%0 Journal Article %T 羟基磷灰石除氟的实验地球化学研究 %A 任超 %A 王洪涛 %A 季峻峰 %A 李伟 %J 高校地质学报 %D 2016 %X 中国和世界上许多国家(地区) 都面临着饮用水氟含量超标的问题,因此研究氟的环境地球化学行为以及探索除氟 技术和原理至关重要。本实验采用廉价的非金属矿物羟基磷灰石作为吸附材料,研究羟基磷灰石吸附溶解态F-的地球化学 行为和机制,考察反应时间、pH、初始F-浓度等环境参数对吸附反应的影响。实验结果发现羟基磷灰石对F-的吸附反应需 进行到48 h以上时才接近反应平衡。在实验条件下(pH≥4),F-的吸附量随pH升高而降低,羟基磷灰石对F-的吸附受pH 调控。同时还发现羟基磷灰石在pH=6条件下对F-的吸附等温线既满足Langmuir等温模式(R2=0.89) 同时也满足Freundlich 等温模式(R2=0.99),并推导出该条件的理论最大吸附量为21.6×10-3。本研究还进一步采用了先进的XRD、SEM、 HR-TEM、19F NMR手段,系统地表征了反应前后吸附产物的形态和成分变化,发现在高F-浓度条件下,F-在羟基磷灰石表 面的吸附机制不再是单层的表面配位。核磁共振的结果表明F-可部分取代羟基磷灰石结构中的隧道羟基而形成含氟羟基磷 灰石。研究结果表明羟基磷灰石是一种相当具有潜力的除氟材料,值得进一步开发。</br>Geologic fluoride pollution is a worldwide environmental problem, as numerous countries and regions are facing problems that drinking water contains excess F concentration. In this research, we adopted low-cost non-metal mineral hydroxyapatite (HAP) as adsorbent to study the geochemical behavior and mechanism of F adsorption as a function of reaction time, pH, and initial F concentration. After 48 hours, the reaction reached equilibrium and yielded a maximum adsorption amount of 21.6 mg/g at pH 6 through regression analysis using Langmuir equation. To further understand the mechanisms of F adsorption on HAP, we employed advanced geochemical approaches, such as XRD, SEM, HR-TEM, and 19F solid state NMR, to characterize the sorption products before and after reaction. It can be concluded that formation of F-Hap (s) solid-solution is the dominant mechanism at high F initial concentration (>10 ppm). This study demonstrates that hydroxyapatite is a good candidate material for fluoride removal. %K 羟基磷灰石< %K /br> %K 氟 %U http://geology.nju.edu.cn/CN/abstract/abstract9773.shtml