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首页> 外文期刊>Journal of environmental sciences >Characteristics and distribution of low molecular weight organic acids in the sediment porewaters in Bosten Lake, China
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Characteristics and distribution of low molecular weight organic acids in the sediment porewaters in Bosten Lake, China

机译:博斯腾湖沉积物孔隙水中低分子量有机酸的特征与分布

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摘要

The composition and vertical profiles of low molecular-weight organic acids (LMWOAs) and the contribution of them to dissolved organic matter (DOM) in sediment porewaters in Bosten Lake, Xinjiang, China were investigated. The results showed that total concentration of LMWOAs was up to 94.5 μmol/L and their proportion in DOM was 5.6%, suggesting that LMWOAs were important chemical components in DOM in lake sediment porewaters. Among the seven LMWOAs, pyruvic and acetic acid had the highest concentrations with 26.30 and 8.31 μmol/L, accounting for 51.4% and 14.92% of LMWOAs, respectively. Trifluoroacetic and sorbic acid had the lowest concentrations, indicating that the compositions of LMWOAs in relative reducing environments were largely different from those reported in glacier, atmosphere and soils. The concentrations of lactic, acetic, formic, sorbic and oxalic acid decreased with increasing depth, probably relating to stronger microbial activities in the initial stage of early diagenesis. Trifluoroacetic acid was mainly anthropogenic with its concentration, showing a diffusive trend from the surface to bottom sediments. The concentrations of lactic acid and nitrate generally showed a consistent profile. The increasing concentration of pyruvic acid in the vertical profile was just opposite to that of sulfate, revealing a significant negative relationship between them. Oxalic acid remained constant except for an obvious peak at 6 cm depth. The results indicated the diversities in sources and behaviors for various LMWOAs during early diagenesis in sediments.
机译:研究了新疆博斯腾湖沉积物孔隙水中低分子量有机酸(LMWOA)的组成和垂直剖面及其对溶解性有机质(DOM)的贡献。结果表明,LMWOAs的总浓度高达94.5μmol/ L,在DOM中的比例为5.6%,表明LMWOAs是湖泊沉积物孔隙水中DOM中的重要化学成分。在这七个LMWOA中,丙酮酸和乙酸浓度最高,分别为26.30和8.31μmol/ L,分别占LMWOA的51.4%和14.92%。三氟乙酸和山梨酸的浓度最低,表明在相对还原性环境中LMWOA的组成与冰川,大气和土壤中报告的那些大不相同。乳酸,乙酸,甲酸,山梨酸和草酸的浓度随深度增加而降低,这可能与早期成岩初期微生物活性增强有关。三氟乙酸的浓度主要是人为的,从表层沉积物到底部沉积物呈扩散趋势。乳酸和硝酸盐的浓度通常显示出一致的曲线。丙酮酸垂直浓度的增加与硫酸盐的浓度正好相反,表明它们之间存在显着的负相关关系。草酸保持恒定,除了在6 cm深度有一个明显的峰。结果表明,在沉积物中早期成岩过程中,各种LMWOA的来源和行为存在多样性。

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