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张东, 李玉红, 张鸿禹, 郝伟博, 晏文荣, 杨伟, 贾保军. 应用改进DDARP方法纯化天然水体样品中硫酸钡固体的效果评价[J]. 岩矿测试, 2019, 38(1): 77-84. DOI: 10.15898/j.cnki.11-2131/td.201804100040
引用本文: 张东, 李玉红, 张鸿禹, 郝伟博, 晏文荣, 杨伟, 贾保军. 应用改进DDARP方法纯化天然水体样品中硫酸钡固体的效果评价[J]. 岩矿测试, 2019, 38(1): 77-84. DOI: 10.15898/j.cnki.11-2131/td.201804100040
Dong ZHANG, Yu-hong LI, Hong-yu ZHANG, Wei-bo HAO, Wen-rong YAN, Wei YANG, Bao-jun JIA. Application of Modified DDARP Method for Purification of Barite in Natural Water Samples[J]. Rock and Mineral Analysis, 2019, 38(1): 77-84. DOI: 10.15898/j.cnki.11-2131/td.201804100040
Citation: Dong ZHANG, Yu-hong LI, Hong-yu ZHANG, Wei-bo HAO, Wen-rong YAN, Wei YANG, Bao-jun JIA. Application of Modified DDARP Method for Purification of Barite in Natural Water Samples[J]. Rock and Mineral Analysis, 2019, 38(1): 77-84. DOI: 10.15898/j.cnki.11-2131/td.201804100040

应用改进DDARP方法纯化天然水体样品中硫酸钡固体的效果评价

Application of Modified DDARP Method for Purification of Barite in Natural Water Samples

  • 摘要: 二乙酸三胺五乙酸(DTPA)溶解再沉淀方法(DDARP)可去除硫酸钡沉淀过程中引入的硝酸盐杂质,但该方法对不同类型水体样品硫酸钡沉淀处理效果报道不多,特别是对有机质含量高的水体样品沉淀的硫酸钡固体是否有纯化作用尚未明确。本文选择硫酸钡高纯试剂以及水体样品沉淀的硫酸钡固体作为研究对象,采用改进DDARP方法纯化后,借助元素分析仪和稳定同位素质谱仪测定纯化前后硫酸钡固体的氧同位素值,对比分析该方法的纯化效果。结果表明:①改进DDARP方法主要内容为20mg硫酸钡沉淀溶于30mL DTPA-氢氧化钠混合溶液,再沉淀后超纯水洗涤2次,硫酸钡高纯试剂纯化前后氧同位素值没有明显变化,说明其杂质少,可直接作为实验室标准使用,而黄河水硫酸钡沉淀纯化前后氧同位素差异均值为0.8‰,说明其杂质较多,需要纯化。②六种不同类型水体硫酸钡沉淀纯化前后氧同位素差异值范围为-0.4‰~+1.9‰,其中溶解性洗衣粉、地下水、河水、生活污水、溶解性化学肥料以及雨水的差异均值分别为0.7‰、0.2‰、0.3‰、-0.3‰、0.1‰和1.4‰。③雨水硫酸钡沉淀纯化前后氧同位素差异值较大(+0.5‰~+1.9‰),与雨水中较高NO3/SO4摩尔比值(0.2~1.9,均值0.7)有关。污水纯化前后氧同位素差异值为负值(-0.2‰~0.4‰),说明纯化方法可以去除有机物干扰。研究认为:改进DDARP方法有效降低了硝酸盐和有机质干扰,有利于获得更准确的硫酸盐样品氧同位素组成,可以作为水体硫酸盐氧同位素标准纯化方法。

     

    Abstract:
    BACKGROUNDDiethylenetriaminepentaacetic acid (DTPA) dissolution and reprecipitation (DDARP) method is used frequently to eliminate encapsulated nitrate during barite precipitation. However, the effect of DDARP on barite precipitated from different kinds of natural water is rarely reported, particularly it is not clear whether the DDARP method plays a role in eliminating the effect of organic matter on barite from organic-rich water samples.
    OBJECTIVESTo obtain more accurate sulfate oxygen isotope values, using the modified DDARP method and identify the factors affecting the oxygen isotope values of barite from natural water samples.
    METHODSElement Analyzer (EA) coupled with Isotope Ratio Mass Spectrometry (IRMS) was used to determine the oxygen isotope values of original and purified barite.
    RESULTSAfter purification, oxygen isotope values of high grade barite reagent show little variations, indicating that purification of high grade barite reagent is not needed and it can be directly used as the laboratory standard. However, oxygen isotope values of barite from Yellow River water have large variations from 0.6 to 1.0 with an average of 0.8‰, indicating that it is necessary to purify natural water barite. The differences in oxygen isotope values between original and purified barite from natural water samples vary from -0.4‰ to +1.9‰, and the average differences of oxygen isotope values are 0.7‰, 0.2‰, 0.3‰, -0.3‰, 0.1‰ and 1.4‰ for dissolved detergent, groundwater, river water, sewage, dissolved fertilizer, and rainwater, respectively. The large positive differences of oxygen isotope values (from +0.5‰ to +1.9‰) between original and purified barite is found in rainwater samples due to nitrate encapsulated in barite, which is related to the high molar ratio of nitrate to sulfate in rainwater (from 0.2 to 1.9 with an average of 0.7). The negative differences of oxygen isotope values (from -0.2‰ to 0.4‰) are observed in sewage with respect to the organic matter encapsulated in barite from organic-rich sewage, suggesting that the purification method can remove organic interference.
    CONCLUSIONSThe modified DDARP method works well in eliminating nitrate and organic matter encapsulated in barite. It can be used to purify barite to obtain more accurate oxygen isotope values of sulfate in natural water samples. The proposed method can be used as a standard purification method for water body sulfate oxygen isotope determination.

     

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