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Distribution of mercury, methyl mercury and organic sulphur species in soil, soil solution and stream of a boreal forest catchment

机译:北方森林集水区土壤,土壤溶液和溪流中汞,甲基汞和有机硫物种的分布

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Concentrations of methyl mercury, CH3Hg (II), total mercury, Hgtot = CH3Hg (II) + Hg (II), and organic sulphur species were determined in soils, soil solutions and streams of a small (50 ha) boreal forest catchment in northern Sweden. The CH3Hg (II)/Hgtot ratio decreased from 1.2–17.2% in the peaty stream bank soils to 0.4–0.8% in mineral and peat soils 20 m away from the streams, indicating that conditions for net methylation of Hg (II) are most favourable in the riparian zone close to streams. Concentrations of CH3Hg (II) bound in soil and in soil solution were significantly, positively correlated to the concentration of Hgtot in soil solution. This, and the fact that the CH3Hg (II)/Hgtot ratio was higher in soil solution than in soil may indicate that Hg (II) in soil solution is more available for methylation processes than soil bound Hg (II). Reduced organic S functional groups (Org-SRED) in soil, soil extract and in samples of organic substances from streams were quantified using S K-edge X-ray absorption near-edge structure (XANES) spectroscopy. Org-SRED, likely representing RSH, RSSH, RSR and RSSR functionalities, made up 50 to 78% of total S in all samples examined. Inorganic sulphide [e.g. FeS2 (s)] was only detected in one soil sample out of 10, and in none of the stream samples. Model calculations showed that under oxic conditions nearly 100% of Hg (II) and CH3Hg (II) were complexed by thiol groups (RSH) in the soil, soil solution and in the stream water. Concentrations of free CH3Hg+ and Hg2+ ions in soil solution and stream were on the order of 10−18 and 10−32M, respectively, at pH 5. For CH3Hg (II), inorganic bi-sulphide complexes may contribute to an overall solubility at concentrations of inorganic sulphides higher than 10−9M, whereas considerably higher concentrations of inorganic sulphides (lower redox-potential) are required to increase the solubility of Hg (II).
机译:测定土壤,溶液中甲基汞,CH3 Hg(II),总汞,Hgtot = CH3 Hg(II)+ Hg(II)和有机硫的浓度瑞典北部一处小面积(50公顷)的北方森林流域。 CH3 Hg(II)/ Hgtot 的比率从河溪土壤中的1.2–17.2%降低到距离河溪20 m的矿物和泥炭土中的0.4–0.8%,这表明Hg(II)的净甲基化在靠近溪流的河岸带最为有利。土壤和土壤溶液中结合的CH3 Hg(II)的浓度与土壤溶液中Hgtot 的浓度呈显着正相关。这以及土壤溶液中CH3 Hg(II)/ Hgtot 比高于土壤中的事实可能表明,土壤溶液中的Hg(II)比土壤结合物更容易用于甲基化过程汞(II)。使用S K边缘X射线吸收近边缘结构(XANES)光谱对土壤,土壤提取物中和溪流中有机物样品中还原的有机S官能团(Org-SRED )进行了定量。 Org-SRED 可能代表RSH,RSSH,RSR和RSSR功能,在所有检查的样品中占总S的50%至78%。无机硫化物[例如FeS2 (s)]仅在十分之一的土壤样品中被检测到,而在所有流样品中均未检测到。模型计算表明,在有氧条件下,土壤,土壤溶液和溪流中的Hg(II)和CH3 Hg(II)中有近100%被巯基(RSH)络合。在土壤溶液和水流中,游离CH3 Hg + 和Hg2 + 离子的浓度分别为10−18 和10−32 M。 pH5。对于CH3 Hg(II),当无机硫化物的浓度高于10-9 M时,无机双硫化物络合物可能对整体溶解度有贡献,而无机硫化物的浓度要高得多(较低)需要氧化还原电位)以增加Hg(II)的溶解度。

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    《Biogeochemistry》 |2003年第1期|53-76|共24页
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