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中国西南部地区卡尼期危机及其成因探讨
  • 期刊名称:矿物岩石地球化学通报,2010, 29(3):227-232
  • 时间:0
  • 分类:O657.3[理学—分析化学;理学—化学]
  • 作者机构:[1]成都理工大学材料与化学化工学院,四川成都610059, [2]成都理工大学沉积地质研究院,四川成都610059
  • 相关基金:国家自然科学基金项目(40872082,41272131)资助
  • 相关项目:青藏高原腹地中新世湖相叠层石成因及古环境演化研究
中文摘要:

针对污泥中复杂基质的特点,进行了三种样品湿法消解体系、还原剂、载流等实验条件的研究,确定了HNO3-HClO4湿法消解体系、5%硝酸载流和0.1%硼氢化钠还原剂、以及标准和样品中5%硝酸+0.05%重铬酸钾混合溶液的酸度介质等,用以测试污泥中痕量Hg的实验条件。该方法快速、准确,易操作,检出限为0.06μg.L-1,连续11次测定4.0μg.L-1 Hg标准溶液相对标准偏差为2.0%,实验建立的氢化物原子荧光(HG-AFS)测定污泥中痕量Hg的测试方法具有较好的应用前景。

英文摘要:

Due to the complex matrix characteristic of sludge samples,the research on three wet digestion systems and the conditions of reducing agent,and carrier flow was carried.The experiment conditions of HNO3-HClO4 wet systems,namely 5% HNO3 carrier flow,0.1% NaBH4 reducing agent,and acidity medium of 5% HNO3+0.05% K2Cr2O7 mixed solution,etc.were finally determined to measure the trace mercury in sludge samples.This recommended method has many advantages,such as accurate and quick detection and simple operation.The determination limit is 0.06 μg·L-1,and the relative standard deviation for 11-time determination of the solution containing 4.0 μg·L-1 Hg is 2.0%.This method for trace mercury in sludge samples by hydride generation-fluorescence(HG-AFS) can be widely used.

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