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使用受限 DET 探针测定沉积物孔隙水中金属和阴离子的分布。

Use of constrained DET probe for a high-resolution determination of metals and anions distribution in the sediment pore water.

机构信息

Faculty of Chemistry, Technical University Brno, Purkynova 118, 61200 Brno, Czech Republic.

出版信息

Talanta. 2002 Apr 22;57(1):145-55. doi: 10.1016/s0039-9140(01)00679-8.

Abstract

The constrained DET (diffusive equilibrium in thin films) probe filled with agarose gel was successfully used for measuring depth profiles of metals and anions in estuarine sediments at high-resolution (mm). The agarose gel was tested for equilibration times and recoveries. For manganese (10 mg l(-1)), the equilibration time between an aqueous solution and the agarose gel was reached after 60 min. In the presence of humic acids it was five times longer. As a consequence, for field applications a deployment time of 5-24 h was applied. The subsequent elution of manganese into nitric acid was completed in less than 10 min even without mixing. For agarose gel in contact with solutions of 10 mg l(-1) ions (cadmium, copper and manganese, bromide, chloride, nitrate and sulfate), recoveries obtained were close to 100%. DET probes were applied in test laboratory sediment and in real sediment in the Authie (France) estuary. Depth profiles for 19 elements (Ag, As, Ba, Bi, Cd, Co, Cr, Cu, Fe, Mn, Mo, Ni, Pb, Sb, Se, Sr, Tl, V, and Zn) and four anions (bromide, chloride, nitrate and sulfate) were established for the test laboratory sediment. In the real sediment, the pore water concentrations of iron and manganese using gel probes were comparable with those obtained by a conventional method (box core-anoxic slicing followed by centrifugation).

摘要

用琼脂糖凝胶填充的约束 DET(薄膜中的扩散平衡)探针成功地用于以高分辨率(mm)测量河口沉积物中金属和阴离子的深度分布。测试了琼脂糖凝胶的平衡时间和回收率。对于锰(10mg/L),水溶液与琼脂糖凝胶之间的平衡时间在 60 分钟后达到。在腐殖酸存在的情况下,时间延长了五倍。因此,对于现场应用,应用了 5-24 小时的部署时间。即使没有混合,锰随后也能在不到 10 分钟的时间内用硝酸洗脱。对于与 10mg/L 离子(镉、铜和锰、溴化物、氯化物、硝酸盐和硫酸盐)溶液接触的琼脂糖凝胶,回收率接近 100%。DET 探针在 Authie(法国)河口的测试实验室沉积物和实际沉积物中进行了应用。对测试实验室沉积物中的 19 种元素(Ag、As、Ba、Bi、Cd、Co、Cr、Cu、Fe、Mn、Mo、Ni、Pb、Sb、Se、Sr、Tl、V 和 Zn)和 4 种阴离子(溴化物、氯化物、硝酸盐和硫酸盐)建立了深度分布。在实际沉积物中,使用凝胶探针测量的铁和锰的孔隙水浓度与传统方法(无氧箱芯切片,然后离心)获得的浓度相当。

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