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首页> 外文期刊>Journal of environmental sciences >Speciation of organic phosphorus in a sediment profile of Lake Taihu II. Molecular species and their depth attenuation
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Speciation of organic phosphorus in a sediment profile of Lake Taihu II. Molecular species and their depth attenuation

机译:太湖II沉积物剖面中有机磷的形态分子种类及其深度衰减

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The understanding of organic phosphorus (P) dynamics in sediments requires information on their species at the molecular level, but such information in sediment profiles is scarce. A sediment profile was selected from a large eutrophic lake, Lake Taihu (China), and organic P species in the sediments were detected using solution phosphorus-31 nuclear magnetic resonance spectroscopy (~(31)P NMR) following extraction of the sediments with a mixture of 0.25 mol/L NaOH and 50 mmol/L EDTA (NaOH-EDTA) solution. The results showed that P in the NaOH-EDTA extracts was mainly composed of orthophosphate, orthophosphate monoesters, phospholipids, DNA, and pyrophosphate. Concentrations of the major organic P compound groups and pyrophosphate showed a decreasing trend with the increase of depth. Their half-life times varied from 3 to 27 years, following the order of orthophosphate monoesters > phospholipids ≥ DNA > pyrophosphate. Principal component analysis revealed that the detected organic P species had binding phases similar to those of humic acid-associated organic P (NaOH-NRP_(HA)), a labile organic P pool that tends to transform to recalcitrant organic P pools as the early diagenetic processes proceed. This demonstrated that the depth attenuation of the organic P species could be partly attributed to their increasing immobilization by the sediment solids, while their degradation rates should be significantly lower than what were suggested in previous studies.
机译:对沉积物中有机磷(P)动力学的理解要求在分子水平上提供有关其种类的信息,但是在沉积物剖面中此类信息很少。从一个富营养化的太湖(太湖)(中国)中选出沉积物剖面,然后用溶液磷31核磁共振谱(〜(31)P NMR)检测沉积物中的有机P物种,然后提取沉积物。 0.25 mol / L NaOH和50 mmol / L EDTA(NaOH-EDTA)溶液的混合物。结果表明,NaOH-EDTA提取物中的P主要由正磷酸盐,正磷酸盐单酯,磷脂,DNA和焦磷酸盐组成。随着深度的增加,主要的有机P化合物基团和焦磷酸盐的浓度呈下降趋势。它们的半衰期从3到27年不等,依次为正磷酸单酯>磷脂≥DNA>焦磷酸。主成分分析表明,所检测到的有机磷物质具有与腐殖酸相关的有机磷(NaOH-NRP_(HA))相似的结合相,这是一种不稳定的有机磷库,随着早期成岩作用,该有机磷库往往转化为顽固的有机磷库。流程继续进行。这表明,有机磷物质的深度衰减可能部分归因于沉积物固体对有机磷物质的固定作用,而其降解速率应大大低于先前研究的建议。

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