子能谱分析等手段研究了分离过程中调整剂六偏磷酸钠的作用机理。结果表明,以烷胺双甲基磷酸(ATF1024)为捕收剂,六偏磷酸钠[(NaPO3)6]为调整剂,可以实现金红石与石榴石之间的浮选分离。(NaPO3)6对石榴石的抑制作用存在两种机理:其一,(NaPO3)6与石榴石表面Fe2 发生化学键合导致其牢固吸附而使石榴石表面强烈亲水;其二,(NaPO3)6选择性溶解石榴石表面Ca2 导致石榴石与捕收剂作用的表面活性质点减少。     

Almandine megacrysts from Yingfengling Cenozoic basalt in Leizhou Peninsula and their parental magma origin

The garnet megacrysts from Yingfengling basalts are characterized by high FeO (>20%), CaO (7.02% –8.16%) and low MgO (5.88%–10.87%). Significant composition variations are observed in these megacrysts, of which Ni, V, Sc, Co, and HREE are positively correlated with their Mg^#, and Zr, Hf, Ga, Y, Sr, Nb, Zn and LREE-MREE are negatively correlated with Mg^#. Megacryst parent magma is a highly evolved residual melt with strongl depletion in Ti, Sr, Hf, Nb and HREE. This parental magma was generated by more than 60% of crystallization fractionation of clinopyroxene, garnet, plagioclase and ilmenite from quartz tholeiitic magma. It has not erupted to the surface, but stayed at the upper mantle and formed the megacrystic cumulate. Megacrysts and their host basalt are in disequilibrium.