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红磷锰矿的常压回流合成、表征及Rietveld结构精修

Synthesis, characterization and Rietveld refinement of hureaulite at atmospheric pressure

中文摘要英文摘要

30 mmol Mn(H2PO4)2溶液在40~100 ℃常压回流下反应生成非均一棱柱状红磷锰矿,X-射线衍射及Rietveld结构精修、傅立叶变换红外吸收光谱和扫描电子显微镜表征产物晶体结构和微观形貌。反应条件相同,而原料不同,所得产物形貌差异显著。上述体系中添加等摩尔量磷酸,只有在100 ℃回流反应才能生成棒状红磷锰矿;进一步添加NaClO溶液可有效提高红磷锰矿收率,产物形貌呈均一棒状。相同条件下,采用MnCl2和H3PO4混合溶液回流反应无红磷锰矿沉淀生成,但反应溶液中添加NaClO溶液可生成颗粒状红磷锰矿。Mn(H2PO4)2溶液在40 ℃回流12 h时,所得产物为红磷锰矿和磷酸一氢锰混合物,二者质量百分含量分别为59.24%和40.76%;随着回流时间延长,磷酸一氢锰逐渐转化为纯相红磷锰矿。回流24 h和48 h,所得产物中,红磷锰矿含量分别增加至86.11%和100%。合成的红磷锰矿为单斜晶系,空间群为C12/c1,晶体常数为:a=17.64183(56)A, b=9.14788(28)A, c=9.51034(32)A, β=96.5665(17)deg,M=718.57 g/mol,V=1524.761(85)A3,ρ=3.01058(17) g/cm3 ,Z=4。不同温度下制备的红磷锰矿具有相似的晶体学参数,但随着温度升高,c轴方向上有一定程度压缩,且β角逐渐减小,产物密度逐渐增加。常压或表生较低温条件下红磷锰矿密度低于热液成因矿物,这可作为判断红磷锰矿成因的快捷方法。本实验较好地模拟了自然界表生环境中红磷锰矿的形成过程,这为红磷锰矿成因矿物学理论提供了新的内容,亦可为其在化学、材料科学等领域的应用提供新的制备方法。

Prismatic hureaulite was synthesized by refluxing of 100 mL 0.3 mol/L Mn(H2PO4)2 solution at atmospheric pressure under different temperatures (40, 50, 60, 80 and 100 ℃). Powder X-ray diffraction, Rietveld refinement, Fourier transform infrared spectroscopy and scanning electron microscopy were used to characterize the crystal structure and micro-morphologies of hureaulite. Products obtained from different reactants had various morphologies. Needle-like hureaulite was fabricated at 100 ℃ when 30 mmol H3PO4 was added into 100 mL 0.3 mol/L Mn(H2PO4)2 solution. Hureaulite was prepared by further adding NaClO solution into the reaction system. Hureaulite was not formed when Mn(H2PO4)2 was substituted by MnCl2 and H3PO4, but it came into being by further adding an amount of NaClO solution in the reaction solution. The transformation process of hureaulite at mild conditions was investigated. Mixture of hureaulite and MnHPO4o3H2O was produced by reflux of 100 mL 0.3 mol/L Mn(H2PO4)2 at 40 ℃ for 12 h, and the former was about 59.24% in mass. MnHPO4o3H2O was then transformed into hureaulite by further prolonging the reflux time. After refluxing for 24 h and 48 h, the content of hureaulite increased to 86.11% and 100% respectively. Synthesized hureaulite crystallized in the space group C12/c1, belonging to the monoclinic system. The unit-cell parameters obtained from Rietveld refinement are: a=17.64183(56)A, b=9.14788(28)A, c=9.51034(32)A, β=96.5665(17)deg ,M=718.57 g/mol,V=1524.761(85) A3,ρ=3.01058(17) g/cm3,Z=4. Most of the crystal parameters were closely similar when products were fabricated at different temperatures, however, the unit cell was compressed in the c axis direction and β decreased with the increase of temperature. The calculated densities of hureaulite increased with the increase of reaction temperature. That was to say, the density of hureaulite in supergene soil is lower than that of those formed by hydrothermal reaction, which help us distinguish the formation mechanism of hureaulite. Hureaulite was successfully prepared in mild conditions, which was similar to the natural temperature in soils, and the genetic mineralogy of hureaulite should be re-recognized. The new preparation method also facilitated the exploitation and application of hureaulite in the field of chemistry and materials science.

刘凡、邱国红、谭文峰、殷辉、冯雄汉

化学晶体学无机化学工业

红磷锰矿常压回流傅立叶变换红外吸收光谱Rietveld结构精修

HureauliteRefluxing at atmospheric pressureFourier transform infrared spectroscopiesRietveld structure refinement

刘凡,邱国红,谭文峰,殷辉,冯雄汉.红磷锰矿的常压回流合成、表征及Rietveld结构精修[EB/OL].(2011-01-07)[2025-08-16].http://www.paper.edu.cn/releasepaper/content/201101-317.点此复制

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