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利用氟磷灰石沉淀法对饮用水进行部分除氟

Partial defluoridation of drinking water using fluorapatite precipitation.

作者信息

Larsen M J, Pearce E I

机构信息

Royal Dental College, Arhus, Denmark.

出版信息

Caries Res. 1992;26(1):22-8. doi: 10.1159/000261421.

Abstract

Ion adsorption and ion exchange are two methods commonly used in small home units to treat drinking water to bring the fluoride concentration to within acceptable limits. However, the necessary flowthrough system is often difficult to arrange where there is no piped supply and gradual exhaustion of the active agent is not easily detected. In an attempt to overcome these problems a defluoridation method based on the precipitation of a sparingly soluble fluoride salt, fluorapatite, has been studied. Samples of simulated high-fluoride drinking waters, approximately 10 ppm F, were saturated with brushite, resulting in a state of supersaturation with respect to fluorapatite. Subsequent seeding with hydroxyapatite caused a lowering of the calcium, phosphate, and fluoride concentrations in solution, indicative of fluorapatite precipitation. Repeating the process had an additive effect. Bone char was a less effective seed than hydroxyapatite with water containing fluoride only, but was a more effective seed with simulated Kenyan borehole water containing additional salts. Sixty-minute brushite saturation and apatite seeding steps were generally more effective than 10-min steps. The results suggest that apatite coprecipitation may be a convenient low-technology way to defluoridate drinking water, although prior testing might be useful to ensure adequate removal of fluoride.

摘要

离子吸附和离子交换是小型家用设备中常用的两种饮用水处理方法,用于将氟化物浓度降至可接受的范围内。然而,在没有管道供水的地方,通常很难安排必要的流通系统,而且活性剂的逐渐耗尽也不容易检测到。为了克服这些问题,人们研究了一种基于难溶性氟化物盐氟磷灰石沉淀的除氟方法。模拟高氟饮用水样品(氟含量约为10 ppm)用透钙磷石饱和,导致相对于氟磷灰石处于过饱和状态。随后用羟基磷灰石晶种接种导致溶液中钙、磷和氟浓度降低,表明有氟磷灰石沉淀。重复该过程具有累加效应。对于仅含氟的水,骨炭作为晶种的效果不如羟基磷灰石,但对于含有额外盐分的模拟肯尼亚钻孔水,骨炭是更有效的晶种。通常,60分钟的透钙磷石饱和和磷灰石晶种接种步骤比10分钟的步骤更有效。结果表明,磷灰石共沉淀可能是一种方便的低技术饮用水除氟方法,不过事先进行测试可能有助于确保氟的充分去除。

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