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Direct Ultraviolet Spectrophotometric Determination of Total Sulfide and Iodide in Natural Waters

机译:直接紫外分光光度法测定天然水样中的总硫和碘

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摘要

A technique is described that allows the determination of total dissolved sulfide in natural waters using direct ultraviolet detection of the HS~(-) ion. The concentration of bisulfide is determined by measuring absorption from 214 to 300 nm and then deconvolution of the HS~(-) spectra from the complex spectrum of natural fluids. A nonlinear least-squares fitting approach is used for the deconvolution. At a pH near 8, where >95% of total sulfide is present as HS~(-), the results are indistinguishable from total sulfide measured using the methylene blue method in a wide range of sample types and matrixes including freshwater from groundwater wells, marine hydrothermal vent fluids, and marine sediment porewaters. The method allows simultaneous determination of other UV-absorbing ions, including nitrate, bromide, and iodide, in samples with low total sulfide concentrations. Bisulfide concentrations can be determined in samples with low background absorption, such as well water and hydrothermal fluids, with a detection limit of <1 μM. The detection limit for bisulfide in sediment porewaters that have a high organic loading, which produces background absorbances of ~0.5 A at 260 nm in a 1-cm cuvette, is 5 μM. The only chemical manipulation required is buffering acidic samples to pH >7 and filtration of particulate-rich samples.
机译:描述了一种技术,该技术允许使用HS〜(-)离子的直接紫外线检测来确定天然水中总溶解的硫化物。通过测量从214到300 nm的吸收,然后从天然流体的复杂光谱中解开HS〜(-)光谱,确定二硫化物的浓度。非线性最小二乘拟合方法用于反卷积。在接近8的pH值下,> 95%的总硫化物以HS〜(-)的形式存在,结果与使用亚甲基蓝法在各种样品类型和基质(包括地下水井中的淡水)中测得的总硫化物没有区别。海洋热液排放流体和海洋沉积物孔隙水。该方法可以同时测定总硫化物浓度低的样品中其他吸收紫外线的离子,包括硝酸根,溴离子和碘离子。可以在背景吸收低的样品(例如井水和热液)中测定二硫化物浓度,检测限<1μM。在1 cm的比色杯中,有机物含量高的沉积物孔隙水中的二硫化物的检出限为5μM,在260 nm处产生的背景吸光度约为0.5A。唯一需要的化学操作是将酸性样品缓冲至pH> 7并过滤富含颗粒的样品。

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