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云南某膠磷礦AMICS工藝礦物學研究及其難選機理探討

Mineralogical analysis of collophane in Yunnan using AMICS and exploration of difficult flotation mechanisms

  • 摘要: 為了深入探討膠磷礦難選的具體原因,采用化學分析、X射線衍射以及礦物自動分析系統(AMICS)測試手段對云南某膠磷礦浮選給料進行了系統深入的工藝礦物學研究,探索了該礦樣難浮選分離的內在機理。結果表明:該樣品中磷主要以氟磷灰石形式存在,其脈石礦物以白云石和石英為主。氟磷灰石的嵌布粒度較細,主要分布于10~75 μm的粒度范圍,其單體解離度為59.17%。除了以單體的形式存在以外,氟磷灰石主要與白云石、石英連生,連生體的質量分數分別為26.23%和9.92%。而白云石和石英的單體解離度相對較低,分別為46.82%和39.10%。進行了粗選脫鎂、一粗兩掃脫硅的閉路流程浮選試驗,獲得了精礦P2O5品位為29.75%、P2O5回收率為81.95%,SiO2品位為12.63%的浮選指標。結合工藝礦物學分析結果,指出該浮選樣品中膠磷礦嵌布粒度細、難以獲得較好的解離度、泥化嚴重是浮選難于獲得更好指標的主要原因。

     

    Abstract: It is a global fact that the mineral ores degrade to the poor grade status and the various properties of ores are adversely altered such as fine dissemination and complex composition due to the continuous exploitation and utilization of phosphate rock resources. Consequently, separation of minerals has become a difficult and daunting task. The automatic mineral identification and characterization system (AMICS) is mostly used only for mineral characterization. There is no much research and literature on process mineralogy that integrates research parameters with flotation test results to quantitatively explore the mechanism of difficulties or problems faced during mineral separation. In this paper, to further explore and analyze the specific reasons for difficult problems faced while separating collophanite, a systematic in-depth mineralogical analysis based on the chemical analyses, X-ray diffraction, and AMICS has been performed on a refractory collophane flotation feed sample from Yunnan, China. The results show that the phosphorus in the sample mainly exists in the form of fluorapatite and also present in the gangue minerals, which are primarily dolomite and quartz. Fluorapatite has a fine dissemination particle size, which is in the range of 10–75 μm with a degree of mineral liberation 59.17%. Apart from existing in the form of liberated particles, fluorapatite is also present in dolomite and quartz as a composite particle and the mass fraction of composition in dolomite and quartz is found to be 26.23% and 9.92%, respectively. Further, dolomite and quartz relatively have a low degree of mineral liberation with the liberation degree of 46.82% and 39.10%, respectively. The closed-circuit flotation test was carried out with a rougher flotation to remove magnesium. Further a roughing and two stages of scavenging is performed which obtained the flotation performance of concentrate P2O5 grade of 29.75%, P2O5 recovery of 81.95%, and SiO2 grade of 12.63%. When the results were studied together with the mineralogical analysis results, it is found that the fine dissemination particle size of collophanite, the poor degree of mineral liberation, and the serious slime generation are the main causes for not able to achieving a better performance in separation of minerals.

     

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