轻组有机质对太湖沉积物氮、磷矿化的影响

Effect of Light Fraction Organic Matter on Mineralization of N and P in Taihu Lake Sediments

  • 摘要: 采用连续淹水培养试验研究轻组有机质(LFOM)对鼋头渚(Y)和贡湖(G)2种不同污染程度太湖沉积物氮、磷矿化的影响. 结果表明,去除LFOM并没有改变沉积物氮、磷的矿化趋势. 试验初期,沉积物累积矿化氮、磷量急速上升,之后增速变慢,至峰值后迅速下降,42 d时达到最小值,并持续至试验结束. 经过77 d的培养试验,不同处理的2种不同污染程度沉积物有24%~39%的总氮(TN)和7%~26%的总磷(TP)被矿化;污染较重的沉积物Y的净矿化氮、磷量和矿化速率均高于沉积物G;去除LFOM使沉积物的净矿化氮、磷量和矿化速率均有所降低,其中沉积物Y的净矿化氮、磷量分别降低了110.86和145.26 mg/kg,下降了15%和74%,沉积物G降低了195.13和29.99 mg/kg,下降了40%和50%. 沉积物Y的氮、磷平均矿化速率分别降低了3.01和5.36 mg/(kg·d),沉积物G分别降低了6.35和1.30 mg/(kg·d).

     

    Abstract: The effect of light fraction organic matter (LFOM) on nitrogen (N) and phosphorus (P) mineralization in the sediments of Taihu Lake was investigated under continuously water-logged incubation. The sediments fromYuantouzhu (Y) and Gonghu (G) at different pollution levels were used. The results showed that the effect of LFOM removal on N and P mineralization of differenttrophic sediments was similar. At the early stage, the amounts of N and P mineralization increased quickly, but later the extent decreased; after reaching the peakvalues, the amounts decreased to the lowest at 42 d and then stayed minimum until the end of the incubation. During 77 day anaerobic incubation, the results showed that 24%-39% of TN and 7%-26% of TP of the studied sediments were mineralized. The amounts and rates of N and P mineralization from the heavily polluted sediment Y were higher than those of sediment G, in which the amounts and rates decreased after removal of the LFOM. In sediment Y, the amounts of N and P mineralized decreased 110.86 mg/kg (amounts to 15%) and 145.26 mg/kg (74%), respectively; in sediment G, the amounts decreased were 195.13 mg/kg (40%) and 29.99 mg/kg(50%), respectively. After the LFOM removal, the average mineralization rates of N and P decreased 3.01 mg/(kg·d) and 5.36 mg/(kg·d) for sediment Y, and 6.35 mg/(kg·d) and 1.30 mg/(kg·d) for sediment G, respectively.

     

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