地质样品中硫化物形式铁的分离和测定

周佳琦, 胡超涌, 马仲武, 谢树成. 地质样品中硫化物形式铁的分离和测定[J]. 海洋地质与第四纪地质, 2010, 30(2): 143-146. doi: 10.3724/SP.J.1140.2010.02143
引用本文: 周佳琦, 胡超涌, 马仲武, 谢树成. 地质样品中硫化物形式铁的分离和测定[J]. 海洋地质与第四纪地质, 2010, 30(2): 143-146. doi: 10.3724/SP.J.1140.2010.02143
ZHOU Jiaqi, HU Chaoyong, MA Zhongwu, XIE Shucheng. SEPARATION AND DETERMINATION OF SULFIDES COMBINED WITH IRON IN THE GEOLOGICAL SAMPLES[J]. Marine Geology & Quaternary Geology, 2010, 30(2): 143-146. doi: 10.3724/SP.J.1140.2010.02143
Citation: ZHOU Jiaqi, HU Chaoyong, MA Zhongwu, XIE Shucheng. SEPARATION AND DETERMINATION OF SULFIDES COMBINED WITH IRON IN THE GEOLOGICAL SAMPLES[J]. Marine Geology & Quaternary Geology, 2010, 30(2): 143-146. doi: 10.3724/SP.J.1140.2010.02143

地质样品中硫化物形式铁的分离和测定

  • 基金项目:

    国家自然科学基金重点项目(40531004)

    中国石油化工股份有限公司海相油气勘探前瞻性项目(G0800-06-2S-319)

详细信息
    作者简介: 周佳琦(1985-),男,硕士生,主要从事海洋地球化学研究,E-mail:jiaqizhou945@gmail.com
  • 中图分类号: P736.21

SEPARATION AND DETERMINATION OF SULFIDES COMBINED WITH IRON IN THE GEOLOGICAL SAMPLES

  • 提出一个利用次氯酸钠氧化铁硫化物碱性磺基水杨酸提取并直接测定碳酸盐相中铁硫化物的方法。结果表明,30%的NaClO溶液浸泡样品40 h以上,可以完全释放铁硫化物并形成氢氧化铁胶体。0.1 g/mL的碱性磺基水杨酸溶液则较容易地溶解新生成的氢氧化铁胶体,形成黄色的铁-磺基水杨酸络合物,可被分光光度法定量测定。该方法集选择性分离、富集和测定于一体,分析流程简单,结果可靠,适合地质样品中硫化物形式铁的测定。
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出版历程
收稿日期:  2009-09-17
修回日期:  2009-11-27

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