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运用原位衰减全反射红外光谱法研究铬磁铁矿对磷酸根的吸附作用
An in Situ ATR-FTIR Study on Adsorption of Phosphate by Chromate Doped Magnetite

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林枭举 1   梁晓亮 2   初本莉 3 *   何宏平 2   朱建喜 2   朱润良 2  
文摘 采用原位衰减全反射红外光谱技术(ATR-FTIR)探讨pH值和磷酸根浓度对磷酸根在磁铁矿表面吸附形态的影响。结果表明:随着pH值降低,磷酸根浓度增大,磷酸根在磁铁矿表面的吸附量随之增加,形成内层吸附。发现有3种吸附模型:①在低pH值时,主要形成对称性为C_1的吸附形态,可能主要是单质子化双齿双核络合形态;②在高pH值条件下发现有2种形态,高磷酸根浓度条件下,形成1种对称性为C_(3v)吸附形态,主要是单齿单核络合形态,在低浓度条件下,发现1种C_(2v)对称性吸附形态,可能是去质子化双齿双核络合形态,与单齿单核络合形态的物种在低浓度条件下共同存在。
其他语种文摘 Phosphate adsorption on Cr-doped magnetite was characterized as the function of pH and phosphate concentration by in situ ATR-FTIR spectroscopy. The aim of this study is to investigate adsorption morphology of phosphate the variation medium condition. Results indicate that three inner-sphere complexes formed. At lower pH,monoprotonated bidentate-binuclear complex is dominated, while the monodentate mononuclear species are predomionated at higher pH and the nonprotonated and bidentate binonuclear species are also existing at higher and lower loadings.
来源 矿物学报 ,2017,37(1/2):188-195 【核心库】
DOI 10.16461/j.cnki.1000-4734.2017.01.023
关键词 磁铁矿 ; 吸附 ; 磷酸根 ; 衰减全反射红外光谱
地址

1. 华南师范大学物理与电信工程学院, 中国科学院矿物学与成矿学重点实验室;;广东省矿物物理与材料开发研究重点实验室, 广东, 广州, 510006  

2. 中国科学院广州地球化学研究所, 中国科学院矿物学与成矿学重点实验室;;广东省矿物物理与材料开发研究重点实验室, 广东, 广州, 510640  

3. 华南师范大学物理与电信工程学院, 广东, 广州, 510006

语种 中文
文献类型 研究性论文
ISSN 1000-4734
学科 地质学;环境污染及其防治
基金 国家自然科学基金项目
文献收藏号 CSCD:5986921

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