中国地质学会岩矿测试技术专业委员会、国家地质实验测试中心主办

电感耦合等离子体发射光谱法测定地热水中的硫化物

李清彩, 赵庆令, 安茂国, 孙宁, 张守文. 电感耦合等离子体发射光谱法测定地热水中的硫化物[J]. 岩矿测试, 2017, 36(3): 239-245. doi: 10.15898/j.cnki.11-2131/td.201612120181
引用本文: 李清彩, 赵庆令, 安茂国, 孙宁, 张守文. 电感耦合等离子体发射光谱法测定地热水中的硫化物[J]. 岩矿测试, 2017, 36(3): 239-245. doi: 10.15898/j.cnki.11-2131/td.201612120181
Qing-cai LI, Qing-ling ZHAO, Mao-guo AN, Nin SUN, Shou-wen ZHANG. Determination of Sulfide in Geothermal Water by Inductively Coupled Plasma-Optical Emission Spectrometry[J]. Rock and Mineral Analysis, 2017, 36(3): 239-245. doi: 10.15898/j.cnki.11-2131/td.201612120181
Citation: Qing-cai LI, Qing-ling ZHAO, Mao-guo AN, Nin SUN, Shou-wen ZHANG. Determination of Sulfide in Geothermal Water by Inductively Coupled Plasma-Optical Emission Spectrometry[J]. Rock and Mineral Analysis, 2017, 36(3): 239-245. doi: 10.15898/j.cnki.11-2131/td.201612120181

电感耦合等离子体发射光谱法测定地热水中的硫化物

  • 基金项目:
    山东省地热资源综合评价项目(鲁地字﹝2017)023号)
详细信息
    作者简介: 李清彩, 工程师, 从事地质实验测试工作。E-mail:qclee2008@163.com
    通讯作者: 赵庆令, 高级工程师, 从事地质实验测试及水工环地质工作。E-mail:zqlzb@126.com
  • 中图分类号: P641;O657.31

Determination of Sulfide in Geothermal Water by Inductively Coupled Plasma-Optical Emission Spectrometry

More Information
  • 地热水中的硫化物(H2S、HS-和S2-)通常受到硫酸根、亚硫酸根、硫代硫酸根等硫元素的共存干扰,并且硫化物具有热、光、氧不稳定性,在水样保存、前处理、标准溶液配制等环节影响着测试的准确度和精密度。本文在现场采集的地热水水样中加入乙酸锌及氢氧化钠,使硫化物形成硫化锌沉淀而与溶液分离,将此沉淀溶于双氧水和逆王水,使低价态的S2-氧化成稳定的SO42-,选择易于纯化且性质稳定的硫酸钠配制硫标准储备液,以182.624 nm谱线作为硫元素分析谱线,应用电感耦合等离子体发射光谱法测定出地热水样中的硫化物含量。硫的浓度在0.1~100 mg/L范围内与其发射强度呈线性(相关系数为0.9994);方法检出限为0.009 mg/L,相对标准偏差(n=11)低于1.80%,实际水样中硫化物的加标回收率介于99.0%~103.0%。与前人相关测试方法相比,本方法的技术指标具有优势。
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  • 图 1  准确度与精密度试验

    Figure 1. 

    表 1  ICP-OES仪器工作参数

    Table 1.  Operating parameters for ICP-OES determination

    工作参数 设定值
    垂直观测高度 15 mm
    蠕动泵泵速 50 r/min
    冷却气流量 一般
    辅助气流量 1.0 L/min
    发射功率 1250 W
    载气压强 0.22 MPa
    冲洗时间 30 s
    短波积分时间 20 s
    下载: 导出CSV
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出版历程
收稿日期:  2016-12-12
修回日期:  2017-05-20
录用日期:  2017-05-28

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