首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Arsenic distribution in the dissolved, colloidal and particulate size fraction of experimental solutions rich in dissolved organic matter and ferric iron
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Arsenic distribution in the dissolved, colloidal and particulate size fraction of experimental solutions rich in dissolved organic matter and ferric iron

机译:富含溶解有机物和三价铁的实验溶液的溶解态,胶态态和颗粒态级分中的砷分布

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Due to the widespread contamination of groundwater resources with arsenic (A_s), controls on As mobility have to be iden_tified. In this study we focused on the distribution of As in the dissolved, colloidal and particulate size fraction of experimental solutions rich in ferric iron, dissolved organic matter (DOM) and As(V). Size fractions between <5 kD_a and >0.2 _m were separated by filtration and their elemental composition was analyzed. A steady-state particle size distribution with stable ele_ment concentration in the different size classes was attained within 24 h. The presence of DOM partly inhibited the formation of large Fe-(oxy)hydroxide aggregates, thus stabilized Fe in complexed and colloidal form, when initially adjusted molar Fe/C ratios in solution were <0.1. Dissolved As concentrations and the quantity of As bound to colloids (<0.2 urn) increased in the presence of DOM as well. At intermediate Fe/C ratios of 0.02-0.1, a strong correlation between As and Fe concentration occurred in all size fractions (R~2 = 0.989). At Fe/C ratios <0.02, As was mainly present in the dissolved size fraction. These observations indicate that As mobility increased in the presence of DOM due to (I) competition between As and organic mole_cules for sorption sites on Fe particles; and (II) due to a higher amount of As bound to more abundant Fe colloids or com_plexes <0.2 _m in size. The amount of As contained in the colloidal size fractions also depended strongly on the initial size of the humic substance, which was larger for purified humic acids than for natural river or soil porewater samples. Arsenic in the particle size fraction >0.2 _m additionally decreased in the order of pH 4 __6 > 8. The presence of DOM likely increases the mobility of As in iron rich waters undergoing oxidation, a finding that has to be considered in the investigation of organic-rich terrestrial and aquatic environments.
机译:由于砷广泛污染地下水资源,必须确定对砷迁移率的控制。在这项研究中,我们集中于富含三价铁,溶解有机物(DOM)和As(V)的实验溶液中As在溶解,胶体和颗粒级分中的分布。通过过滤分离出<5 kD_a和> 0.2 _m之间的大小部分,并分析其元素组成。在24小时内获得了不同尺寸类别中具有稳定元素浓度的稳态粒径分布。当最初调整的溶液中Fe / C摩尔比<0.1时,DOM的存在会部分抑制大的Fe-(羟基)氢氧化物聚集体的形成,从而以复合和胶体形式稳定Fe。在DOM的存在下,溶解的As浓度和与胶体结合的As量(<0.2 um)也增加。当Fe / C的中间比率为0.02-0.1时,在所有尺寸分数中,As和Fe浓度之间都存在很强的相关性(R〜2 = 0.989)。在Fe / C比<0.02时,As主要存在于溶解的胶体中。这些观察结果表明,在DOM存在下,As迁移率增加是由于(I)As与有机分子之间竞争Fe颗粒上的吸附位点; (II)由于大量的As结合到尺寸更宽的<0.2 _m的更丰富的Fe胶体或复合体上。胶体粒径级分中所含的As含量也强烈取决于腐殖质的初始粒径,腐殖酸的初始粒径比天然河水或土壤孔隙水样品的粒径大。砷的粒径分数> 0.2 _m时,其pH值依次为4 __6>8。DOM的存在可能会增加砷在经历氧化作用的富铁水中的迁移率,这一发现在研究有机物时必须加以考虑。丰富的陆地和水生环境。

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