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镁离子型Birnessite的合成和表征 被引量:1

Synthesis and Characterization of Mg-Birnessite
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摘要 采用MnO-4和Mn2+在强碱性条件下制得层状结构的Mg_Birnessite,用XRD(X射线多晶粉末衍射)、FT-IR(傅里叶红外光谱)、TG-DTG/DTA(热失重-微商热失重/热分析)等方法对它进行了表征。Mg_Birnesite在200~400℃时为无定形,在600℃生成结晶良好的Mn2O3相。CCl4、CH3OH、n_C6H14的吸附等温线类似于第三种类型的吸附等温线,在接近饱和的情况下都有凝聚现象产生。在600℃,比表面和吸附数据表明出现层状结构塌陷。吸附吡啶FT-IR谱表明在Mg_Birnesite中存在非质子酸(L酸)和质子酸(B酸)酸位。 Mg_Birnessite,a layer_structured manganese oxide,was prepared by the redox reaction between Mn^2+and MnO_4 under strong alkaline conditions.Its characterization was carried out by means of X-ray diffraction (XRD),Fourier-transform infrared spectrophotometry (FT-IR),thermal gravity-differential thermal gravity analysis/differential thermal analysis(TG_DTG/DTA).Mg-Birnessite upon heating between 200~400 ℃ is turned to an amorphous phase.At 600 ℃ it is transformed into a well crystalline Mn_2O_3 phase.Adsorption isotherms of CCl_4,CH_3OH and n-C_6H_14 vapors are analogous to the third-type isotherms.In all cases,condensation occurred near saturation points.At 600 ℃,the specific surface area and adsorption data suggest the collapse of the layer structure.The FT_IR spectra of adsorbed pyridine show the presence of both Lewis and Brnsted acid sites in Mg-Birnessite.
出处 《分析测试学报》 CAS CSCD 1998年第2期20-23,共4页 Journal of Instrumental Analysis
关键词 镁离子型 BIRNESSITE 锰氧化物 Mg-Birnessite Mg-Birnessite,Characterization,Adsorption isotherm,Acid site
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参考文献4

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同被引文献57

  • 1Cai J, Liu J, Suib S L. Preparative parameters and framework dopant effects in the synthesis of layer-structure birnessite by air oxidation. Chemistry of Materials, 2002, 14: 2071~2077
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  • 5Yang D S, Wang M K. Syntheses and characterization of birnessite by oxidizing pyrochroite in alkaline conditions. Clays and Clay Minerals, 2002, 50: 63~69
  • 6Feng X H, Liu F, Tan W F, et al. Synthesis of birnessite by O2 oxidation in alkali medium: Effects of synthesis conditions. Clays and Clay Minerals, 2004, 52(2): 240~250
  • 7Lanson B, Drits V A, Feng Q, et al. Structure of synthetic birnessite: Evidence for a triclinic one-layer unit cell. American Mineralogist, 2002, 87: 1662~1671
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