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首页> 外文期刊>Fresenius Environmental Bulletin >EFFECTS OF AIR-DRYING ON PHOSPHORUS SORPTION IN SHALLOW LAKE SEDIMENT, CHINA
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EFFECTS OF AIR-DRYING ON PHOSPHORUS SORPTION IN SHALLOW LAKE SEDIMENT, CHINA

机译:空气干燥对浅水湖泊沉积物中磷吸收的影响

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摘要

Air-drying has significant influences on phosphorus sorption behaviors in soils. It is urgently necessary to expend the relevant knowledge to sediments of lakes, especially large eutrophic ones. Sediments were collected at different sites in a Chinese large shallow eutrophic lake (Lake Chaohu) and an urban shallow lake (Lake Donghu) in November 2007; contents of organic matter (OM) were measured. Phosphorus sorption behavior fitted Langmuir equation well. Compared to the field-moist sample, the air-dried sediments had significantly lower sorption energy (K). Additionally, there was a significant positive relationship between the OM content and K value in the field-moist sediments. The changes in geochemical characteristics of iron oxide and organic carbon may be mainly responsible for the decreasing K value in air-dried sediment. Furthermore, in the incubation experiments, the air-dried sediments generally gave higher concentrations of soluble reactive phosphorus coupled with alkaline phosphatase activity, which was mainly due to the decreased phosphorus sorption energy, because there was no significant differences of pH values and dissolved oxygen concentrations between the air-dried and field-moist sediments. Finally, in contrast with the field-moist samples, the air-dried ones showed a significantly positive relationship between OM content and EPC_0 value, suggesting that the breakdown of OM during drying may be a major source of P upon reflooding.
机译:空气干燥对土壤中磷的吸附行为有重要影响。迫切需要将有关知识扩展到湖泊,特别是大型富营养化湖泊的沉积物中。 2007年11月,在中国大型浅水富营养化湖泊(巢湖)和城市浅水湖泊(东湖)的不同地点收集了沉积物;测量有机物的含量(OM)。磷的吸附行为很好地拟合了朗缪尔方程。与田间潮湿的样品相比,风干的沉积物的吸附能(K)明显较低。此外,田间湿润沉积物中的OM含量和K值之间存在显着的正相关。氧化铁和有机碳的地球化学特征的变化可能是造成风干沉积物中K值降低的主要原因。此外,在温育实验中,风干的沉积物通常会产生较高浓度的可溶性反应性磷,并伴有碱性磷酸酶活性,这主要是由于磷吸附能降低,因为pH值和溶解氧浓度没有显着差异在风干和田间潮湿的沉积物之间。最后,与现场潮湿的样品相反,风干的样品在OM含量和EPC_0值之间显示出显着的正相关关系,这表明在干燥过程中OM的分解可能是回潮后P的主要来源。

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