SEPARATION AND DETERMINATION OF SULFIDES COMBINED WITH IRON IN THE GEOLOGICAL SAMPLES
-
摘要: 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。Abstract: A method was proposed for the determination of trace iron released from sulfides in geological samples. Iron was extracted and spectrophotometry measured by sulphosalicylic acid after sulfides were oxidized by sodium hypochlorite. The results show that 30% of sodium hypochlorite soaking the sample for more than 40 hours could transform iron sulfides completely into colloidal ferric hydroxide, which can be easily extracted by the sulphosalicylic acid solution. We integrate the selective sepatation,enrichment and determination of iron in the procedure to make the method simple and suitable for determination of iron sulfides in geological samples.
-
Key words:
- iron sulfides /
- sodium hypochlorite /
- sulphosalicylic acid /
- spectrophotometer
-
-
[1] 刘相梅,彭平安,黄伟林,等.自然界中铁硫化物矿物对含氯有机化合物降解作用[J].地质地球化学,2002,30(04):46-52.
[LIU Xiangmei,PENG Pingan,HUANG Weilin,et al.Degradation of chlorinated organic compounds by iron sulfide minerals in natural processes[J].Geology and Geochemistry,2002,30(04):46-52.]
[2] 初凤友,陈丽蓉,申顺喜,等.南黄海自生黄铁矿成因及其环境指示意义[J].海洋与湖沼,1995,26(3):227-233.
[CHU Fengyou,CHEN Lirong,SHEN Shunxi,et al.Origin and environmental significance of authigenic pyrite from the South Yellow(Huanghai)Sea sediment[J].Oceanologia and Limnologia,1995,26(3):227-233.]
[3] Berner R A.Sedimentary pyrite formation[J].American Journal of Science,1970,268:1-23.
[4] Lyons T W,Severmann S.A critical look at iron paleoredox proxies:New insight from modern euxinic marine basins[J].Geochimica et Cosmochimica Acta,2006,70:5698-5722.
[5] Canfield D E,Raiswell R,Westrich J T.The use of chromium reduction in the analysis of reduced inorganic sulfur in sediments and shales[J].Chemical Geology,1986,54(1-2):149-155.
[6] Burdett J W,Arthur M A,Richardson M.A Neogene seawater sulfur isotope age curve from calcareous pelagicmicrofossils[J].Earth and Planetary Science Letters,1989,94(3-4):189-198.
[7] 岩石矿物分析编写组.岩石矿物分析·第一分册[M].第三版.北京:地质出版社,1991:250-251.[The group of rock and mineral analysis of the preparation.Rock and Mineral Analysis First Fascicle[M].The third published.Beijing:Geological Publishing House,1991:250
-251.]
[8] [9] 程建光,薛彦辉,张培志.化学脱硫方法初探[J].选煤技术,2001,5:14-17.[CHENG Jianguang,XUE Yanhui,ZHANG Peizhi.Methods of chemical desulfurization[J].Coal Preparation Technology,2001
,5:14-17.]
[10] 王德杰,范代读,李从先.不同预处理对沉积物粒度分析结果的影响[J].同济大学学报,2003,31(3):314-318.
[WANG Dejie,FAN Daidu,LI Congxian.The results of different pretreatment of the sediment grain size analysis[J].Journal of Tongji University,2003,31(3):314-318.]
-
计量
- 文章访问数: 790
- PDF下载数: 0
- 施引文献: 0