过量藻期湖泊沉积物中磷形态转化规律研究

Cao Shiwei, Chen Wei, Yang Min
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引用次数: 1

摘要

通过对城市浅水湖泊(以宣武湖为例)沉积物中磷形态及磷释放影响因素的实验研究,结果表明:藻过量期水体pH值较高时,沉积物中磷深度释放,总溶解磷(TDP)从0.049mg/L增加到3.255mg/L,是原浓度的66倍。沉积物中的有机磷(OP)转化为无机磷(IP),成为影响沉积物磷释放的重要磷形态。沉积物中溶解磷(DOP)和碱性磷酸盐(APA)与水体TDP呈正相关,说明微生物加速了沉积物中磷的释放过程。过量藻期结束后,水体pH值缓慢下降,沉积物中的磷不再释放,沉积物再次成为水环境中污染物的集合。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study on the Law of the Phosphorus Forms Transformation in the Sediment of Excess Alga Period Lake
Based on the experiment of the phosphorus forms and the effect factors of phosphorus release from sediment in the urban shallow lake (taking Lake Xuanwu as a example)¿the results showed that when the water body had higher pH value during the excess alga period, phosphorus in the sediment was released deeply and the total dissolved phosphorus(TDP) was increased from 0.049mg/L to 3.255mg/L as 66 times as the origin concentration. The organic phosphorus(OP) in the sediment was transformed into inorganic phosphorus(IP) and became the important phosphorus forms that influenced the phosphorus release from sediment. The results also showed that the dissolved phosphorus(DOP) and alkaline phosphate(APA) in the sediment had positive correlated with the TDP of the water, which proved that microbial hasten the process of phosphorus release from the sediment. After the excess alga period ending, the pH value of waterbody would decrease slowly, phosphorus in sediment would not release any longer and sediment would become the collection of pollutants in the water environment again.
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