期刊文献+

海洋沉积物孔隙水中阴阳离子含量的离子色谱法分析方法 被引量:5

ION CHROMATOGRAM METHOD FOR ANALYZING ANIONS AND CATIONS IN PORE WATER FROM MARINE SEDIMENTS
下载PDF
导出
摘要 分别采用Metrosep A Supp4-250型阴离子柱和Metrosep C 2-150型阳离子柱,以1.8 mmol/L Na2CO3+1.7 mmol/L NaHCO3和4 mmol/L酒石酸+0.75 mmol/L吡啶二羧酸为阴阳离子淋洗液,用离子色谱仪来测定海洋沉积物孔隙水中阴离子Cl-、Br-和SO42-浓度和阳离子Na+、NH4+、K+、Ca2+、Mg2+的浓度。特别是针对高Cl-和高Na+背景下Br-和NH4+的测定做了专门分析,得到了较理想的结果,建立了一套离子色谱法测定海洋沉积物孔隙水中常见的阴阳离子含量的实验方法。 We use ion chromatogram technique to determine the anion and cation ion concentrations in pore waters. Metrosep A Supp4-250 type column and 1.8 mmol/L Na2CO3 +1.7 mmol/L NaHCO3mixed solution in anion system are used to determine concentrations of Cl^-, Br-and SO4^2- in pore water, and Metrosep C 2-150 type column and 4 mmol/L tartaric acid+0. 75 mmol/L C7H5NO4 mixed solution in cation system are used to determine concentrations of Na^+ , NH^+ , K^+ , Ca^3+ and Mg^2+. The results indicate that correlation coefficient between measured and standard values for each ion in standard solutions preponderates over 0. 999. The detection limit is less than 0. 5 mg/L, and the relative standard deviation is better than 3%. In particular, we carried out special experiment to measure Br^- concentration under high Cl^- concentration background as well as NH4^+ concentration under high Na^+ concentration background. Right now, a tentative ion chromatograph method for analyzing concentrations of cations and anions in pore water from marine sediments has been established in our lab. This method has been proved to be rapid, simple, sensitive, and accurate.
出处 《海洋地质与第四纪地质》 CAS CSCD 北大核心 2006年第4期125-130,共6页 Marine Geology & Quaternary Geology
基金 国家高新技术研究开发计划("863")天然气水合物探测技术课题(2003AA611020/02) 天然气水合物资源综合评价及勘探开发战略研究项目(GZHZ200200203-04-02)
关键词 离子色谱 孔隙水 阴阳离子 天然气水合物 ion chromatograph pore water cation anion gas hydrate
  • 相关文献

参考文献15

二级参考文献80

  • 1杨书农,李元山,田昭武.新型无泵阀毛细管等速电泳仪的研制——Ⅰ.积木式分离管路结构及电位梯度检测器[J].分析测试通报,1990,9(6):69-72. 被引量:5
  • 2杨书农 李元山 等.-[J].分析测试通报,1990,9(6):69-69.
  • 3穆纪千 卓向东 等.-[J].厦门大学学报:自然科学版,1991,30(6):537-537.
  • 4-.-[J].二氧化氯技术资料,1999,(1):5-6.
  • 5Kastner M, Kvenvolden K A, Whiticar M J, et al. Relation between pore fluid chemistry and gas hydrates associated with bottom-simulating reflectors at Cascadia Margin, Site 889 and 892[A]. Carson B, Westbrook G K, Musgrave R J, et al. Proceedings of the Ocean Drilling Program, Scientific Results, 146[C]. College Station, Texas: Texas A & M University ( Ocean Drilling Program), 1995. 175 - 187.
  • 6Borowski W S, Paull C K, Ussler Ⅲ, W. Global and local variations of interstitial sulfate gradients in deep-water, continental margin sediments: Sensitivity to underlying methane and gas hydrates [J]. Marine Geology, 1999, 159:131-154.
  • 7Zhu Y, Huang Y, Matsumoto R, et al. Geochemical and stable isotopic compositions of pore fluids and authigenic siderite concretions from Site 1146, ODP Leg 184: Implications for gas hydrate [ A]. Prell W L, Wang P, Blum P, et al. Proceedings of the Ocean Drilling Program, Scientific Results [ C]. College Station, Texas: Texas A & M University ( Ocean Driuing Program), 2003. 184:1 -15.
  • 8Hesse R. Pore water anomalies of submarine gas-hydrate zones as tool to assess hydrate abundance and distribution in the subsurface: What have we learned in the past decade? [J]. Earth Sciences Reviews, 2003, 61: 149 - 179.
  • 9Kvenvolden K A, Kastner M. Gas hydrates of the Peruvian outer continental margin [ A ]. Suess E, Von Huene R, et al. Peru Continental Margin. Proceedings of the Ocean Drilling Program,Scientific Results, 112 [ C]. College Station, Texas: Texas A & M University (Ocean Drilling Program), 1990. 112:517 -526.
  • 10Hesse R, Harrison W E. Gas hydrates (clathrates) causing porewater freshening and oxygen-isotope fractionation in deep-water sedimentary sections of terrigenous continental margins [ J ].Earth and Planetary Science Letters, 1981, 55:453 -462.

共引文献171

同被引文献149

引证文献5

二级引证文献19

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部