有机磷对无镁白钨矿形成的影响

Toshiisa Konishi, Sadayuki Watanabe
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引用次数: 0

摘要

以不同烷基链长度的有机磷酸盐为原料,通过溶剂热反应合成了无镁白脱石(WH)颗粒。研究了有机磷酸盐及其Ca/P摩尔比对WH生成的影响。随着有机磷酸盐烷基链长度的增加和Ca/P摩尔比的增加,优势相由WH变为羟基磷灰石(HA)。这一结果表明,有机磷酸盐具有不同的水解速率。对于所有的有机磷酸盐,只有在Ca/P摩尔比为0.25时才能得到WHs。此外,利用H和P核磁共振波谱分析了WH的局部结构,发现WH含有质子化磷酸(HPO4)和微量HA亚相。(2021年7月12日收稿;2021年9月15日录用)
本文章由计算机程序翻译,如有差异,请以英文原文为准。
EFFECT OF ORGANOPHOSPHATES ON THE FORMATION OF MAGNESIUM-FREE WHITLOCKITE
Objective of the present study was to synthesize Mg-free whitlockite (WH) particles using organophosphates with different alkyl chain lengths via a solvothermal reaction. The effects of the organophosphates and their Ca/P molar ratio on the formation of WH were investigated. With increasing alkyl chain length of the organophosphate and increasing Ca/P molar ratio, the dominant phase changed from WH to hydroxyapatite (HA). This result suggests that the organophosphates exhibited different hydrolysis rates. With all of the organophosphates, WHs were obtained only at a Ca/P molar ratio of 0.25. In addition, an analysis of the local structure using H and P nuclear magnetic resonance spectroscopy indicated that the WH contained protonated phosphate (HPO4 ) and trace amount of HA subphase. (Received Jul 12, 2021; Accepted Sept 15, 2021)
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