Ding Kaiwei, Qiu Tingsheng, Qiu Xianhui, Zhao Guanfei, Jiao Qinghao, Fang Jiangjie, Lai Ruisen, Yang Wenhui
College of Resource and Environmental Engineering, Jiangxi University of Science and Technology, Ganzhou 341000, China.
Jiangxi Provincial Key Laboratory of Low-Carbon Processing and Utilization of Strategic Metal Mineral Resources, Ganzhou 341000, China.
Molecules. 2024 Sep 4;29(17):4194. doi: 10.3390/molecules29174194.
The floatability of fluorite and calcite exhibit similar properties, rendering their flotation separation challenging. Macromolecular polysaccharide reagents containing the polyhydroxyl group have shown broad promising application. The selectivity of polysaccharide is relatively low. In this study, the introduction of Fe was employed to enhance the selective adsorption capacity of Pullulan polysaccharide towards fluorite and calcite minerals, thereby achieving effective flotation separation. Furthermore, the mechanism underlying intramolecular interactions was elucidated. The DFT calculation and XPS analysis revealed that the adsorption of Fe on the calcite surface was more favorable, leading to the formation of a Ca-O-Fe structure. The MD simulation, XPS analysis, and Zeta potential analysis revealed that the Fe-OH groups on the surface of calcite reacted with the -OH groups in Pullulan and formed bonds, resulting in the formation of a Calcite-Fe-Pullulan structure. This facilitated the attachment of a significant number of Pullulan molecules to the calcite surface. The formation of a hydrophilic layer on the outer surface of calcite by Pullulan, in contrast to the absence of such layer on fluorite's surface, results in an increased disparity in surface floatability between these two minerals, thereby enhancing the efficiency of flotation separation.
萤石和方解石的可浮性表现出相似的性质,这使得它们的浮选分离具有挑战性。含有多羟基的大分子多糖试剂已显示出广阔的应用前景。多糖的选择性相对较低。在本研究中,引入铁以增强普鲁兰多糖对萤石和方解石矿物的选择性吸附能力,从而实现有效的浮选分离。此外,还阐明了分子内相互作用的机制。密度泛函理论(DFT)计算和X射线光电子能谱(XPS)分析表明,铁在方解石表面的吸附更有利,导致形成Ca-O-Fe结构。分子动力学(MD)模拟、XPS分析和ζ电位分析表明,方解石表面的Fe-OH基团与普鲁兰中的-OH基团反应并形成键,从而形成方解石-Fe-普鲁兰结构。这有利于大量普鲁兰分子附着在方解石表面。与萤石表面不存在这种层相反,普鲁兰在方解石外表面形成亲水性层,导致这两种矿物之间表面可浮性的差异增加,从而提高了浮选分离效率。