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Electrokinetic properties of hydroxyapatite under flotation conditions

机译:浮选条件下羟基磷灰石的电动特性

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The effect of calcite supernatant, calcium, and carbonate ions on the hydroxyapatite (HA) zeta potential without and in the presence of sodium oleate (1 × 10~(-4) mol L~(-1)) was examined within the pH range from 4 to 12. The interpretation of results was based on the HA surface and oleate solution chemistry, and on some floatability tests. HA, with different positive and negative surface sites formed depending on its solubility and pH, had a negative zeta potential over the whole pH range. This mineral is not naturally floatable (flotation recovery, 5% < R < 18%). The oleate ions (Ol~-), present in a very low concentration in an acidic medium (pH from 4.8 to 6), chemisorb individually on HA surface centers {triple bond, long}Ca~+, {triple bond, long}HPO_4Ca~+, and {triple bond, long} OH_2~+, increasing the negative zeta potential of the mineral. Within the pH range from 7 to 9, the dominant oleate species Ol- ion and ion-molecule complex, H (Ol)_2~-, adsorbed on HA by head groups toward the solid and associated due to chain-chain interaction in hemimicelles, made the HA surface with zeta potential about -22/-23 mV, and more floatable (R = 80-100%) than in 4 < pH < 7 (R = 15-35%) or in pH > 9.3. The HA surface is less negatively charged in calcite supernatant than in water from pH 6.6 to 9.2 due to the adsorption on HA negative surface active centers ({triple bond, long} HPO_4~- and {triple bond, long} PO_4~(2 -)) of the Ca~(2+), CaHCO_3~+, and CaOH~+ ions (present in the calcite supernatant), producing more surface sites {triple bond, long}HPO_4Ca~+, {triple bond, long}PO_4Ca, {triple bond, long}HPO_4CaOH, and {triple bond, long} PO_4~- CaOH, and new centers {triple bond, long}HPO_4CaHCO~3 and {triple bond, long} PO_4~- CaHCO~3. In the presence of 1 × 10~(-3) mol L~(-1) CaCl_2, the HA sample has positive zeta potential, the same as calcite from the same deposit, up to IEP at pH 11.25. Carbonate ions (1 × 10~(-3) mol L~(-1) Na_2CO_ 3) do not affect the HA zeta potential. However, a possible process can be the ion-exchange reaction between bicarbonate (or carbonate) and some anion from the surface sites formed on HA. The obtained values of the HA zeta potential with the collector (1 × 10~(-4) mol L~(-1) Na-oleate) added into hydroxyapatite/calcite supernatant suspensions corroborate the weak chemisorption of Ol- and H (Ol)_2~-. The likely processes in this system also are the ion-exchange reactions on {triple bond, long}HPO_4CaOH and {triple bond, long} PO_4~- CaOH, {triple bond, long}HPO_4CaHCO_3 and {triple bond, long} PO_4~- CaHCO_3 between oleate ion and surface hydroxyl and bicarbonate ions, surface and bulk precipitations of calcium oleate, Ca(Ol)_2, and the surface and bulk precipitations of Ca [H (Ol)_2~-]_2 over the pH range from 7 to 9. Calcite supernatant does not influence natural floatability of the mineral. However, calcite supernatant depresses the hydroxyapatite flotation in the presence of 1 × 10~(-4) mol L~(-1) Na-oleate (pH 9, R ~ 50%), a likely result of the weak chemisorption due to the steric effect of heterogeneous HA surface formed in calcite supernatant, Ca(Ol)_2 and Ca [H (Ol)_2~-]_2 surface and bulk precipitations.
机译:在pH范围内,检查了无油酸钠(1×10〜(-4)mol L〜(-1))下方解石上清液,钙和碳酸根离子对羟基磷灰石(HA)ζ电位的影响。从4到12。结果的解释是基于HA表面和油酸盐溶液的化学性质,以及一些漂浮性测试。 HA的溶解度和pH值不同,会形成不同的正负表面位点,在整个pH范围内其zeta电位均为负。该矿物质不是天然漂浮的(浮选回收率,5% 9.3更高的漂浮性(R = 80-100%)。由于在HA负表面活性中心上的吸附({三键,长} HPO_4〜-和{三键,长} PO_4〜(2--),方解石上清液中HA表面的负电荷比pH 6.6至9.2的水中的负电荷少。 ))中的Ca〜(2 +),CaHCO_3〜+和CaOH〜+离子(存在于方解石上清液中),产生更多的表面位点{三重键,长} HPO_4Ca〜+,{三重键,长} PO_4Ca, {三键,长} HPO_4CaOH和{三键,长} PO_4〜-CaOH,以及新的中心{三键,长} HPO_4CaHCO〜3和{三键,长} PO_4〜-CaHCO〜3。在存在1×10〜(-3)mol L〜(-1)CaCl_2的情况下,HA样品具有正zeta电位,与来自同一沉积物的方解石相同,直至pH为11.25的IEP。碳酸根离子(1×10〜(-3)mol L〜(-1)Na_2CO_ 3)不会影响HA Zeta电位。但是,可能的过程可能是碳酸氢根(或碳酸根)与来自HA上形成的表面部位的某些阴离子之间的离子交换反应。将收集剂(1×10〜(-4)mol L〜(-1)油酸钠)添加到羟基磷灰石/方解石上清液悬浮液中得到的HAζ电位值证实了Ol-和H(Ol)的弱化学吸附_2〜-。该系统中可能的过程还包括对{三键,长} HPO_4CaOH和{三键,长} PO_4〜-CaOH,{三键,长} HPO_4CaHCO_3和{三键,长} PO_4〜-的离子交换反应CaHCO_3在油酸离子与表面羟基和碳酸氢根离子之间,油酸钙,Ca(Ol)_2的表面和整体沉淀,以及Ca [H(Ol)_2〜-] _ 2的表面和整体沉淀,pH范围为7至9.方解石上清液不会影响矿物的自然漂浮性。然而,方解石上清液在存在1×10〜(-4)mol L〜(-1)油酸钠(pH 9,R〜50%)的情况下抑制了羟基磷灰石的浮选,这可能是由于化学吸附较弱所致。方解石上清液,Ca(Ol)_2和Ca [H(Ol)_2〜-] _ 2表面及大量沉淀物中形成的异质HA表面的空间效应。

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