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扰动频率对底泥吸附和固定磷的影响
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摘要
以重污染河道底泥和上覆水为材料,研究了周期性加入外源磷条件下,不同扰动频率下底泥吸附和固定磷的作用机制.结果表明,增加扰动频率显著增加了了外源磷吸附量.尽管加入的磷以溶解性磷酸盐形式存在,但扰动强化了溶解态磷向颗粒态磷的转化,从而降低磷的生物可利用性.内源磷形态分析表明,弱吸附态磷(NH4Cl-P)均呈降低趋势,而铁铝结合态磷(Fe/Al-P)、钙结合态磷(HCl-P)则呈增加趋势.增加扰动频率可以增加生物难利用磷占总磷的比例.说明增加扰动频率,有利于底泥对外源磷的吸附以及促进生物可利用态磷向难被生物利用态磷的转化.
The mechanism of phosphorus(P) adsorption and immobility under different disturbance frequency was investigated in laboratory. The sediments and water were taken from an inner-city heavily polluted canal.Addition of KH2PO4 into the experimental units were made similar to the external P input into the canal and carried out continuously. Results show that P adsorption amount increased with the disturbance frequency increase. The addition of KH2PO4 into the overlying water is main dissolved inorganic P(DIP), but sediment disturbance could promote the transformation of P from dissolved P to particulate P, indicating the bioavailability of P decrease. Sedimentary P fractionation shows that the NH4Cl-P decreased and the Fe/Al-P and the HCl-P increased. The ratio of nonbioavailable P to total P in the sediments increased with the disturbance frequency increase. It is suggested that increasing disturbance frequency is favor of P adsorption on the sediments and promotion of the transformation of P from bioavailable P to nonbioavailable P in the sediments.
引文
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