首页> 外文期刊>Brazilian journal of chemical engineering >EFFECT OF DISSOLUTION KINETICS ON FLOTATION RESPONSE OF CALCITE WITH OLEATE
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EFFECT OF DISSOLUTION KINETICS ON FLOTATION RESPONSE OF CALCITE WITH OLEATE

机译:溶出动力学对岩石铝浮选响应的影响

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Phosphate flotation performance can be influenced by the dissolution kinetics of the minerals that compose the ore. The purpose of this work was to investigate the effect of dissolution kinetics on flotation response with oleate (collector) of calcites from different origins and genesis. The calcite samples were first purified and characterized by x-ray Fluorescence (XRF) and the Rietveld method applied to x-ray Diffractometry data (RXD). Experiments of calcite dissolution and microflotationwere performed at pH 8 and pH 10. The pH effect on the calcite dissolution and flotation indicates the possible influence of the carbonate/bicarbonate ions provided by the CO2 present in the air. In addition, the flotation response is greater as the dissolution increases, making more Ca2+ ions available to interact with collector molecules. This result corroborates the surface precipitation mechanism proposed foroleate adsorption on the calcite surface.
机译:磷酸浮选性能可以受到构成矿石的矿物质的溶解动力学的影响。 这项工作的目的是探讨溶解动力学对来自不同起源和创世纪的钙化岩石(收集器)对浮选响应的影响。 首先通过X射线荧光(XRF)和施加到X射线衍射测定数据(RXD)的RIETVELD方法以纯化的方解石样品。 在pH8和pH10中进行的方解石溶解和微型荧光卷发的实验。对方解石溶解和浮选的pH效应表明碳酸盐/碳酸氢盐离子的可能影响在空气中存在。 另外,随着溶解的增加,浮选响应更大,使得更多的Ca2 +离子可用于与收集剂分子相互作用。 该结果证实了所提出的表面沉淀机制在方解石表面上的吸附。

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