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Synthesis of a kaolin-based geopolymer using a novel fusion method and its application in effective water softening

机译:一种新型融合方法合成高岭土基高分子及其在有效水软化中的应用

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In this study, kaolin-based geopolymer was synthesized using a two-step method that consists of a fusion step (fusion of kaolin and sodium hydroxide), and a hydration and dealkalization step. The fusion step was performed at a temperature range of 400-800 degrees C for 10 to 20 h, and the hydration and dealkalization step was carried out by washing the fusion product with demineralized water for a short time (< 10 min). The synthesized geopolymer was characterized using XRD, FTIR, SEM, EDS and BET analyses. The sorption efficiency of the synthesized geopolymer was examined via removing Ca2+ and Mg2+ from both model media and groundwater. Results showed that sodium hydroxide to kaolin ratio, fusion time and temperature have profound effects on the performance of geopolymer in reduction of water hardness. Response Surface Methodology (RSM) was used to determine the optimal geopolymer synthesis conditions. RSM results indicated that the sodium hydroxide to kaolin ratio of > 2.2, the fusion time of > 14 h and the fusion temperature range of 500-700 degrees C provide the optimal synthesis conditions. Moreover, the synthesized geopolymer can efficiently adsorb Ca2+ and Mg2+ from both model media and groundwater. Based on the Langmuir isotherm model, the maximum Ca2+ adsorption capacity was 76.34 mg/g at 25 degrees C, increasing to 94.34 mg/g at 45 degrees C. Similarly, the maximum Mg2+ adsorption capacity increased from 39.68 mg/g at 25 degrees C to 51.55 mg/g at 45 degrees C. The adsorption experimental data at the above mentioned temperatures (i.e., 25 and 45 degrees C) fitted well with the pseudo-second-order model. Finally, efficient regeneration of the saturated geopolymer, using sodium chloride solution, suggested that the dominating mechanism of water softening by the synthesized geopolymer is ion exchange.
机译:在这项研究中,高岭土基聚合物是通过两步法合成的,该方法包括一个融合步骤(高岭土和氢氧化钠的融合)以及一个水合和脱碱步骤。在400-800℃的温度范围内进行熔融步骤10至20小时,并且通过用去离子水短时间(<10分钟)洗涤熔融产物来进行水合和脱碱化步骤。使用XRD,FTIR,SEM,EDS和BET分析对合成的地质聚合物进行表征。通过从模型介质和地下水中去除Ca2 +和Mg2 +来检查合成的地质聚合物的吸附效率。结果表明,氢氧化钠与高岭土的比例,熔融时间和温度对降低水硬度对地聚合物的性能有深远的影响。响应面法(RSM)用于确定最佳的地质聚合物合成条件。 RSM结果表明,氢氧化钠与高岭土之比> 2.2,熔融时间> 14h,熔融温度范围为500-700℃提供了最佳的合成条件。此外,合成的地质聚合物可以有效地从模型介质和地下水中吸收Ca2 +和Mg2 +。根据Langmuir等温模型,在25摄氏度时最大Ca2 +吸附容量为76.34 mg / g,在45摄氏度时增加至94.34 mg / g。类似地,最大Mg2 +吸附容量从25摄氏度时的39.68 mg / g增加。在45摄氏度时,其吸附量为51.55 mg / g。在上述温度(即25和45摄氏度)下的吸附实验数据与拟二阶模型非常吻合。最后,使用氯化钠溶液对饱和地质聚合物进行有效再生,表明合成的地质聚合物软化水的主要机理是离子交换。

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